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HomeMy WebLinkAboutWetland Classification, Identification, Delineation-2014 t`, I I : I � � : . � , ' � . � I � " :� :�,� �, .. ;. .� � . �!. : : ' - • . - � � � � • � . • � • . ' �'�� �� I�` / � _ � � �` `v . '�. ��'. 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Table of Contents ABSTRACT.................................................................................................................................................1 INTRODUCTION.......................................................................................................................................1 METHODS..................................................................................................................................................1 RESULTS....................................................................................................................................................2 DISCUSSION..............................................................................................................................................6 RECOMMENDATIONS............................................................................................................................6 CERTIFICATION......................................................................................................................................8 DATASOURCES.......................................................................................................................................9 LITERATUREREFERENCED..............................................................................................................10 FIGURES: Figure 1: Site Location Overlaid on Topographic Map Figure 2a: National Wetland Inventory Figure 2b: Hennepin County Wetland Inventory Figure 2c: 2014 DNR NWI Update Figure 3: Web Soil Survey-Hennepin County Figure 4: Public Waters Inventory Figure 5: Approximate Wetland Boundary and Sample Point Location Figure 6: Approximate Wetland Boundary and Soils TECHNICAL DOCUMENTS: Photo Log Field Data Sheets Plant Indicator Status Soil Series Data ABSTRACT Svoboda Ecological Resources (SER) visited the above referenced properry on October 9 and October 1 S, 2014 to examine the site for the presence of areas meeting wetland criteria. The study parcel is located in Orono, MN, Hennepin County (Figure 1). Three wetland boundaries was flagged and one area was sampled at this site. Sample transects were established along the boundary at vegetation transition points in order to characterize the soil, vegetation, and existing hydrology within the wetland-to-upland transition zone. INTRODUCTION The subject parcels, 200 and 350 Stubbs Bay Road, are approximately 30.29 acres in size in total. and are dominated by various cover types including hardwood forest, lowland forest, emergent wetland, vacant grassland, and two separate residential structures with accompanying outbuildings. The topography of the site slopes generally eastward towards a large wetland complex. The surrounding land use is mostly undeveloped semi-rural land in the City of Orono with scattered single family homes. US Highway 12 and a major rail corridor lie just ot the north of the site. The identified wetlands were classified according to the Cowardin et al., the Circular 39 and the Eggers and Reed classification systems and marked with pink "Wetland Delineation" pin flags. The Technical Documents section of this report contains field data sheets, plant indicator status information, soil survey information, and wetland definition information. METHODS The methods used to delineate the subject parcel are as described in the 1987 US Army Corps of Engineers Wetlands Delineation Manual and the 2010 Midwest Regional Supplement Manual. In the 1987 Manual, the methods used were described under the "routine" methods for sites greater than 5 acres. This methodology is followed in order to assess whether the three parameters of a wetland are met for areas on the subject parcel. The three parameters required under normal circumstances in order to delineate a wetland are described in the Technical Documents section. The Midwest Regional Supplement Wetland Delineation Manual is also being utilized to increase the accuracy of our wetland boundaries. This addendum to the original 87 Manual was created to address the many regional differences that affect wetlands and the delineation methods used throughout the country. The following explanations are passages from that document. "This Regional Supplement is part of a nationwide effort to address regional wetland characteristics and improve the accuracy and efficiency of wetland- delineation procedures. Regional differences in climate, geology, soils, hydrology plant and animal communities, and other factors are important to the identification and functioning of wetlands. These differences cannot be considered adequately in a single national manual. The development of this supplement follows National Academy of Sciences recommendations to increase the regional sensitivity of wetland-delineation methods (National Research Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 1 Orono Council 1995). The intent of this supplement is to bring the Corps Manual up to date with current knowledge and practice in the region and not to change wetland boundaries." "...This Regional Supplement is designed for use with the current version of the Corps Manual (Environmental Laboratory 1987) and all subsequent versions. Where differences in the two documents occur, this Regional Supplement takes precedence over the Corps Manual for applications in the Midwest Region." National Wetland Inventory (NWI) maps (Figure 2a) Hennepin County Wetland Inventory (HCWI) maps (Figure 2b), 2014 DNR NWI Update maps (Figure 2c), Web Soil Survey of Hennepin County map (Figure 3), Minnesota Public Waters Inventory maps (Figure 4), and 2012 aerial photographs were reviewed prior to the site visit to identify areas that may be wetlands. Areas illustrating evidence of wetland conditions were examined in greater detail during the field survey. Vegetation, soils and hydrology were examined (as outlined in the 1987 Manual) and used to characterize wetland types and determine wetland boundaries. Sample transects were established in representative wetland-to-upland transition zones in order to characterize the vegetation, soils, and hydrology of the site. Transects consist of a representative upland sample point and representative wetland sample point. Information obtained at the sample points can be found on the field data sheets located in the Technical Documents section. Wetland boundaries were marked at the site by pink "Wetland Delineation" pin flags. The wetland boundary is considered to be the topographically highest extent of the wetland basin; areas below the staked boundary met the three required wetland criteria while areas above were lacking in one or more of these criteria. Wetlands were classified in accordance with methods described by Cowardin et al. (1979) and used in the NWI (e.g. PEMB, PSS1C, etc.), completed by the U.S. Fish and Wildlife Service. The Circular 39 and Eggers and Reed classification systems are also given. The indicator status of plants, as described in the Technical Documents section, was determined using the National Wetland Plant List (Lichvar, et al. 2014. l�ttp://rvetla�rd pla»ts.u.cncc.arrnV.Ntil�. RESULTS The National Wetland Inventory indicates the presence of one large wetland complex along the northern and eastern edge of the survey area. The wetland is categorized by the NWI as PFO/EMCd (Figure 2a). The HCWI indicates probable and potential wetlands in the same location(Figure 2b). The DNR NWI update in 2014 indicates generally similar wetland types but generally does not map the wetlands on the 200 Stubbs Bay Road parcel (Figure 2c). The Web Soil Survey of Hennepin County (Figure 3) identifies six soil map units within the study area. They are Lester loam, Muskego, Blue Earth, and Houghton, ponded, Cordova loam, Hamel-Glencoe, Angus loam, and LeSueur loam. The Muskego, Blue Earth and Houghton complex is considered hydric, the Cordova and the Hamel-Glencoe soils are predominantly hydric and the Lester loam, Angus loam and LeSueur loam are considered predominantly non- hydric. Soil series descriptions are provided in the Technical Documents section. The Minnesota Department of Natural Resources, State Protected Waters Map (Public Water Inventory) indicates no public waters or wetlands within the study area (Figure 4). Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 2 Orono Site Visit SER ecologists examined the subject property for areas meeting jurisdictional wetland criteria during the site visit. One area meeting the jurisdictional criteria of a wetland was flagged, and the boundary deternuned and delineated. The approximate wetland boundary is outlined in yellow (Figures 5 and 6). Accumulated precipitation since 4/O1/2014, as recorded at MSP and reported by the USDA National Agricultural Statistics Service in cooperation with the Minnesota Department of Agriculture reports that for the week ended October 19, 2014, was 6.63" above normal. Precipitation for the period 10/13/14 to 10/19/14 was reported to be 0.53" below normal and for the preceding 4 weeks was 0.65"below normal. The construction of a driveway through a large wetland area divided one potential basin into two. Therefore, this wetland investigation determined the presence of three wetland basins within the site boundary. Each basin is described below according to the findings at each sample point. Basin I The majority of the first wetland basin on this parcel is classified as a PFO 1 B, Type 1 L, floodplain forest wetland located south of the driveway and stretching southeast through a shallow ravine. East of sample transect 1-1 there is a portion of the wetland basin classified as PEMC, Type 2, fresh (wet) meadow. East of sample transect 1-2 there is a portion of the wetland basin classified as a PEMF, Type 3/4, shallow/deep marsh. The wetland vegetation was dominated by reed canary grass (Phalaris arundinacea FACV� in the herb stratum for sample points 1-1 WET. Sample point 1-2 WET was dominated by sandbar willow (Salix interior OBL) in the shrub stratum with Canada goldenrod (Solidago Canadensis FACU) and Field horsetail (Equisetum arvense FAC) in the herb stratum. The transition to upland can be marked by the change in vegetation community. The further upslope the more upland species, such as Kentucky bluegrass (Poa pratensis FAC), buckthorn (Rhamnus cathartica FAC), prickly ash (Zanthoxylum americanum FACU), smooth brome (Bromus inermis FACU) and Canada goldenrod (Solidago Canadensis FACU) become dominant as evidenced in upland samples 1-1 UP, and 1-2 UP. The upland forested areas exhibited a dominance of eastern cottonwood (Populus deltoides FAC), green ash (Fraxinus pennsylvanica FACV� and silver maple(Acer saccharinum FACV�. The soils at sample point 1-1 WET consisted of muck for 2 inches of depth where it changes to a clay with depletions until 15 inches of depth, then changed to a sandy clay with concentrations. Sample point 1-1 WET had hydric indicator Al2 (Thick Dark Surface) and F7 (Depleted Dark Surface). The web soil survey indicates the soil series as Hamel-Glencoe. The soils at sample point 1-2 WET consisted of clay for 24 inches of depth with depletions present. Sample point 1-2 WET had hydric indicator F7 (Depleted Dark Surface). The web soil survey indicates the soil series as Hamel-Glencoe. The soils at sample point 1-1 UP consisted of clay for 22 inches of depth, then switching to sandy clay with a depleted matrix from 22-30 inches. The web soil survey indicates the soil series as Lester loam. The soils at sample point 1-2 UP consisted of clay for 24 inches of depth Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 3 Orono with concentrations and depletions between 14-20 inches. The web soil survey indicates the soil series as Hamel-Glencoe. Hydric indicator Al2 (Thick Dark Surface) was present at sample locations 1-1 UP. Wetland hydrology was present at sample point 1-1 WET as signified by primary indicator A3 (Saturation) as well as secondary hydrology indicators C2 (Dry-Season Water Table), D2 (Geomorphic Position) and DS (FAC-Neutral Test). Wetland hydrology was present at sample point 1-2 WET as signified by primary indicator A3 (Saturation) as well as secondary hydrology indicators C2 (Dry-Season Water Table) and D2 (Geomorphic Position). At sample points 1-1 UP and 1-2, UP no hydrology indicators were present as the samples were located upslope, approximately 1-2 feet higher in elevation than the two wetland samples. Basin 2 The majority of the second wetland basin on this parcel is classified as a PEMC, Type 2, fresh (wet) meadow wetland located north, east and south of the residence driveway. East of sample transects 2-2 and 2-3 there is a portion of the wetland basin classified as PFO1C, Type 1L, floodplain forest. The wetland vegetation was dominated by reed canary grass (Phalaris arundinacea FACW) in the herb stratum for all sample points and green ash (Fraxinus pennsylvanica FACV� in the shrub stratum in sample point 2-3 WET. The transition to upland can be marked by the change in vegetation community. The further upslope the more upland species, such as Kentucky bluegrass (Poa pratensis FAC) and Canada goldenrod (Solidago canadensis FACU)become prevalent. The soils at sample point 2-1 WET consisted of clay for 22 inches of depth where it changes to a sandy clay with concentrations and depletions. The web soil survey indicates the soil series as Glencoe loam. The soils at sample point 2-2 WET consisted of clay for 30 inches of depth with concentrations present below 12 inches and a depleted matrix present below 20 inches. The web soil survey indicates the soil series as Muskego, Blue Earth, and Houghton soils. T'he soils at sample point 2-3 WET consisted of clay for 28 inches of depth where it changes to a sandy clay with a depleted matrix and concentrations. The web soil survey indicates the soil series as Cordova loam. Hydric indicator Al2 (Thick Dark Surface) was present at all three wetland sample locations. The soils at sample point 2-1 UP consisted of clay for 24 inches of depth with concentrations at 12-24 inches. The web soil survey indicates the soil series as Lester loam. The soils at sample point 2-2 UP consisted of clay for 36 inches of depth with concentrations present below 12 inches and a depleted matrix below 30 inches. The web soil survey indicates the soil series as LeSueur loam. The soils at sample point 2-3 UP consisted of clay for 38 inches of depth with a depleted matrix with concentrations from 30-38 inches. The web soil survey indicates the soil series as Cordova loam. Hydric indicator Al2 (Thick Dark Surface) was present at all three upland sample locations. Wetland hydrology was present at sample points 2-1 WET, 2-2, WET and 2-3 WET as signified by secondary hydrology indicators D2 (Geomorphic Position) and DS (FAC-Neutral Test) with the addition of primary indicator A3 (Saturation) at sample point 2-1 WET. At sample points 2- 1 UP, 2-2, UP and 2-3 UP no hydrology indicators were present as they were located upslope approximately two feet higher in elevation than the three wetland samples. Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 4 Orono Transect 2-3 was established along the edge of what the property owner describes as a former field road. This field road segment is bordered on either side by upland (on the west side by a former farm field/hay meadow and on the east side by a wooded area populated by green ash, boxelder and buckthorn among other species. The field road exhibits wetland characteristics while the two parallel adjoining areas do not. The reason for this change in condition is unclear. Basin 3 The third wetland basin on this parcel is classified as a PEMB, Type 2, fresh (wet) meadow wetland located in a depressional swale. The wetland vegetation was dominated by reed canary grass (Phalaris arundinacea FACV�. The transition to upland can be marked by the change in vegetation community. The further upslope the more upland species, such as smooth brome (Bromus inermis FACU), and Kentucky bluegrass(Poa pratensis FAC)become prevalent. The soils at sample point 3-1 WET consisted of clay for 30 inches of depth. The web soil survey indicates the soils series as LeSueur loam. Hydric indicator Al2 (Thick Dark Surface) was present. Soils were moist but not saturated at the time of sampling. The soils at sample point 3-1 UP consisted of 36 inches of clay with concentrations below 20 inches and a depleted matrix below 28 inches. The web soil survey indicates the soils series as Le Sueur loam. Hydric indicator Al2 (Thick Dark Surface)was present. Wetland hydrology was present at sample point 3-1 WET as evidenced by secondary hydrology indicators D2 (Geomorphic Position) and DS (FAC-Neutral Test). At sample point 3-1 UP no hydrology indicators were present as it was located upslope approximately two feet higher in elevation than the wetland sample 3-1 WET. Area A Area A is an isolated area lying at the edge of the vacant field and is characterized by a slight depression in the landscape. Area A has not been flagged subject to review by the LGU. Vegetation at sample point A-1 Wet was dominated by reed canary grass (100 percent) with a canopy presence of silver maple (20 percent). A-1 Up vegetation consisted primarily of Kentucky bluegrass(50 percent) and smooth brome(20 percent). The soils at sample point A-1 UP consisted of clay for 16 inches of depth with sandy clay containing concentrations in a depleted matrix between 16-24 inches. The web soil survey indicates the soil series as Lester loam for sample point A-1 UP. The soils at sample point A-1 WET consisted of clay for 20 inches of depth where it changes to a sandy clay with concentrations. Sample point A-1 WET had hydric indicator Al2 (Thick Dark Surface). The web soil survey indicates the soil series as Lester loam. Hydric indicator Al2 (Thick Dark Surface)was present at sample location A-1 UP. Wetland hydrology was present at sample point A-1 WET as signified by secondary hydrology indicators D2 (Geomorphic Position) and DS (FAC-Neutral Test). At sample point A-1 UP no hydrology indicators were present as the sample was located upslope, approximately 1-2 feet higher in elevation than the wetland sample. Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 5 Orono Detailed soils, vegetation, and hydrology data for the delineated jurisdictional wetlands are provided in the data sheets of the Technical Documents section. DISCUSSION A previous wetland delineation was completed for the 200 Stubbs Bay Road parcel by SER on 9/26/2005 (copy available upon request). It was reviewed by the Minnehaha Creek Watershed District and a�wetland type and boundary approval was issued by MCWD on July 5, 2006. Area A was examined in the prior delineation and determined to be non-wetland as was much of the area along the eastern edge of the former field/meadow (Area B sample point). Application of the 2010 Midwest Regional Supplement methodology provides a different result in the wetland boundary in some instances. Vegetation at Area A was markedly different in 2014 than what occurred in 2005.No reed canary grass was noted in the 2005 survey whereas in 2014 it occupied 100 percent of the area sampled. According to the report figures and documentation the sampled areas were likely nearly the same as the location in 2005 was described as a"low area". The"low area" is yuite small and easily identifiable. SER completed all on-site delineations based on the three required technical criteria as outlined by the 1987 Manual: the presence of hydric soils, a predominance of hydrophytic vegetation, and indicators of wetland hydrology in each basin. The wetland boundary was flagged on 10/09/14 and field data was collected on 10/15/14. SER personnel examined the subject property for areas meeting jurisdictional wetland criteria during the site visit and delineated the edges of the intermittently inundated depression as being jurisdictional wetland. (Figures 5 and 6). Detailed soils, vegetation and hydrology data are provided in the data sheets of the Technical Documents section. A set of figures is provided in the Figures section. RECOMMENDATIONS Activities that impact or could potentially impact wetlands are regulated at several levels of government. In Minnesota, the two primary jurisdictions are covered at the state and federal levels by the provisions of the following legislative actions. ➢ State jurisdiction by the Wetland Conservation Act of 1991 (WCA)administered by the WCA Local Governmental Unit(LGU). ➢ Federal jurisdiction by the Clean Water Act of 1972 and subsequent amendments. Wetland protection is implemented by the Corps of Engineers(Corps)with permit certification issued by the Environmental Protection Agency. While the wetland boundaries that SER has delineated are not official until approved by a WCA approved local government unit (LGU), SER advises the property owner/developer to refrain from any filling, draining, or excavating, or any impact to the area SER has delineated as Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 ( Orono wetland. No grading or filling in wetland basins should commence until all necessary permits have been obtained. Violation of wetland regulations may result in substantial civil and criminal penalties. Local ordinances may regulate wetland modifications such as brush and tree removal and burning in addition to grading and filling. Depending on the location of the property, buffers around the wetland may also be protected. Any activities in the proximity of the wetland should be cleared with appropriate WCA regulatory agencies. It is also advisable to have the wetland boundary surveyed by a licensed land surveyor. Since the pin flags used along the boundary can be vandalized or inadvertently knocked over, a GPS survey of the flags will assure the permanence of the boundary. The client should also be aware that according to current BWSR and COE wetland rules and regulations approved wetland boundaries are typically valid for five years from the date of approval. To avoid project delays associated with wetland regulations, it is essential that you acquire necessary permits from all jurisdictional agencies before initiating activities. A WCA Sequencing form, a WCA and Army Corps of Engineers Replacement Plan Application form, and a DNR pernut application are among the materials that you may be required to submit if impacts are proposed for the delineated wetlands. By initiating the permit process as soon as possible,potential costly delays to the project may be avoided. Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 '] Orono CERTIFICATION Frank Svoboda completed the flagging of the wetland boundary on 10/09/2014 and Nick McCabe collected sample data on 10/15/2014. This delineation was performed according to the procedures described by the US Army Corps of Engineers in the 1987 Wetlands Delineation Manual and the 2010 Midwest Region Supplement Wetland Delineation Manual. The delineation meets the standards and a criterion described in these manuals and conforms to the applicable standards and regulations in force at the time the delineation was completed. Report and graphics were prepared by David Remucal (Wetland Ecologist)on this day 10/16/14. The delineation report was prepared by Frank Svoboda, President of Svoboda Ecological Resources and Nick McCabe. Client: Chris Bollis Project Name: 200 and 350 Stubbs Bay Road Project No.: 2014-037-03 Location: Orono MN �;�} ��-� Nick McCabe, Senior Environmental ScientisdCertified Wetland Delineator(WDCP#1218) J� ' David Remucal,Wetland Ecologist �..a,r.D�`_" d' Franklin Svoboda, President, Svoboda Ecological Resources 10/27/2014 Date Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 g Orono DATA SOURCES Minnesota Deparixnent of Natural Resources, Public Waters Inventory Basin Delineations, Published 7/31/2008 and retrieved from http://deli.dnr.state.mn.us United States Fish and Wildlife Service National Wetland Inventory Map. Retrieved from http://www.fws.gov/wetlands/Data/Mapper.html on 06/19/12. 2010 Aerial Color Photos. Publicly Distributed by MN Geo WMS Service. Topographic maps obtained via the National Geographic Society's USA Topo service through ESRI. Web Soil Survey for Hennepin County,MN. Retrieved from http://websoilsurvey.nres.usda.gov/app/HomePage.htm Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 9 Orono LITERATURE REFERENCED Cowardin, L.M.,V. Carter, F.C. Golet, and R.T. LaRoe. 1979. Classification of Wetlands and Deepwater Habitats of the United States. U.S. Fish and Wildlife Service, FWS/OBS-79/31. 103pp. Eggers, Steve D. and Donald M. Reed. 1997. Wetland Plants and Plant Communities of Minnesota and Wisconsin. US Army Corps of Engineers, St. Paul District. 263pp,unclassified. Environmental Laboratory. 1987. 1987 U.S. Army Corps of Engineers Wetlands Delineation Manual. Technical Report Y-87-1, US Army Engineer Waterways Experiment Station, Vicksburg,Mississippi. Gleason, H.A. and A.C. Cronquist. 1991.Manual of Vascular Plants of Northeastern United States and Adjacent Canada.New York Botanical Garden, Bronx. 910pp. Sabine, B. J. 1999.National List of Plant Species that Occur in Wetlands: Region 3—North Central(Indiana, Illinois, Iowa, Michigan, Minnesota, Missouri, Wisconsin). Resource Management Group, Inc. 77pp. Shaw, S.P., and C.G. Fredine. 1956. Wetlands of the United States. U.S. Fish and Wildlife Service, Circular 39. 67pp. U.S. Army Corps of Engineers. August 2010. Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Midwest Region(Version 2.0). ERDC/EL TR-10-16. Vicksburg, MS: US Army Engineer Research and Development Center. Svoboda Ecological Resources 300&350 Stubbs Bay Road Project Number: 2014-037-03 1� Orono FIGURES . � .:� '�-'�.�� e• •��i ' �'{I�F, . � R�) "'F j'� ...„. � •'� "JSDY -- (3Y.f)��:.��_.._-._.� =------- � --�—� -- _ 'nRP Rt►}— _ "�'--�',-••.. .,. � `' � �.. _+ �i�3�} � i0a \� �+,.�'� r;�- � � t • ,q � f''� O • �. �- - � t y . . _ m� y _ , .- r ,�. _.. -�� , � g � � ' '���: .,. 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Wetland Subsections �' � ' �� '. i � � � 9 e Approximate Wetland Boundary � -� •. ,�. , ,9► • , �'x s (� � - +�`+�' '��`�""' � ��'���',� �kT��� � Approximate Parcel Boundary � � ��- '�� ���,�.%��`�' �, $OI�S , !, �,��r-�w�'���'�'���`����'* " H dric � �:�✓/`�'��j�i.I'��„� .�����'�,�� ,�, •�� . � _ y . � ° ,a_,�� , �r � . ���"''�' ��.�.�. .-.�: . : � r � -` � r.� �;�j Predominantly hydric . .� =r"�-;: ;� *'•����, +�,��*",� . •� ��� �'f*, `+`�� ` Predominantly nonhydric y.� �- �. � �� � � � �lt- 1 "�� x'3w s3' Wetland Boundaries and Soils Figure 6 Overlaid on 2012 Aerial Photo 2014-037 ��;kSVOBODA 0 175 350 700 200 & 350 Stubbs Bay Rd N : • Ecc�luRical Resourcec Feet Orono, MN THE TECHNICAL DOCUMENTATION SECTION Field Data Sheets WETLAND DETERMINATION DATA FORM-Midwest Region ProjecUSite 350 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 1-1 UP Investigator(s): NM 3ection,Township,Range: S32,T118W,R23W Landform(hillslope,terrace,etc.): Slight hillslope Local relief(concave,convex,none): None Slope(%): 2 Lat: Long: Datum: Soil Map Unit Name Lester loam VWI Classification: None Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? N Hydric soil present? Y Is the sampled area within a wetland? N indicators of wetland hydrology present? N f yes,optional weUand site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 1 (A) 2 Total Number of Dominant 3 Species Across all Strata: 2 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 50.00% (A/B) 0 =Total Cover Saolina/Shrub straturr (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 10 x 2= 20 4 FAC species 30 x 3= 90 5 FACU species 60 x 4= 240 0 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 100 (A) 350 (B) 1 Solidago canadensis 60 Y FACU Prevalence Index=B/A= 3.50 2 Poa pratensis 30 Y FAC 3 Phalaris arundinacea 10 N FACW Hydrophytic Vegetation Indicators: 4 Rapid test for hydrophytic vegetation 5 Dominance test is>50% g Prevalence index is 53.0* 7 Morphogical adaptations'(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation" 100 =Total Cover (explain) WOodY vin8 StratUm (Plot Siz@: ) •Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ic 0 =Total Cover �egetation present? N Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 1-1 UP Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type' Loc" Texture Remarks 0-22 10YR 2/1 100 CLAY 22-30 10 YR 6/1 100 SANDY CLAY *Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. "*Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) SVatified Layers(A5) Loamy Gleyed Matrix(F2) _Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) "Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emarks: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired;check all that a��lvl Seconda Indicators minimum of two r uired Surface Water(A1) Aquatic Fauna(B13) SurFace Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(610) Saturation(A3) Hydrogen Suifide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(62) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(B3) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algai Mat or Crust(64) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(65) (C6) _FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(67) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(68) Gauge or Well Data(D9) Water-Stained Leaves(69) Other(Explain in Remarks) iel bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No �Depth(inches): hydrology present? N (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located —two feet higher than 1-1 WET. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM -Midwest Region Project/Site 350 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 1-1 WET Investigator(s): NM 3ection,Township,Range: S32N T118N,R23W Landform(hillslope,terrace,etc.): Depresion/swale Local relief(concave,convex,none): Concave Slope(%): 0 Lat: Long: Datum: Soil Map Unit NameHamel-Glencoe VWI Classification: None Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,expiain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? Y Indicators of wetland hydrology present? Y f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) Wetland Boundry was flagged based on change in vegetation communiry as you move upslope. VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 1 (A) 2 Total Number of Dominant g Species Across all Strata: 1 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 100.00% (A/B) 0 =Total Cover Sa�lina/Shrub straturr (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 100 x 2= 200 4 FAC species 0 x 3= 0 5 FACU species 0 x 4= 0 0 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 100 (A) 200 (B) 1 Phalaris arundinacea 100 Y FACW Prevalence Index=B/A= 2.00 2 3 Hydrophytic Vegetation Indicators: 4 Rapid test for hydrophytic vegetation 5 X Dominance test is>50% g X Prevalence index is 53.0' 7 Morphogical adaptations*(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation` 100 =Total Cover (explain) WOOdV vine SVBtum (PIOt SiZB: ) •Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover vegetation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 1-1 WET Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type" Loc`" Texture Remarks 0-2 10YR 2/1 100 MUCK 2-15 10 YR 2/1 90 10 YR 5/1 10 D M CLAY 15-24 10 YR 6/1 90 10 YR 4/6 10 C M CLAY "Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. *"Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) SVipped Matrix(S6) iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) X Depleted Dark Surface(F7) •Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emar s: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired:check all that aaalv) Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(613) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(610) Saturation(A3) Hydrogen Sulfide Odor(C1) �Dry-Season Water Table(C2) Water Marks(61) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(B2) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(B3) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Aigal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils �Geomorphic Position(D2) Iron Deposits(65) (C6) �FAC-Neutral Test(D5) Inundation�sible on Aerial Imagery(B7) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(68) Gauge or Well Data(D9) Water-Stained Leaves(B9) Other(Explain in Remarks) Fie d bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes X No Depth(inches): 15 Indicators of wetland Saturation present? Yes T No Depth(inches): -� hydrology present? Y (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if availabie: emar s: Located within swale. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM-Midwest Region ProjecUSite 350 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 1-2 UP Investigator(s): NM 3ection,Township,Range: S32,T118N,R23W Landform(hillslope,terrace,etc.): Slight hillslope Local relief(concave,convex,none): none Slope(%): 1 to 2 Lat: Long: Datum: Soil Map Unit NameHamel-Glencoe VWI Classification: None Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significanUy disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? N Is the sampled area within a wetland? N Indicators of wetland hydrology present? N f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species 1 Populus deltoides 60 Y FAC that are OBL,FACW,or FAC: 4 (A) 2 Fraxinus pennsylvanica 30 Y FACW Total Number of Dominant 3 Species Across all Strata: 5 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 80.00% (A/B) 90 =Total Cover Sa�lina/Shrub straturr (Plot size: ) Prevalence Index Worksheet 1 Rhamnus cathartica 70 Y FAC Total%Cover of: 2 Zanthoxylum americanum 20 Y FACU OBL species 0 x 1 = 0 3 FACW species 30 x 2= 60 4 FAC species 170 x 3= 510 5 FACU species 20 x 4= 80 90 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 220 (A) 650 (B) 1 Rhamnus cathartica 40 Y FAC Prevalence Index=B/A= 2.95 2 3 Hydrophytic Vegetation Indicators: 4 Rapid test for hydrophytic vegetation 5 X Dominance test is>50% g X Prevalence index is 53.0* 7 Morphogical adaptations`(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation* 40 =Total Cover (explain) Woodv vine stratum (Plot size: ) *Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover vegetation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 1-2 UP Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type` Loc"' Texture Remarks 0-14 10YR 2/1 100 CLAY 1420 10YR 2/1 96 10 YR 4/4 2 C M CLAY 10YR 6/1 2 D M 20-24 10 YR 4/1 100 CLAY •Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. *"Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark SurFace(F6) Thick Dark Surface(Al2) Depleted Dark Surface(F7) *Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(FS) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? N Depth(inches): emar s: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired;check all that aoalv) Secondarv Indicators(minimum of two reauired Surface Water(A1) Aquatic Fauna(613) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(614) Drainage Patterns(B10) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(62) (C3) Saturation Visibie on Aerial Imagery(C9) Drift Deposits(63) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(B5) (C6) FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(67) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(68) Gauge or Well Data(D9) Water-Stained Leaves(B9) Other(Explain in Remarks) Fie d servations: Surface water present? Yes No X Depth(inches): Water table present? Yes � No Depth(inches): 28 Indicators of wetland Saturation present? Yes �— No Depth(inches): �� hydrology present? N (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located—1 foot upslope from 1-1 WET. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM-Midwest Region ProjecUSite 350 Stubbs Bay Rd. City/Counry: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 1-2 WET Investigator(s): NM 3ection,Township,Range: S32,T118N,R23W Landform(hillslope,terrace,etc.): Depression Local relief(concave,convex,none): Concave Slope(%): 0 Lat: Long: Datum: Soil Map Unit NameHamel-Glencoe VWI Classification: PEMC Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? Y Indicators of wetland hydrology present? Y f yes,optional weUand site ID: Remarks:(Explain alternative procedures here or in a separate report.) Wetland boundary in this area flagged based on changes in vegetation from willow shrub to buckthorn shrub as you move upslope. VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 2 (A) 2 Total Number of Dominant g Species Across all Strata: 3 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 66.67% (A/B) 0 =Total Cover Saolina/Shrub sVaturr (Plot size: ) Prevalence Index Worksheet 1 Salix interior 70 Y FACW Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 75 x 2= 150 4 FAC species 55 x 3= 165 5 FACU species 40 x 4= 160 70 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 170 (A) 475 (B) 1 Solidago canadensis 40 Y FACU Prevalence Index=B/A= 2.79 2 Equisetum arvense 30 Y FAC 3 Rhamnus cathartica 10 N FAC Hydrophytic Vegetation Indicators: 4 Poa pratensis 10 N FAC Rapid test for hydrophytic vegetation 5 Acer negundo 5 N FAC X Dominance test is>50% 6 Phalaris arundinacea 5 N FACW X Prevalence index is<_3.0* 7 Morphogical adaptations'(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation' 100 =Total Cover (explain) WOOdY vin2 StfBtUm (Plot Size: ) •Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover vegetation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 1-2 WET Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) °/a Color(moist) % Type` Loc" Texture Remarks 0-24 10YR 2/1 95 10YR 5/1 5 D M CLAY `Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. '"Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) _Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) •Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emar s: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired;check all that a�olvl Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(613) SurFace Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(614) Drainage Patterns(610) Saturation(A3) Hydrogen Sulfide Odor(C1) �Dry-Season Water Tabie(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(B2) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(63) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(84) Recent Iron Reduction in Tilled Soils X Geomorphic Position(D2) Iron Deposits(B5) (C6) _FAC-Neutral Test(D5) Inundation�sible on Aerial Imagery(B7) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(68) Gauge or Well Data(D9) Water-Stained Leaves(69) Other(Explain in Remarks) Fiel bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes X No Depth(inches): 14 Indicators of wetland Saturation present? Yes X No Depth(inches): 10 hydrology present? Y (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Open water—10 feet west. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM -Midwest Region ProjecUSite 200 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 1-3 UP Investigator(s): NM 3ection,Township,Range: 32S,T118N,R23W Landform(hilislope,terrace,etc.): Slight hillslope Local relief(concave,convex,none): none Slope(%): 1 to 2 Lat: Long: Datum: Soil Map Unit Name Lester loam VWI Classification: None Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (if needed,explain any answers in remarks.) Hydrophytic vegetation present? N Hydric soil present? Y Is the sampled area within a wetland? N Indicators of wetland hydrology present? N f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 1 (A) 2 Total Number of Dominant 3 Species Across all Strata: 2 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 50.00% (A/B) 0 =Total Cover Saolina/Shrub straturc (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 10 x 2= 20 4 FAC species 50 x 3= 150 5 FACU species 40 x 4= 160 0 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 100 (A) 330 (B) 1 Poa pratensis 50 Y FAC Prevalence Index=B/A= 3.30 2 Bromus inermis 20 Y FACU 3 Solidago canadensis 10 N FACU Hydrophytic Vegetation Indicators: 4 Cirsium arvense 10 N FACU Rapid test for hydrophytic vegetation 5 Phalaris arundinacea 10 N FACW Dominance test is>50% g Prevalence index is<_3.0' � Morphogical adaptations'(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation 100 =Total Cover (explain) Woodv vine stratum (Plot size: ) 'Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover vegetation present? N Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 1-3 UP Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type" Loc*" Texture Remarks 0-16 10YR 2/1 100 CLAY 16-24 10 YR 5/1 80 10YR 4/4 20 C M SANDY CLAY 'Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. ""'Location:PL=Pore Lining,M=Matrix Hydric Soil indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark SurFace(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) _Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) *Indicators of hydrophytic vegetation and weltand Sandy Mucky Minerai(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emarks: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired:check all that ao�lv) Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(613) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(614) Drainage Patterns(610) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish BuRows(C8) Sediment Deposits(B2) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(B3) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(65) (C6) _FAC-NeuVal Test(D5) Inundation Visible on Aerial Imagery(67) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(B8) Gauge or Well Data(D9) Water-Stained Leaves(B9) Other(Explain in Remarks) Field bservations: Su�face water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No —C�Depth(inches): hydrology present? N (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located—one foot higher than 1-3 WET. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM-Midwest Region ProjecUSite 350 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 2-1 UP Investigator(s): NM 3ection,Township,Range: S32,T118N,R23W landform(hillslope,terrace,etc.): Hillslope Local relief(concave,convex,none): Convex Slope(%): 2 to 5 Lat: Long: Datum: Soil Map Unit NameLester loam VWI Classification: PF01/EMCd Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? N Indicators of weUand hydrology present? N f yes,optional weUand site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree SVatum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 2 (A) 2 Total Number of Dominant 3 Species Across all Strata: 3 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 66.67% (A/B) 0 =Total Cover Saolina/Shrub straturr (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 30 x 2= 60 4 FAC species 30 x 3= 90 5 FACU species 40 x 4= 160 0 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 100 (A) 310 (B) 1 Solidago canadensis 40 Y FACU Prevalence Index=B/A= 3.10 2 Poa pratensis 30 Y FAC 3 Phalaris arundinacea 30 Y FACW Hydrophytic Vegetation Indicators: 4 Rapid test for hydrophytic vegetation 5 X Dominance test is>50% g Prevalence index is 53.0` 7 Morphogical adaptations*(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation• 100 =Total Cover (explain) Woodv vine stratum (PIOt Siz@: ) 'Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover �e9etation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 2-1 UP Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type* Loc" Texture Remarks 0-12 10YR 2/1 100 CLAY 12-24 10YR 6/1 95 10YR 4/6 5 C M CLAY "Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. *"Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) "Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emar s: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired:check all that aaalv) Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(613) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(B10) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish Burcows(C8) Sediment Deposits(62) (C3) Satura6on Visible on Aerial Imagery(C9) Drift Deposits(B3) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(B5) (C6) FAC-Neutral Test(DS) Inundation Visible on Aerial Imagery(B7) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(68) Gauge or Well Data(D9) Water-Stained Leaves(B9) Other(Explain in Remarks) ield Observations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No �—Depth(inches): hydrology present? N (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located--two feet higher than 2-1 WET. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM -Midwest Region ProjecUSite 350 Stubbs Bay Rd. Ciry/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 2-1 WET Investigator(s): NM 3ection,Township,Range: S32,T118N,R23W Landform(hillslope,terrace,etc.): Deprresion Local relief(concave,convex,none): Concave Slope(%): 0 Lat: Long: Datum: Soil Map Unit NameGlencoe loam VWI Classification: PF01/EMCd Are climatic/hydrologic conditions of the site rypical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? Y Indicators of weUand hydrology present? Y f yes,optionai wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) Wetland boundary flagged based on change in vegetation community as you move upslope. VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 1 (A) 2 Total Number of Dominant g Species Across all Strata: 1 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 100.00% (A/B) 0 =Total Cover Sa�lina/Shrub straturr (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 100 x 2= 200 4 FAC species 0 x 3= 0 5 FACU species 0 x 4= 0 0 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 100 (A) 200 (B) 1 Phalaris arundinacea 100 Y FACW Prevalence Index=B/A= 2.00 2 3 Hydrophytic Vegetation Indicators: 4 Rapid test for hydrophytic vegetation 5 X Dominance test is>50% g X Prevalence index is<_3.0* 7 Morphogical adaptations*(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation` 100 =Total Cover (explain) WoodV vine st�8tum (Plot Size: ) •Indicators of hydric soil and weUand hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover vegetation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 2-1 WET Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type' Loc"" Texture Remarks 0-22 10YR 2/1 100 CLAY 22-30 10YR 6/1 80 10YR 5/6 15 C M SANDY CLAY 106G 6/1 5 D M 'Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. ""Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) SVatified Layers(A5) Loamy Gleyed Matrix(F2) _Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) *Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emarks: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired;check all that aaolv) Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(B13) Surface Soil Cracks(66) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(610) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(62) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(63) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils �Geomorphic Position(D2) Iron Deposits(BS) (C6) X FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(B7) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(68) Gauge or Well Data(D9) Water-Stained Leaves(B9) Other(Explain in Remarks) iel bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes No —C�Depth(inches): Indicators of wetland Saturation present? Yes —� No Depth(inches): �— hydrology present? Y (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emarks: US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM-Midwest Region ProjecUSite 350 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 2-2 UP Investigator(s): NM 3ection,Township,Range: S32,T118N,R23W Landform(hillslope,terrace,etc.): Slight hillslope Local relief(concave,convex,none): none Slope(%): 1 to 2 Lat: Long: Datum: Soil Map Unit NameLe Sueur loam VWI Classification: None Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetiand? N Indicators of wetland hydrology present? N f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 4 (A) 2 Total Number of Dominant 3 Species Across all Strata: 5 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 80.00% (A/B) 0 =Total Cover Sa�lin4/Shrub straturr (Plot size: ) Prevalence Index Worksheet 1 Rhamnus cathartica 30 Y FAC Total%Cover of: 2 Cornus alba 10 Y FACW OBL species 0 x 1 = 0 3 FACW species 30 x 2= 60 4 FAC species 70 x 3= 210 5 FACU species 40 x 4= 160 40 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 140 (A) 430 (B) 1 Solidago canadensis 40 Y FACU Prevalence Index=B/A= 3.07 2 Poa pratensis 40 Y FAC 3 Phalaris arundinacea 20 Y FACW Hydrophytic Vegetation Indicators: 4 Rapid test for hydrophytic vegetation 5 X Dominance test is>50% 6 Prevalence index is<_3.0' � Morphogical adaptations"(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation" 100 =Total Cover (explain) WOOdY Vlne St�BtUm (Plot SiZe: ) •Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover vegetation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 2-2 UP Profile Description: (Describe to the depth needed to document the indicator or confrm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type" Loc*" Texture Remarks 0-12 10YR 2/1 100 CLAY 12-30 10YR 2/1 95 2.5YR 4/8 5 C M CLAY 30-36 10YR 6/1 95 1.5 YR 4/4 5 C M CLAY `Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. "Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(lRR K,L) Black Histic(A3) SVipped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) •Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emar s: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired:check all that a�nlv) Seconda Indicators minimum of two re uired SurFace Water(A1) Aquatic Fauna(613) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(B10) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(62) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(63) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(65) (C6) FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(B7) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(BS) Gauge or Well Data(D9) Water-Stained Leaves(69) Other(Explain in Remarks) ie d bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No �—Depth(inches): hydrology present? N (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located—two feet higher than 2-2 WET. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM-Midwest Region ProjecUSite 200 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 2-3 UP Investigator(s): NM 3ection,Township,Range: S23,T118N,R23W Landform(hillslope,terrace,etc.): Slight hillsiope Local relief(concave,convex,none): none Slope(%): 1 to 2 Lat: Long: Datum: Soil Map Unit NameCordova loam VWI Classification: None Are climatic/hydrologic conditions of the site rypical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significanUy disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally probiematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? N Indicators of weUand hydrology present? N f yes,optional weUand site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species 1 Fraxinus pennsylvanica 90 Y FACW that are OBL,FACW,or FAC: 2 (A) 2 Total Number of Dominant 3 Species Across all Strata: 2 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 100.00% (A/B) 90 =Total Cover Sa�lina/Shrub straturr (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 0 x 1 = 0 g FACW species 90 x 2= 180 q FAC species 90 x 3= 270 5 FACU species 10 x 4= 40 0 =Tota1 Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 190 (A) 490 (B) 1 Poa pratensis 80 Y FAC Prevalence Index=B/A= 2.58 2 Rhamnus cathartica 10 N FAC 3 Solidago canadensis 10 N FACU Hydrophytic Vegetation Indicators: q Rapid test for hydrophytic vegetation 5 X Dominance test is>50% g X Prevalence index is 53.0" 7 Morphogical adaptations'(provide g supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation' 100 =Total Cover (explain) Woodv vine stratum (Plot size: ) 'Indicators of hydric soil and weuand hydrology must be � present,unless disturbed or problematic 2 y fOp �IC 0 =Total Cover vegetation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 2-3 UP Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type' Loc" Texture Remarks 0-24 10YR 2/1 100 CLAY 24-30 10 YR 3/1 100 CLAY 30-38 2.5 Y 5/2 98 10YR 4/6 2 C M CLAY 'Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. `*Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) _Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark SurFace(F7) "Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Oepth(inches): emarks: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired;check all that a�nlv) Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(B13) Surface Soil Cracks(B6) High Water Tabie(A2) True Aquatic Plants(B14) Drainage Patterns(810) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(61) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(B2) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(63) Presence of Reduced Iron(C4) Stunted or SVessed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(B5) (C6) _FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(67) Thin Muck SurFace(C7) Sparsely Vegetated Concave Surface(B8) Gauge or Well Data(D9) Water-Stained Leaves(B9) Other(Explain in Remarks) fe d Observations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No —C�Depth(inches): hydrology present? N (inGudes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located —two feet higher than 2-3 WET. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM -Midwest Region ProjecUSite 200 Stubbs Bay Rd. City/Counry: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 2-3 WET Investigator(s): NM 3ection,Township,Range: S32,T118N,R23W Landform(hillslope>terrace,etc.): Depression Local relief(concave,convex,none): Concave Slope(%): 0 Lat: Long: Datum: Soil Map Unit NameCordova loam VWI Classification: PF01/EMCd Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? Y Indicators of wetland hydrology present? Y f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) Wetland boundary flagged based on changes in vegetation community as you move upslope. VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 2 (A) 2 Total Number of Dominant 3 Species Across all Strata: 2 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 100.00% (A/B) 0 =Total Cover Sa�lina/Shrub straturr (Plot size: ) Prevalence Index Worksheet 1 Fraxinus pennsylvanica 30 Y FACW Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 130 x 2= 260 q FAC species 0 x 3= 0 5 FACU species 0 x 4= 0 30 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 130 (A) 260 (B) 1 Phalaris arundinacea 100 Y FACW Prevalence Index=B/A= 2.00 2 3 Hydrophytic Vegetation Indicators: q Rapid test for hydrophytic vegetation 5 X Dominance test is>50% g X Prevalence index is 53.0' 7 Morphogical adaptations*(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation' 100 =Total Cover (explain) Woodv vine stratum (Plot size: ) •Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover �e9etation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 2-3 WET Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type* Loc** Texture Remarks 0-28 10YR 2/1 100 CLAY 28-36 10 YR 6/1 98 10YR 5/6 2 C M SANDY CLAY "Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. '"Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed MaVix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) _Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) `Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emarks: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired:check all that aqalv) Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(613) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(614) Drainage Patterns(B10) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(61) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(62) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(63) Presence of Reduced Iron(C4) Stunted or SVessed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils X Geomorphic Position(D2) Iron Deposits(85) (C6) X FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(B7) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(B8) Gauge or Well Data(D9) Water-Stained Leaves(B9) Other(Explain in Remarks) Fiel bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes �— No Depth(inches): —�� hydrology present? Y (inGudes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emarks: US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM -Midwest Region ProjecUSite 200 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: 3-1 UP Investigator(s): NM 3ection,Township,Range: S32,T118W,R23W Landform(hillslope,terrace,etc.): Slight hillslope Local relief(concave,convex,none): none Slope(%): 1 to 2 Lat: Long: Datum: Soil Map Unit NameLe Sueur loam VWI Classification: None Are climatic/hydrologic conditions of the site rypical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significanUy disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? N Hydric soil present? Y Is the sampled area within a wetland? N Indicators of wetland hydrology present? N f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 1 (A) 2 Total Number of Dominant 3 Species Across all Strata: 2 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 50.00% (A/B) 0 =Total Cover Saalino/Shrub sVaturr (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 0 x 2= 0 4 FAC species 25 x 3= 75 5 FACU species 75 x 4= 300 0 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 100 (A) 375 (B) 1 Bromus inermis 70 Y FACU Prevalence Index=B/A= 3.75 2 Poa pratensis 25 Y FAC 3 Cirsium arvense 5 N FACU Hydrophytic Vegetation Indicators: q Rapid test for hydrophytic vegetation 5 Dominance test is>50% g Prevalence index is 53.0* 7 Morphogical adaptations*(provide 8 supporting data in Remarks or on a g separate sheet) �p Problematic hydrophytic vegetation* 100 =Total Cover (explain) WOOdV VinB St�atum (PIOt SiZe: ) 'Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover �e9etation present? N Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 3-1 UP Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type" Loc*` Texture Remarks 0-20 10YR 2/1 100 CLAY 20-28 10 YR 3!1 95 10YR 3/4 5 C M CLAY 28-36 2.5 YR 5/1 95 10YR 4/6 5 C M CLAY "Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. *'Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed MaVix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) SVatified Layers(A5) Loamy Gleyed MaVix(F2) _Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) •Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emarks: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired:check all that aanlv) Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(B13) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(B10) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(B2) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(B3) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils Geomorphic PosiUon(D2) Iron Deposits(B5) (C6) _FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(B7) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(B8) Gauge or Well Data(D9) Water-Stained Leaves(69) Other(Explain in Remarks) iel bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No —C�Depth(inches): hydrology present? N (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located—two feet higher in elevation than 3-1 WET. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM-Midwest Region Project/Site 200 Stubbs Bay Rd. City/Counry: Orono/Hennepin Sampling Date: 10/15/2014 Applicant/Owner: Chris Bollis State: Minnesota Sampling Point: 3-1 WET Investigator(s): NM 3ection,Township,Range: S32,T118N,R23W Landform(hillslope,terrace,etc.): Depression/swale Local relief(concave,convex,none): Concave Slope(%): 0 Lat: Long: Datum: Soil Map Unit Name Le Sueur loam VWI Classification: None Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? Y Indicators of wetland hydrology present? Y f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 1 (A) 2 Total Number of Dominant 3 Species Across all Strata: 1 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 100.00% (A/B) 0 =Total Cover Sa�linca/Shrub straturr (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 1 x 1 = 1 3 FACW species 99 x 2= 198 4 FAC species 0 x 3= 0 5 FACU species 0 x 4= 0 0 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 100 (A) 199 (B) 1 Phalaris arundinacea 99 Y FACW Prevalence Index=B/A= 1.99 2 Scirpus atrovirens 1 N OBL 3 Hydrophytic Vegetation Indicators: 4 Rapid test for hydrophytic vegetation 5 X Dominance test is>50% g X Prevalence index is<_3.0" 7 Morphogical adaptations*(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation* 100 =Total Cover (explain) Woodv vine stratum (Plot size: ) 'Indicators of hydric soil and wetland hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover vegetation present? Y Remarks:(Inciude photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 3-1 WET Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) °/a Type* Loc"" Texture Remarks 0-24 10YR 2/1 100 CLAY 2430 10 YR 4/1 90 10YR 4/6 10 C M CLAY `Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. "Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) Other(explain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark SurFace(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) "Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emar s: Upper part of soil profile moist, not saturated. � HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired;check all that aoolvl Secondar Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(B13) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(610) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(81) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(B2) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(B3) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(64) Recent Iron Reduction in Tilled Soils �Geomorphic Position(D2) Iron Deposits(65) (C6) X FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(67) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(B8) Gauge or Well Data(D9) Water-Stained Leaves(B9) Other(Explain in Remarks) Field bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No —C�Depth(inches): hydrology present? Y (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Sample located in depressional swale. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM -Midwest Region ProjecUSite 200 Stubbs Bay Rd. City/Counry: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: A-1 UP Investigator(s): NM 3ection,Township,Range: 32S,T118N,R23W Landform(hillslope,terrace,etc.): Slight hillslope Local relief(concave,convex,none): none Slope(%): 1 to 2 Lat: Long: Datum: Soil Map Unit NameLester loam VWI Classification: None Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (if needed,explain any answers in remarks.) Hydrophytic vegetation present? N Hydric soil present? Y Is the sampled area within a wetland? N Indicators of wetland hydrology present? N f yes,optional weUand site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species � that are OBL,FACW,or FAC: 1 (A) 2 Total Number of Dominant 3 Species Across all Strata: 2 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 50.00% (A/B) 0 =Total Cover Sa�lina/Shrub straturr (Plot size: ) Prevalence Index Worksheet � Total%Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 10 x 2= 20 4 FAC species 50 x 3= 150 5 FACU species 40 x 4= 160 0 =Total Cover UPL species 0 x 5= 0 Herb sVatum (Plot size: ) Column totals 100 (A) 330 (B) 1 Poa pratensis 50 Y FAC Prevalence Index=B/A= 3.30 2 Bromus inermis 20 Y FACU 3 Solidago canadensis 10 N FACU Hydrophytic Vegetation Indicators: 4 Cirsium arvense 10 N FACU Rapid test for hydrophytic vegetation 5 Phalaris arundinacea 10 N FACW Dominance test is>50% g Prevalence index is 53.0* � Morphogical adaptations"(provide 8 supporting data in Remarks or on a g separate sheet) 10 Problematic hydrophytic vegetation" 100 =Total Cover (explain) WOOdV vine Stratum (PIOt SIZe: ) "Indicators of hydric soil and weUand hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover vegetation present? N Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: A-1 UP Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type' Loci' Texture Remarks 0-16 10YR 2/1 100 CLAY 16-24 10 YR 5/1 SO 10YR 4/4 20 C M SANDY CLAY "Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. "Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed MaVix(F2) Other(explain in remarks) 2 cm Muck(A10) Depleted MaVix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) 'Indicators of hydrophytic vegetation and weitand Sandy Mucky Mineral(S1) Redox Depressions(FS) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): � emarks: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired:check all that a�olv) Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(B13) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(610) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots Crayfish Burrows(C8) Sediment Deposits(62) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(B3) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(B4) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(B5) (C6) FAC-Neutral Test(D5) Inundation Visibie on Aeriai Imagery(B7) Thin Muck Surface(C7) Sparsely Vegetated Concave SurFace(68) Gauge or Well Data(D9) Water-Stained Leaves(69) Other(Explain in Remarks) Field bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No —$�Depth(inches): hydrology present? N (inGudes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located—one foot higher than 1-3 WET. US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM -Midwest Region ProjecUSite 200 Stubbs Bay Rd. City/County: Orono/Hennepin Sampling Date: 10/15/2014 ApplicanUOwner: Chris Bollis State: Minnesota Sampling Point: A-1 WET Investigator(s): NM 3ection,Township,Range: S32,T118N,R23W Landform(hillslope,terrace,etc.): Depression Local relief(concave,convex,none): Concave Slope(%): 0 Lat: Long: Datum: Soil Map Unit NameLester loam VWI Classification: None Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation ,soil ,or hydrology significantly disturbed? Are"normal circumstances" Are vegetation ,soil ,or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? Y Indicators of wetland hydrology present? Y f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) Wetland boundary flagged based on changes in vegetation community as you move upslope. VEGETATION--Use scientific names of plants. Absolute Dominan Indicator pominance Test Worksheet Tree Stratum (Plot size: ) %Cover t Species Staus Number of Dominant Species 1 Acer saccharinum 20 Y FACW that are OBL,FACW,or FAC: 2 (A) 2 Total Number of Dominant 3 Species Across all Strata: 2 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 100.00% (A/B) 20 =Total Cover Saolina/Shrub straturr (Plot size: ) Prevalence Index Worksheet � Total°/a Cover of: 2 OBL species 0 x 1 = 0 3 FACW species 120 x 2= 240 q FAC species 0 x 3= 0 5 FACU species 0 x 4= 0 0 =Tota1 Cover UPL species 0 x 5= 0 Herb stratum (Plot size: ) Column totals 120 (A) 240 (B) 1 Phalaris arundinacea 100 Y FACW Prevalence Index=B/A= 2.00 2 3 Hydrophytic Vegetation Indicators: 4 Rapid test for hydrophytic vegetation 5 X Dominance test is>50% g X Prevalence index is 53.0* 7 Morphogical adaptations"(provide g supporting data in Remarks or on a g separate sheet) �p Problematic hydrophytic vegetation' 100 =Total Cover (explain) WOOdV vine St�BtUm (PIOt SiZe: ) "Indicators of hydric soil and weUand hydrology must be � present,unless disturbed or problematic 2 y rop ytic 0 =Total Cover �e9etation present? Y Remarks:(Include photo numbers here or on a separate sheet) Wetland area in weeds and Silver maple canopy cover with Canada wood nettle, scattered sedge sp.and Blue joint grass understory. US Amy Corps of Engineers Midwest Region SOIL Sampling Point: A-1 WET Profile Description: (Describe to the depth needed to document the indicator or conflrm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type' Loc"* Texture Remarks 0-20 10YR 2/1 100 CLAY 20-28 10 YR 5/1 80 10YR 4/6 20 C M SANDY CLAY "Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. "'Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(A1) Sandy Gleyed Matrix(S4) Coast Prairie Redox(A16)(LRR K,L,R) Histic Epipedon(A2) Sandy Redox(S5) Dark Surface(S7)(LRR K,L) Black Histic(A3) Stripped Matrix(S6) Iron-Manganese Masses(F12)(LRR K,L,R) Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Very Shallow Dark Surface(TF12) Stratified Layers(A5) Loamy Gleyed Matrix(F2) _Other(exp�ain in remarks) 2 cm Muck(A10) Depleted Matrix(F3) Depleted Below Dark Surface(A11) Redox Dark Surface(F6) X Thick Dark Surface(Al2) Depleted Dark Surface(F7) *Indicators of hydrophytic vegetation and weltand Sandy Mucky Mineral(S1) Redox Depressions(F8) hydrology must be present,unless disturbed or 5 cm Mucky Peat or Peat(S3) probiematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): emar s: HYDROLOGY Wetland Hydrology Indicators: Primarv Indicators(minimum of one is reauired:check all that aoolvl Seconda Indicators minimum of two re uired Surface Water(A1) Aquatic Fauna(B13) Surface Soil Cracks(B6) High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(610) Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on living Roots Crayfish Burrows(CS) Sediment Deposits(62) (C3) Saturation Visible on Aerial Imagery(C9) Drift Deposits(B3) Presence of Reduced Iron(C4) Stunted or Stressed Plants(D1) Algal Mat or Crust(64) Recent Iron Reduction in Tilled Soils �Geomorphic Position(D2) Iron Deposits(65) (C6) �FAC-NeuVal Test(D5) Inundation Visible on Aerial Imagery(67) Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(B8) Gauge or Well Data(D9) Water-Stained Leaves(69) Other(Explain in Remarks) ield bservations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No —$�Depth(inches): hydrology present? Y (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: emar s: Located within saddle at top of shallow ravine. US Army Corps of Engineers Midwest Region THE TECHNICAL DOCUMENTATION SECTION Plant Indicator Status INDICATOR CATEGORIES* Obligate Wetland (OBL)—Occur almost always (estimated probability>99%)under natural conditions in wetlands. Facultative Wetland (FACV�—Usually occur in wetlands (estimated probability 67%-99%), but occasionally found in non-wetlands. Facultative(FAC)—Equally likely to occur in wetlands or non-wetlands (estimated probability 34%-66%). Facultative Upland(FACU)—Usually occur in non-wetlands (estimated probabiliry 67%- 99%),but occasionally found in wetlands (estimated probabiliry 1%-33%). Obligate Upland(UPL)—Occur in wetlands in another region,but occur almost always (estimated probabiliry>99%)under natural conditions in non-wetlands in the region specified. If a species does not occur in wetlands in any region, it is not on the National List. *Reed, P.B. 1988. National list of plant species that occur in wetlands: Minnesota. National Wetlands Inventory, U.S. Fish and Wildlife Service, St. Petersburg,Florida. THE TECHNICAL DOCUMENTATION SECTION Soil Series Descriptions Acquired from Natural Resource Conservation Service Website,Official Soil Series Descriptions CORDOVA SERIES The Cordova series consists of very deep,poorly drained soils that formed mostly in loamy calcareous glacial till on ground moraines and till plains.The upper part of the profile in some of these soils formed in modified glacial till.These soils have moderately slow permeability.Their slopes are less than 2 percent. Mean annual precipitation is about 28 inches.Mean annual temperature is about 48 degrees F. TAXONOMIC CLASS: Fine-loamy,mixed, superactive,mesic Typic Argiaquolls TYPICAL PEDON: Cordova clay loam with a plane slope of 1 percent in a cultivated field. (Colors are for moist soil unless otherwise stated.) Ap--O to 10 inches; black(N 2/0)clay loam,very dark gray(lOYR 3/1)dry; moderate medium subangular blocky structure; friable; about 1 percent gravel; neutral; abrupt wavy boundary. A--10 to 18 inches; black(N 2/0)clay loam, very dark gray(lOYR 3/1)dry; moderate medium subangular blocky structure; friable; about 1 percent gravel; neutral; clear wavy boundary. (Combined A horizon is 8 to 20 inches.) Btgl--18 to 30 inches; olive gray(SY 4/2) clay loam; few fine prominent dark yellowish brown(l 0YR 4/6) Fe concentrations; moderate medium angular blocky structure parting to moderate fine angular blocky; friable; common very dark gray(SY 3/1)clay films on faces of peds and in pores; about 3 percent gravel; neutral; clear wavy boundary. Btg2--30 to 38 inches; olive gray(SY 5/2)clay loam; common fine prominent dark yellowish brown(lOYR 4/6)Fe concentrations; weak medium subangular blocky structure; friable; few distinct very dark gray(SY 3/1) clay films on faces of peds and in pores; about 3 percent gravel; neutral; abrupt wavy boundary. (Combined Btg horizon is 12 to 40 inches thick.) C--38 to 80 inches; light olive gray(SY 6/2) loam; common medium prominent yellowish brown(lOYR 5/6)Fe concentrations; massive; friable; about 5 percent gravel; strongly effervescent; slightly alkaline. TYPE LOCATION: Waseca County, Minnesota; about 5 miles north of Waseca; 550 feet south and 1100 feet east of the northwest corner of Sec. 22, T.108N., R.22W.; USGS Morristown quadrangle; lat. 44 degrees 8 minutes 32 seconds N. and long. 93 degrees 27 minutes 45 seconds W.,NAD27. RANGE IN CHARACTERISTICS: Depth to free carbonates ranges from 24 to 50 inches. Thickness of the mollic epipedon ranges from 10 to 24 inches. Rock fragment content is 2 to 6 percent throughout and is of mixed lithology,but some pedons have less than 2 percent in the upper part. The A horizons are neutral to moderately acid. The B horizons range from strongly acid to slightly alkaline. The Ap or A horizon has hue of lOYR, 2.SY or is neutral,value of 2 or 3 and chroma of 0 or 1. It is loam, silty clay loam,or clay loam. Eluviation is evident in some pedons by a few porous coatings on the faces of peds in the lower A and/or upper B horiozns. Some pedons have AB horizons. The Btg horizon has a matrix with hue of lOYR to SY, value of 3 to 5, value of 3 is only in the upper part, and chroma of 1 or 2. Some pedons have a BA horizon. The B horizon typically is silty clay loam or clay loam but ranges to loam in the lower part. The upper 20 inches of the argillic horizon averages between 28 to 35 percent clay and exceeds 15 percent fine sand and coarser. The B/A clay ratios range from 1.2 to 1.4. A Bk horizon is present in some pedons. The C horizon has a matrix with SY or 2.SY hue, value of 4 to 6, and chroma of 2 to 4. It is loam or clay loam and is slightly alkaline ar moderately alkaline. COMPETING SERIES: These are the Barry, Bei���ille, Brookston, Buntin�;ville, Clackamas, Ha�ncl, Jameston, Maren��o, Millgrove, Navan, Nosoni, Renssel��cr, and Westland series. Barry soils have less than 27 percent clay in the control section. Berville soils contain more than 6 percent gravel in the control section. Brookston soils are more moist in the soil moisture control section during the 120 days following the summer solstice and have less montmorillonite in the lower part of the series control section. Buntingville, Clackmas, and Nosoni soils are drier in the soil moisture control secrion during the 120 days following the summer solstice. Hamel soils have A horizons 16 to 27 inches thick and and chroma of 1 or less in the upper B horizons. Jameston soils have very firm till beginning at depths ranging from 18 to 30 inches. Marengo soils typically have thicker sola, contain appreciable amounts of sedimentary rock fragments in the silty clay lower B and C horizons, and are more moist in the soil moisture control section. Millgrove soils have up to 15 percent gravel in the upper part and 7 percent or mare in the lower part of the control section and very poorly drained.. Navan soils have than 35 percent more clay in the lower B and C horizons. Rensselaer soils have reaction greater than 6.1 in the upper part of the control section, are more moist in the moisture control section and are poorly drained. Westland soils have 7 percent or more gravel in the lower part of the control section. GEOGRAPHIC SETTING: The Cordova soils have slightly concave to slightly convex slopes on broad flat ridge tops in rolling moraine areas or on lower lying areas in ground moraines and till plains. Slope gradients are 0 to 2 percent. Soils formed mostly in friable, calcareous, loamy till of Late Wisconsinan age. However, the upper part of the sola in some pedons is from modified glacial till or drift. The mean annual temperature is about 45 to 52 degrees F. Mean annual precipitation is about 26 to 32 inches. GEOGRAPHICALLY ASSOCIATED SOILS: The main ones are the Dundas, Lester, and Lc Sucur soils. These soils formed in materials similar to those of the Cordova soils and are members of a hydrosequence with the Cordova soils. The well drained Lester soils are on nearby undulating to hilly slopes. The moderately well to somewhat poorly drained Le Sueur and the somewhat poorly to poorly drained Dundas soils are on nearby higher positions. The poorly drained Webster and Hamcl soils and the very poorly drained Glencoe soils are a nearby associate in a few places. DRAINAGE AND PERMEABILITY: Poorly drained. Surface runoff is low. Permeability is moderately slow. USE AND VEGETATION: Most of the soil is cleared, drained and cropped to corn and soybeans. A few areas remain in woodlots or permanent pasture.Native vegetation was northern hardwoods, largely basswood,maple, and elm, and an understory of grasses and sedges. DISTRIBUTION AND EXTENT: South-central Minnesota and north-central Iowa. Extensive. MLRA OFFICE RESPONSIBLE: St. Paul,Minnesota SERIES ESTABLISHED: Waseca County, Minnesota, 1963. REMARKS: Diagnostic horizons and features recognized are: Mollic epipedon from 0 to 18 inches (Ap and AB horizons); argillic horizon from 18 to 38 inches(Btgl and Btg2 horizons); aquic moisture regime - low chroma with redox features beneath the mollic epipedon. ADDITIONAL DATA: Refer to pedon 69 MN-7-11 for results of some laboratory analysis of the typical pedon of this series. GLENCOE SERIES The Glencoe series consists of very deep,very poorly drained soils that formed in loamy sediments from glacial till on glacial moraines.These soils have moderate or moderately slow permeability.Slopes are 0 to 1 percent.Mean annual precipitation is about 28 inches.Mean annual temperature is about 48 degrees F. TAXONONIIC CLASS: Fine-loamy, mixed, superactive,mesic Cumulic Endoaquolls TYPICAL PEDON: Glencoe clay loam with a concave slope of less than 1 percent in a depression on a ground moraine in cultivated field. (Colors are for moist soil unless otherwise noted.) Ap--O to 10 inches;black(N 2/0)clay loam; massive; friable; about 2 percent gravel; ' cloddy; neutral; abrupt smooth boundary. A--10 to 24 inches;black(N 2/0)clay loam; weak fine subangular blocky structure; friable; about 2 percent gravel; neutral; clear wavy boundary. (Combined thickness of A horizon is 16 to 32 inches.) ABg--24 to 35 inches; very dark gray(SY 3/1) clay loam; weak fine subangular blocky structure; friable; few tongues of dark olive gray(SY 3/2)and olive gray(SY 4/2); about 2 percent gravel; neutral; gradual irregular boundary. (0 to 26 inches thick) Bg--35 to 48 inches; olive gray(SY 4/2)loam; moderate coarse subangular blocky structure; friable: few tongues of very dark gray(SY 3/1); about 5 percent gravel; common fine prominent light olive brown(2.SY 5/4)and common medium prominent strong brown(7.SYR 5/6) Fe concentrations; neutral; gradual wavy boundary. (0 to 30 inches thick) Cg--48 to 60 inches; grayish brown(2.SY 5/2) loam; massive; friable; about 5 percent gravel; many medium distinct light olive brown(2.SY 5/4) Fe concentrations; strongly effervescent; slightly alkaline. TYPE LOCATION: Steele County, Minnesota; about 5 miles northwest of Owatonna; 2,640 feet south, 2,660 feet west of the northeast corner of sec. 24,T. 108 N., R. 21 W.; USGS Medford West quadrangle; lat. 44 degrees 8 minutes 46 seconds N. and long. 93 degrees 17 minutes 45 seconds W.,NAD27. RANGE IN CHARACTERISTICS: Depth to free carbonates is 30 to 60 inches or more. The Ap in a few pedons will have small amounts of free carbonates. The thickness of the mollic epipedon ranges from 24 to 80 inches. The control section averages between 22 and 35 percent clay and from 15 to 30 percent fine sand and coarser. Rock fragments of mixed lithology comprise 0 to 5 percent of the volume of the A and B horizons and 2 to 8 percent of the C horizon. Some pedons have an 0 horizon up to 6 inches in thickness. A stratified substratum phase is recognized with silt loam, sand, sandy loam, and loamy sand textures below 40inches. The Ap or A horizon has hue of lOYR to SY or neutral,value of 2 or 3, and chroma of 0 or l. It is clay loam, silty clay loam,or loam with 25 to 35 percent clay. Ponded phases may have mucky modifiers. It is commonly neutral but ranges from slightly alkaline to slightly acid. AB horizon has colors and textures similar to the A and Bg horizons. The Bg horizon has hue of SY or 2.SY, value of 2 to 5, and chroma of 1 or 2. Dark colored tongues from the A horizon range from few to common. It is loam, clay loam or silty clay loam. Near the center of some depressions, some pedons have B horizons that have a slight clay increase relative to the A horizons. It is neutral to slightly alkaline, but in some pedons the lower part of the B horizon is slightly alkaline with slight effervescence. The Bg horizon is absent in some pedons. The Cg horizon has hue of SY or 2.SY, value of 4 to 6, and chroma of 1 to 4. It is loam, clay loam or silty clay loam. It is slightly alkaline, with weak or strong effervescence. Calcium carbonate segregations are present in some pedons. COMPETING SERIES: These are the Coland, Comfi�ev, Delft, Gielo���, James Canyon, Kcddie, Kimmerlin��, Kc�nner, McCla�e, Peoh, Ronulell, Shandet�, and Wcnas series. Coland and Comfrey soils do not have rock fragments in their control sections. In addition, Coland soils are deeper to free carbonates. Delft soils are poorly drained, are not in closed depressions, have prismatic structure in subsoil, and do not have tongues of the A horizon in the Bg horizon. Gielow, James Canyon, Keddie, Kimmerling, Konner, McClave, Peoh, and Wenas soils are drier in the soil moisture control section during the 120 days following the summer solstice. Romnell soils contain appreciable amounts of gypsum in their sola. Shandep soils do not have tongues of A horizon in the Bg horizon and have a coarse textured 2C horizon. GEOGRAPHIC SETTING: Glencoe soils typically are in closed depressions or low gradient swales within the Des Moines lobe of the Late Wisconsinan glaciation. The Glencoe soils are formed in loamy colluvial sediments and loamy glacial till. Mean annual temperature ranges from 45 to 52 degrees F. Mean annual precipitation ranges from 25 to 32 inches. The frost free days range from 124 to 172. The elevation above sea level range from 700 to 1600 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Canisteo, Clai-ion, Harr�s, I�icollet, and �'��ebster soils. The well drained Clarion soils are on the sloping uplands. Somewhat poorly drained Nicollet and the poorly drained Canisteo, Webster, and Harps soils are on nearly level to gently undulating slopes. All the above have mollic epipedons less than 24 inches thick. In addition, the Canisteo and Harps soils contain free carbonates throughout. The Glencoe soils also are associated with the Havden and Lester soils and their respective topographic associates in some places. DRAINAGE AND PERMEABILITY: Very poorly drained. Surface runoff is negligible. Permeability is moderate or moderately slow. USE AND VEGETATION: Mostly drained and cropped to corn and soybeans.Native vegetation was a wet site plant community of the tall grass prairie plant formation. DISTRIBUTION AND EXTENT: South-central Minnesota and possibly north- central Iowa. Large extent. MLRA OFFICE RESPONSIBLE: St. Paul, Minnesota SERIES ESTABLISHED: Dakota County, Minnesota, 1945. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon-the zone from the surface to a depth of 35 inches(Ap,A, and ABg horizons); cumulic subgroup-mollic epipedon is more than 24 inches thick; aquic moisture regime- low chroma immediately below the A horizons. HAMEL SERIES The Hamel series consists of very deep,poorly drained and somewhat poorly drained soils that formed in slope colluvium and glacial till on moraines.These soils have moderately slow permeability.Their slopes range from 1 to 4 percent.Mean annual precipitation is about 28 inches.Mean annual air temperature is about 47 degrees F. TAXONOMIC CLASS: Fine-loamy,mixed, superactive,mesic Typic Argiaquolls TYPICAL PEDON: Hamel loam with a 2 percent concave slope on a glacial moraine in a cultivated field. (Colors are for moist soil unless otherwise noted.) Ap--O to 10 inches; black(lOYR 2/1) loam,very dark brown(lOYR 2/2)dry; weak very fine subangular blocky structure; friable; common very fine roots; about 1 percent gravel; neutral; abrupt smooth boundary. A--10 to 16 inches;black(lOYR 2/1) loam, very dark gray(lOYR 3/1)dry; weak very fine subangular blocky structure; friable; common very fine roots; about 4 percent gravel; neutral; gradual smooth boundary. (Combined thickness of A horizon is 14 to 30 inches.) AB--16 to 24 inches; very dark gray(l 0YR 3/1)clay loam, dark grayish brown(l 0YR 4/2)dry; many fine prominent brown(7.SYR 4/4)Fe concentrations; moderate fine angular blocky structure; friable; common very fine roots; about 4 percent gravel; neutral; gradual wavy boundary. (0 to 10 inches thick.) Btgl--24 to 40 inches; very dark grayish brown(2.SY 3/2) clay loam, grayish brown (lOYR 5/2) dry; many fine prominent brown(7.SYR 4/4)Fe concentrations; moderate medium prismatic structure; friable; few black(l 0YR 2/1)clay films on faces of peds; about 5 percent gravel; neutral; gradual wavy boundary. Btg2--40 to 46 inches; dark grayish brown(2.SY 4/2) clay loam; many coarse prominent brown(7.SYR 4/4) Fe concentrations; moderate medium subangular blocky structure; friable; few black(lOYR 2/1)clay films on faces of peds; about 4 percent gravel; neutral; clear wavy boundary. (Combined thickness of Btg horizons is 12 to 30 inches.) Cg1--46 to 55 inches; olive gray(SY 5/2) loam; many medium prominent yellowish brown(lOYR 5/6)Fe concentrations; massive; friable; about 3 percent gravel; slightly effervescent; slightly alkaline; gradual wavy boundary. Cg2--55 to 80 inches; olive gray(SY 5/2) loam; many medium prominent yellowish brown(lOYR 5/6) Fe concentrations; massive; friable; about 4 percent gravel; slightly effervescent; slightly alkaline. TYPE LOCATION: Wright County,Minnesota; about 1.5 miles southwest of Silver Creek, 1200 feet south and 2300 feet west of the northeast corner of Sec. 18,T.121 N., R.26 W., USGS Annandale quadrangle; lat. 45 degrees 17 minutes 34 seconds N.; long. 94 degrees 00 minutes 13 seconds W.,NAD27 RANGE IN CHARACTERISTICS: Depth to free carbonates range from 30 to 65 inches. The mollic epipedon thickness ranges from 24 to 60 inches. Typically the upper colluvim contains less than 2 percent gravel by volume and the lower part contains 2 to 6 percent gravel by volume of mixed lithology. The A horizons have hue of lOYR or is neutral, value of 2 or 3, and chroma of 0 to 2. Typically it is loam or clay loam, but silt loam or silty clay loam are within the range. It has coatings of clean sand and silt particles in the lower part of the A horizon in some pedons. It is moderately acid to neutral. The Btg horizon has hue of lOYR, 2.SY, or SY, value of 2 to 4, and chroma of 1 or 2. It is clay loam, silty clay loam high in sand, or loam. It has between 25 and 35 percent clay and 15 to 35 percent fine sand and coarser. It has B/A clay ratios of 1.2 to 1.4. It has few to many, faint to prominent clay films. It is moderately acid to neutral. The C horizon has hue of a 2.SY or SY, value of 4 to 6, chroma of 1 or 2. It is loam or clay loam. It is slightly alkaline or moderately alkaline. The clay content ranges from 18 to 32 percent and the total sand content ranges from 25 to 45 percent. COMPETING SERIES: These are the Alvada, Barrv, Berville, Brookston, Buntin��ville, Clach��mas, Cordova, Forestcity, Jameston, Maren�o, Mill�rove,Navan, Nosoni, Rensselaec, and Westland soils. The Alvada series (Tentative - OH) is not in the OSD file at this time. The Barry, Berville, Brookston, Cordova, Marengo, Millgrove, Navan, Rensselaer, and Westland soils have a mollic epipedon that is less than 24 inches thick. The Buntingville soils have carbonates at depths of less than 20 inches. The Clackamas and Nosoni soils lack free carbonates in the series control section. The Forestcity soils have 45 to 65 percent sand and 10 to 18 percent clay in the underlying material. The Jamesto��m soils formed in a firm and very firm till associated with the Iowan Erosional surface. GEOGRAPHIC SETTING: Hamel soils have concave slopes in swales, rims of closed depressions, foot and toe slopes, and upper drainageways below sloping to very steep slopes. Slope gradients are 1 to 4 percent. Hamel soils formed in slope colluvium and glacial till of Late Wisconsinan Age. Mean annual air temperature is about 45 to 48 degrees F. Mean annual precipitation is about 25 to 30 inches. Frost free days range from 125 to 165. Elevation above sea level ranges from 700 to 1600 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are principally the Havdcn and Lester soils. These soils are well drained and are on the higher lying, gently sloping to very steep slopes. DRAINAGE AND PERMEABILITY: Poorly drained and somewhat poorly drained. Surface runoff is low or moderately low. Permeability is moderately slow. The apparent seasonal high water table is at .5 to 1.5 feet for the poorly drained phase and 1.5 to 2.5 feet for the somewhat poorly drained phase during spring in normal years. USE AND VEGETATION: Most of this soil is cropped to corn, hay, soybeans, and small grains. However, significant areas are in pasture and forest. Native vegetation is mixed wet prairie grasses and deciduous forest. DISTRIBUTION AND EXTENT: Primarily in the southeast one-quarter of Minnesota in the timbered,hilly, "gray" till region. Moderately extensive. MLRA OFFICE RESPONSIBLE: St. Paul,Minnesota SERIES ESTABLISHED: Hennepin County, Minnesota, 1969. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon-the zone from the surface to a depth of 40 inches(Ap,A,AB and Btgl); argillic horizon-the zone from 24 to 46 inches(Btgl,Btg2,). Type location moved from Hennepin County, Mn. to Wright County,Mn., 11/96 to better exemplify the series concept. A somewhat poorly drained overwash phase is recognized that has 8 to 20 inches of colluvium over the original dark colored surface. ADDITIONAL DATA: Refer to MAES Central File Code No. 785 for results of some laboratory analysis of this series. LE SUEUR SERIES The Le Sueur series consists of very deep,somewhat poorly drained soils that formed in calcareous loamy glacial till on moraines.These soils have moderate permeability.Their slopes range from 1 to 3 percent. Mean annual precipitation is about 29 inches.Mean annual air temperature is about 47 degrees F. TAXONOMIC CLASS: Fine-loamy,mixed, superactive,mesic Aquic Argiudolls TYPICAL PEDON: Le Sueur clay loam with a 2 percent plane slope on glacial till plain in a pastured woodlot. (Colors are for moist soil unless otherwise noted.) Ap--O to 12 inches; black(lOYR 2/1) clay loam, dark grayish brown(lOYR 4/2) dry; moderate medium granular blocky structure parting to moderate fine subangular; friable; about 2 percent gravel; slightly acid; abrupt smooth boundary. (6 to 12 inches thick) AB--12 to 17 inches; very dark gray(lOYR 3/1) and about 25 percent dark yellowish brown(lOYR 4/4)clay loam, grayish brown(lOYR 5/2)dry; moderate fine subangular blocky structure; friable; about 2 percent gravel; slightly acid; clear smooth boundary. (0 to 8 inches thick) Bt1--17 to 24 inches; olive brown(2.SY 4/3)clay loam; moderate medium prismatic structure parting to strong fine subangular blocky; friable; common dark brown(lOYR 3/3)clay films on faces of peds; about 2 percent gravel; few fine faint dark grayish brown (2.SY 4/2) Fe depletions; slightly acid; clear smooth boundary. Bt2--24 to 37 inches; olive brown(2.SY 4/3) clay loam; weak medium prismatic structure parting to moderate fine subangular blocky; friable; common very dark grayish brown(2.SY 3/2)clay films on faces of peds and in pores; about 4 percent gravel; few fine faint grayish brown(2.SY 5/2) Fe depletions and few fine prominent dark yellowish brown(lOYR 4/6) Fe concentrations; neutral; abrupt smooth boundary. (Combined thickness of the Bt horizon is 16 to 45 inches.) Bk--37 to 46 inches; light olive brown(2.SY 5/4) loam; weak medium subangular blocky structure; friable;common light gray pale brown(2.SY 7/2) soft masses of carboante throughout and carbonate tl�reads; about 5 percent gravel; common medium distinct grayish brown(2.SY 5/2) Fe depletions and common medium distinct light olive brown (2.SY 5/6) Fe concentrations; strongly effervescent; slightly alkaline; clear smooth boundary. C--46 to 80 inches; grayish brown(2.SY 5/2) loam; weak medium subangular blocky structure parting to massive; friable; common light gray pale brown(2.SY 7/2) soft masses of carbonate throughout and carbonate threads; about 5 percent gravel; many common medium prominent dark yellowish brown(lOYR 4/4) and dark yellowish brown (lOYR 4/6) Fe concentrations; strongly effervescent; slightly alkaline. TYPE LOCATION: Waseca County, Minnesota; about 9 miles south of Waseca; 2000 feet south and 1950 feet south of northwest corner of sec. 26, T. 108 N., R. 22 W.; USGS Morrisontown quadrangle; lat. 44 degrees 7 minutes 57 seconds N. and long. 93 degrees 26 minutes 45 seconds W.,NAD27. RANGE IN CHARACTERISTICS: Depth to free carbonates ranges from 22 to 55 inches. The thickness of the mollic epipedon ranges from 10 to 18 inches. Rock fragment content is 1 to 8 percent by volume throughout and is of mixed lithology. The A horizon has hue of lOYR, value of 2 or 3, and chroma of 1 or 2. The A horizon is clay loam, loam, silt loam, or silty clay loam. It has 20 to 30 percent clay. It is moderately acid to neutral. An E horizon as much as 3 inches thick is in some pedons. The AB horizon has characteristics similar to the A and the Bt. The upper part of the Bt horizon has hue of lOYR or 2.SY, value of 3 to 5, and chroma of 2 or 3. The lower part of the Bt horizon has a hue of 2.SY, value of 4 or 5, and chroma of 2 to 4. The Bt horizon is mostly clay loam or loam. The argillic horizon averages between 24 and 35 percent clay and from 15 to 40 percent fine sand or coarser. The Bt horizon is strongly acid to slightly acid in the upper part and strongly acid to neutral in the lower part. The bulk density ranges from 1.30 to 1.45 gm/cc. Some pedons have a BC or Bk horizon. The C horizon has hue of 2.SY or SY, value of 4 to 6, and chroma of 2 to 4. It is loam or clay loam. It is slightly alkaline or moderately alkaline. The bulk density ranges from 1.45 to 1.60 gm/cc. COMPETING SERIES: These are the Andres, Aurand(T), Aztalan, Crane, Dai-�-och, Gilbe�a, Houstcnader(T), La Ho�ue, Marcellon, Mokcila, Nachusa, Nenno, Newhaven, ndell, Protivin, Tiderishi, Vi�ar, and Wil�ner series. The Aurand(T) and Tiderishi series are presently not in the OSD file. The Andres, Aztalan, and Mokena soils have silty clay loam lower B and C horizons. Aztalan soils also have hue of 7.SYR in the B and C horizons. Crane soils have more than 8 percent rock fragments in the lower part of the argillic horizon. Darroch soils have C horizons of stratified silty and sandy sediments within the series control section. Gilboa soils have silt loam and silty clay loam in the upper part of the series control section. Houstenader soils have 30 to 40 percent gravel in the lower third of the series control section. La Hogue soils have less than 20 percent clay in the lower part of the series control section. Marcellon soils have less than 24 percent clay in the argillic horizon. Nachusa soils do not have rock fragments in the upper part of the series control section. Nenno soils have more than 8 percent rock fragments in the lower part of the series control section. Newhaven soils do not have free carbonates in the series control section. Odell soils have hue of lOYR in the lower B and C horizons and higher chroma in the upper B horizon. Protivin soils have bulk density greater than 1.60 gm/cc in the lower part of the series control section. Vigar soils have a mollic epipedon greater than 24 inches thick. Wilmer soils have more than 40 percent fine sand or coarser in the argillic horizon. GEOGRAPHIC SETTING: The Le Sueur soils have slightly concave,plane, or slightly convex slopes on moraines within the Des Moines lobe and Grantsburg sublobe of the Late Wisconsin glaciation. They formed in a calcareous, loamy till. Slopes range from 1 to 3 percent. Mean annual air temperature ranges from 45 to 52 degrees F. Mean annual precipitation ranges from 25 to 32 inches. Frost-free days range from 125 to 165. Elevation above sea level ranges from 700 to 1600 feet. GEOGRAPHICALLY ASSOCIATED SOILS: The main ones are the Cordo�a, Lester, and Hamcl soils. These soils formed in materials similar to the I,e Sueur soils and are members of a hydrosequence with the Le Sueur soils. The poorly drained Cordova and Hamel soils are common associates on adjacent nearly level slopes. The well drained Lester soils are the most common associate on the undulating to gently undulating slopes. The well drained Havden soils and the poorly drained Dundas soils are associates in some places. DRAINAGE AND PERMEABILITY: Somewhat poorly drained. Surface runoff is low. Permeability is moderate. An apparent water table is at 1.5 to 2.5 feet during November to June in most years. USE AND VEGETATION: Mostly under cultivation with corn, soybeans, grain, and hay the principal crops. Native vegetation was deciduous forest, dominantly elm, basswood, and maple in some areas, and oak with prairie and brush understory in the timber outliers within the prairie. DISTRIBUTION AND EXTENT: South-central Minnesota and north-central Iowa. This soil is extensive. MLRA OFFICE RESPONSIBLE: St. Paul, Minnesota SERIES ESTABLISHED: Le Sueur County, Minnesota, 1944. REMARKS: Diagnostic horizons and features recognized in this pedon are: mollic epipedon-the zone from the surface to 13 inches (A and AB horizons); argillic horizon- the zone from 13 to 41 inches (Bt horizons); aquic subgroup-hue of lOYR and chroma of 2 immediately below mollic epipedon. Somewhat poorly drained matches depth to redox (2 chroma at 17 inches) and taxonomic class (Aquic subgroup) closer than the previous moderately well drained class. LESTER SERIES The Lester series consists of very deep,well drained soils that formed in calcazeous loamy glacial till on till plains and moraines.These soils have moderate permeability.Their slopes range from 5 to 70 percent. Mean annual precipitation is about 28 inches.Mean annual temperature is about 47 degrees F. TAXONOMIC CLASS: Fine-loamy,mixed, superactive, mesic Mollic Hapludalfs TYPICAL PEDON: Lester loam with a convex slope of about 9 percent on a ground moraine in a cultivated field. (Colors are for moist soil unless otherwise noted.) Ap--O to 7 inches; very dark grayish brown(lOYR 3/2) loam, grayish brown(lOYR 5/2) dry; moderate fine subangular blocky structure; friable; many fine roots; about 3 percent gravel; slightly acid; abrupt smooth boundary. (6 to 10 inches thick) Btl--7 to 21 inches; brown(lOYR 4/3)clay loam; moderate medium subangular blocky structure; firm; many very fine roots; common very dark grayish brown(lOYR 3/2)clay films on faces of peds and few very dark gray(lOYR 3/1) organic coats on faces of peds; about 2 percent gravel; slightly acid; clear smooth boundary. Bt2--21 to 38 inches; dark yellowish brown(lOYR 4/4)clay loam; moderate medium subangular blocky structure; friable; common fine roots; common dark grayish brown (lOYR 4/2)clay films on faces of peds and few very dark brown(lOYR 2/2)organic coats on faces of peds; about 3 percent gravel; slightly acid; gradual smooth boundary. (Combined Bt horizon is 10 to 40 inches.) Bk1--38 to 50 inches; yellowish brown(lOYR 5/4) loam; weak medium subangular blocky structure; friable; few fine roots; common very pale brown(lOYR 8/2)carbonate threads; about 2 percent gavel; violently effervescent; slightly alkaline; clear wavy boundary. Bk2--50 to 60 inches; yellowish brown(lOYR 5/4)loam; weak medium subangular blocky structure; friable; common fine distinct yellowish brown(l 0YR 5/6)relict Fe concentrations; common very pale brown(lOYR 8/2)carbonate threads; about 2 percent gravel; violently effervescent; slightly alkaline; clear wavy boundary. C--60 to 80 inches; yellowish brown(lOYR 5/4)loam; ; massive; friable; common medium distinct yellowish brown(l 0YR 5/6)relict Fe concentrations and few fine distinct light brownish gray(lOYR 6/2)relict Fe depletions; about 1 percent gravel; strongly effervescent; slightly alkaline. TYPE LOCATION: Wright County, Minnesota; about 3 miles west of Otsego, 1460 feet south and 200 feet west of the northeast corner of Sec. 15, T.121 N., R.24 W.; USGS Big Lake quadrangle; lat. 45 degrees 17 minutes 29 seconds N.; long. 93 degrees 41 minutes 3 seconds W.,NAD27 RANGE IN CHARACTERISTICS: Depth to free carbonates ranges from 20 to 54 inches. Rock fragments of mixed lithology comprise 1 to 8 percent of the volume of the control section. The A or Ap horizons have hue of l OYR, value of 2 or 3, and chroma of 1 or 2. The E horizon where present, has value of 3 to 5, and chroma of 1 to 3. The A and E horizons are loam or clay loam, but sandy loam, fine sandy loam, or silt loam is within the range. They range from moderately acid to neutral. The Bt horizon has hue of 1 OYR or 2.SY, value of 4 or 5, and chroma of 3 or 4. It is clay loam or loam and has 24 to 35 percent clay and 30 to 45 percent sand. The B/A clay ratios range from 1.2 to 1.4. It is strongly acid to slightly acid in the upper part and moderately acid to neutral in the lower part. A Bw horizon is sometimes present below the Bt. The Bk horizon has hue of lOYR or 2.SYR, value of 4 or 5, and chroma of 3 to 6. The Bk horizon is loam or clay loam. It is slightly alkaline or moderately alkaline. Relict redoximorphic features are present in some pedons. The C horizon has hue of 2.SY or lOYR, value of 4 to 6, and chroma of 3 to 6. It is loam or clay loam. It is slightly alkaline or moderately alkaline. Relict redoximorphic features are present in some pedons. COMPETING SERIES: These are the A�, Ar�vle, Baltimore, Bassett, Bloomin�;, Caleb, Dowa�;iac, Dunbrid�e, Gara, Koronis, Lauramie, Lon lg ois, L�k, Mohawk, Neda, Ne���coiner, Oneco, Orwood, Racine, Razort, Sebbo, Tao�i, Waucoma, and ��'inneshick soils in the same family. Angus and Sebbo soil have saturation in the lower third of the series control section. Argyle, Baltimore, and Oneco soils have B horizons with 7.SYR or redder hue. Bassett soils are very strongly acid to moderately acid in the upper part of the Bt horizon. Blooming and Racine soils have 15 to 35 percent sand in the upper part of the particle-size control section. Caleb soils have some subhorizons that have more than 45 percent in the lower part of the control section. Dowagiac and Koronis soils have less than 24 percent clay in the lower one third of the particle-size control section. Dunbridge, Waucoma,Newcomer and Winneshiek soils have sola terminated by bedrock at depths above 60 inches. Gara soils average less than 2 percent rock fragments in the control section. Longlois, Lydic, and Neda soils have more than 8 percent rock fragments in some subhorizon of the control section. Lauramie soils have more than 45 percent sand in some subhorizon in the middle part of the control section. Mohawk soils have a higher content of silt and have dark colors in the B horizon which apparently are inherited from dark shale. Orwood soils have no rock fragments in the particle-size control section. Razort soils have less than 30 percent sand in the control section. GEOGRAPHIC SETTING: These soils have convex slopes on moraines and till plains. Slope gradients range from 5 to 70 percent. They formed in calcareous, loamy glacial till of late Wisconsinan Age. Mean annual temperature ranges from 45 degrees to 52 degrees F. Mean annual precipitation ranges from 25 to 33 inches. Frost free days range from 125 to 165. Elevations range from 700 to 1600 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These include the Cordova, Dundas, Glencoc, Hamel, Hou�llton, Klossner, Le Sueur, Muske�o, and Nessel soils. Poorly drained Cordova and somewhat poorly and poorly drained Dundas soils are on flats and upper drainageways with a high seasonal water table. Very poorly drained Glencoe, Houghton,Klossner, and Muskego soils are mostly in depressions. Poorly drained Hamel soils are on foot and toe slopes. Moderately well drained Le Sueur and Nessel soils are on slightly elevated flats and gently convex slopes. DRAINAGE AND PERMEABILITY: Well drained. Permeability is moderate. Runoff is medium to high. USE AND VEGETATION: Mostly cropped to corn and soybeans. Some is in pasture and forest.Native vegetation is savanna. DISTRIBUTION AND EXTENT: South-central and east-central Minnesota and northeastern Iowa. Extensive. MLRA OFFICE RESPONSIBLE: St. Paul, Minnesota SERIES ESTABLISHED: Dakota County,Minnesota, 1945. REMARKS: Diagnostic horizons and featured recognized in this pedon are: mollic subgroup-the zone from the surface to 7 inches(Ap horizon); argillic horizon-the zone from 7 to 38 inches(Bt horizons). Type locarion moved from Waseca County, Mn. to Wright County, Mn., 11/96 to better exemplify the series concept within the MLRA. 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