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Wetland Classification, Identification, and
Delineation Report
Prepared for:
Lillian Stubbs
By:
Svoboda Ecological Resources
Project Number 2014-030-03
October 21, 2014
T'he contents and format of this report are considered intellectual property and
are subject to copyright restrictions and may not be reproduced without
the express permission of Svoboda Ecological Resources.
Table of Contents
ABSTRACT.................................................................................................................................................1
INTRODUCTION.......................................................................................................................................1
METHODS..................................................................................................................................................1
RESULTS.....................................................................................................................................................2
DISCUSSION..............................................................................................................................................4
RECOMMENDATIONS............................................................................................................................4
CERTIFICATION......................................................................................................................................5
DATASOURCES........................................................................................................................................6
LITERATURE REFERENCED................................................................................................................7
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 10/9/14 to examine the
site for the presence of areas meeting wetland criteria. The study parcel is located in the ciry of Orono,
MN in Hennepin County (Figure 1). Two wetland boundaries were delineated at this site. Two sample
transects were established (one each) along the northeastern boundary of the wetland area on the
northwest end of the property and one along the northwestern side of the wetland on the south side of
the property in order to characterize the soil, vegetation, and existing hydrology within the wetland-to-
upland transition zone. One other area was examined for the presence of wetland indicators and the area
was determined to be non-wetland.
INTRODUCTION
The subject parcel at 185 Old Crystal Bay Rd is approximately 9.8 acres in size. The parcel is
dominated by a rolling topography, with a mix of woodlands and open grassy areas. The east half of the
property is dominated by open parking space, industrial structures and equipment associated with a
house moving enterprise where the domestic/commercial structure is present. The surrounding land use
is primarily widely to closely-spaced single family homes to the south and east and widely-spaced
homes interspersed with wetlands to the northwest. 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 less 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 Council 1995). T'he 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
Svoboda Ecological Resources 185 Old Crystal Bay Road
2014-030-03 1 Lillian Stubbs
wetland boundaries." "...This Regional Supplement is designed for use with the current
version of the Corps Manual (Environmental Laboratory ]987) 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. http://wetland plants.usace.armumi/�.
RESULTS
The National Wetland Inventory does not indicate any wetlands in the survey area (Figure 2a). The
HCWI indicates the presence of one probable wetland in the survey area (Figure 2b) on the far western
end of the parcel. The DNR NWI update in 2014, like the original NWI also does not indicate any
wetlands in the survey area(Figure 2c).
The Web Soil Survey of Hennepin County (Figure 3) identifies four soil map units present on the
subject property. They are as follows: Hamel-Glencoe, depressional, complex; Angus loam, morainic;
Shorewood silty clay loam; and Lester loam, morainic, eroded. The Hamel-Glencoe soil is
predominantly hydric while the remaining types are predominantly nonhydric. Soil series descriptions
are provided in the Technical Documents section.
The Minnesota Department of Natural Resources, State Protected Waters Map (Public Waters
Inventory) indicates no public waters within the study area (Figure 4).
Site Visit
SER ecologists examined the subject property for areas meeting jurisdictional wetland criteria during
the site visit. Two area meeting the jurisdictional criteria of a wetland were flagged on 10/06/14 and
boundaries were determined and delineated. Field data was collected on 10/09/14. The approximate
wetland boundaries are outlined in yellow (Figures 5 and 6). Additionally one other area, on the west
side of the property, was examined for wetland indicators.
Svoboda Ecological Resources 185 Old Crystal Bay Road
2014-030-03 2 Lillian Stubbs
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 12, 2014, was 7.16" above normal. Precipitation for the period 10/06/14 to
10/12/14 was reported to be 0.58" below normal and for the preceding 4 weeks was 0.51" below
normal.
The 2014 DNR NWI update does not identify the wetland on the west side of the property. The HCWI
indicates the presence of a probable wetland in the area. The wetland is a wet meadow dominated by
emergent herbaceous vegetation on one side and surrounded by woodland. We would classify this
wetland as PEM1A in the NWI Cowardin classification system (Eggers and Reed Classification— Wet
Meadow; Circular 39 Type 2). Vegetation in the seasonally inundated wetland was dominated by reed
canarygrass (Phalaris arundinacea FACV�. Transition to uplands is marked by slope and increased
woody vegetation.
Transect SP 1-1 was taken from the northeastern boundary of the wetland. The soils at sample point SP
1-1 Wet consisted of a dark loam layer at the surface with clay loams beneath. Hydric indicators F6
(Redox Dark Surface) and F8 (Redox Depressions) were present. The soils at sample point SP 1-1 Up
consisted of a dark loam at the surface with lighter-colored sandy loam layers below. No hydric
indicators were present at this sample point.
At sample point SP 1-1 Wet secondary hydrology indicators D2 (Geomorphic Position) and DS (FAC-
Neutral Test) were present. Wetland hydrology was not indicated at sample point SP 1-1 Up with only
one secondary indicator, DS (FAC-Neutral Test).
Wetland 2 is also not indicated by the NWI, nor is it by the HCWI. The wetland is a depressional wet
meadow lying in the lowest part of the parcel along the southern boundary. We would classify this
wetland as PEM1A in the NWI Cowardin classification system (Eggers and Reed Classification— Wet
Meadow; Circular 39 Type 2). Vegetation in the seasonally inundated wetland was dominated by reed
canarygrass (Phalaris arundinacea FACV�. Transition to uplands is marked by slope and loss of reed
canarygrass.
Transect SP 2-1 was taken from the northwestern boundary of the wetland. The soils at sample point SP
2-1 Wet consisted of dark loam clays at the surface and a depleted clay matrix below Hydric indicators
F6 (Redox Dark Surface) and Al2 (Thick Dark Surface) were present. The soils at sample point SP 2-1
Up consisted of loam layers. No hydric indicators were present at this sample point.
At sample point SP 2-1 Wet secondary hydrology indicators D2 (Geomorphic Position) and DS (FAC
Neutral)were present. Wetland hydrology was not indicated at sample point SP 2-1 Up.
A third area, labeled Area A, was examined to determine if it met wetland requirements. The area is just
south and slightly upslope of Wetland 1. There were some wetland species present, a small amount of
reed canarygrass mixed in with the bluegrass. However, at sample point SP A, the soil consisted of a
lighter-colored loam and was not found to be hydric. Wetland hydrology was not indicated, either.
Detailed soils, vegetation, and hydrology data for the delineated jurisdictional wetlands are provided in
the data sheets of the Technical Documents section.
Svoboda Ecological Resources 185 Old Crystal Bay Road
2014-030-03 3 Lillian Stubbs
DISCUSSION
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 10/06/14 and field data were
collected on 10/09/14.
SER personnel examined the subject properties for areas meeting jurisdictional wetland criteria during
the site visit and delineated the edges of two wetlands as being jurisdictional wetlands (Figures 5 and
6). One potential wetland area (Area A) was examined and determined to lack the required wetland
indicators. Detailed soils, vegetation and hydrology data is 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.
i* State jurisdiction by the Wetland Conservation Act of 1991 (WCA) administered by the WCA
Local Governmental Unit(LGU).
2* 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 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 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 permit 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 Ecologicai Resources 185 Old Crystal Bay Road
2014-030-03 4 Lillian Stubbs
CERTIFICATION
Frank Svoboda completed the flagging of the wetland boundaries on 10/06/2014 and David Remucal
collected sample data on 10/09/2014. 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. T'he 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 10/21/14. The
delineation report was reviewed by Frank Svoboda, President of Svoboda Ecological Resources.
Client: Lillian Stubbs
Project Name: 185 Old Crystal Bay Rd
Project No.: 2014-030
Location: Orono, MN
� "
David Remucal, Wetland Ecologist
�-�°�--- d.
President, Svoboda Ecological Resources
October 21, 2014
Date
Svoboda Ecological Resources 185 Old Crystal Bay Road
2014-030-03 5 Lillian Stubbs
DATA SOURCES
Minnesota Department 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 5/28/12.
2012 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 185 Old Crystal Bay Road
2014-030-03 6 Lillian Stubbs
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. 201 L Wetland Plants and Plant Communities of Minnesota and
Wisconsin, Third Edition. US Army Corps of Engineers, St. Paul District. 478pp, 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.
Lichvar, R.W., M. Butterwick,N.C. Melvin, and WN. Kirchner. 2014.
The National Wetland Plant List: 2014 Update of Wetland Ratings.
Phytoneuron 2014-41: 1-42. httn://wetland plants.usace.armv.miU
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 185 Old Crystal Bay Road
2014-030-03 7 Lillian Stubbs
FIGURES
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Partiall h d�ic ��, � , � � ,.:-�,�' �� ,� � 3. .��� �;� y �.� �� ,�' � .
Y Y � �.,� � r < �,< � ��,�� � ;� � r ;�
� ��' �,�,��~ �,������°����is� -� �7�"`"� ��"�'� �� �✓ �� «
�� /w�� w > � �' � �� �' � � r. �� '� ,y.�� y;� �y�%�:
Predominantly hydric �;� '�� �� � �` ,;�f. ,
� � ,. • • ' � r a . ! � � e •-
,• � � �
Predominantly nonhydric '� � � '' `` �''� s =� °� � '-��
� •- : �- � `� �' �
� � � ' � s . � • � � ,� �� � �
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./ ` " . .� �
�_____ _ �����c�l.c�.c�`'!�`' . . .�A .,�_��'�.. �_ _ .. __�; � � . '� .,t��_ �'' _ �..�(_.
_.__.. ._._ __ � �
TIIgN �3w s33 Approximate Wetland Boundary and Soils Figure 6
Overlaid on 2012 Aerial Photo
.��-��►SVOBC�DA zoi4-o3o
0 175 350 700 185 Old Crystal Bay Road
�� �� Ecoloszical Resources FPP�
THE TECHNICAL DOCUMENTATION SECTION
Field Data Sheets
WETLAND DETERMINATION DATA FORM -Midwest Region
Project/Site 185 Old Crystal Bay Rd City/County: Orono/Hennepin Sampling Date: 10/9/14
ApplicanUOwner: Lillian Stubbs State: MN Sampling Point: SP 1-1 Up
Investigator(s): FJS, DR 3ection,Township, Range: T118N R23W S33
Landform(hillslope,terrace,etc.): slope Local relief(concave,convex, none): none
Slope(%): 1-2 Lat: Long: Datum: NAD83
Soil Map Unit Name Hamel-Glencoe,depressional, complex,0 to 3 percent slopes VWI Classification: none
Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarics)
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 remarics.)
Hydrophytic vegetation present? Y
Hydric soil present? N Is the sampled area within a weUan� N
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: 30' ) %Cover t Species Staus Number of Dominant Species
1 Acer negundo 30 Y FACW that are OBL,FACW,or FAC: 4 (A)
2 Rhamnus cathartica 10 Y FAC Total Number of Dominant
3 Species Across all Strata: 4 (B)
4 Percent of Dominant Species
5 that are OBL,FACW,or FAC: 100.00% (A/B)
40 =Total Cover
Saplinq/Shrub straturr (Plot size: 15' ) Prevalence Index Worksheet
1 Rhamnus cathartica 40 Y FAC Total%Cover of:
2 OBL species 0 x 1 = 0
3 FACW species 30 x 2= 60
4 FAC species 130 x 3= 390
5 FACU species 0 x 4= 0
40 =Total Cover UPL species 0 x 5= 0
Herb stratum (Plot size: 5' ) Column totals 160 (A) 450 (B)
1 Rhamnus cathartica 80 Y FAC Prevalence Index=B/A= 2.81
2
3 Hydrophytic Vegetation Indicators:
4 Rapid test for hydrophytic vegetation
5 X Dominance test is>50%
6 X Prevalence index is 53.0'
� Morphogical adaptations*(provide
8 supporting data in Remarks or on a
9 separate sheet)
10 Problematic hydrophytic vegetation"
80 =Total Cover (explain)
WOOdY vi�@ StfBtUm (PIOt SIZB: 30' ) *Indicators of hydric soil and wetland hydrology must be
� present,unless disturbed or problematic
2 y rop yt c
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: SP 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
0-3 10YR 3/1 100 Loam
3-7 10YR 3/2 85 10YR 6/2 15 D PL/M Sandy loam redox in soft masses
7-24 10YR 3/2 40 10YR 6/2 10 D M Sandy loam
7-24 10YR 2/1 20 10YR 4/2 30 D M Sandy loam
*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) 5 cm Mucky Peat or Peat(S3)(LRR K,L,R)
Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Iron-Manganese Masses(F12)(LRR K,L,R)
Stratified Layers(A5) Loamy Gleyed Matrix(F2) Very Shallow Dark Surface(TF12)
2 cm Muck(A10) Depleted Matrix(F3) Other(explain in remarks)
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(F8) 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):
Remarks:
HYDROLOGY
WeUand Hydrology Indicators:
Primarv Indicators(minimum of one is reauired:check all that applv) 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(B1) Oxidized Rhizospheres on Living Roots Cra�sh 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) �C 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(B9) Other(Explain in Remarks)
ie d bservations:
Surface water present? Yes No X Depth(inches): Wetland
Water table present? Yes No X Depth(inches): hydrology
Saturation present? Yes No X Depth(inches): present? N
(includes capillary fringe)
Describe recorded data(stream gauge, monitoring well, aerial photos, previous inspections), if available:
Remarks:
US Army Corps of Engineers Midwest Region
WETLAND DETERMINATION DATA FORM -Midwest Region
Project/Site 185 Old Crystal Bay Rd City/County: Orono/Hennepin Sampling Date: 10/9/14
ApplicanUOwner: Lillian Stubbs State: MN Sampling Point: SP 1-1 Wet
Investigator(s): FJS, DR 3ection,Township, Range: T118N R23W S33
Landform(hillslope,terrace,etc.): depression Local relief(concave,convex, none): concave
Slope(%): 0 Lat: Long: Datum: NAD83
Soil Map Unit Name Hamel-Glencoe,depressional,complex,0 to 3 percent slopes 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 remarics.)
Hydrophytic vegetation present? Y
Hydric soil present? Y Is the sampled area within a wetlan� Y
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: 30' ) %Cover t Species Staus Number of Dominant Species
1 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
Saolina/Shrub straturc (Plot size: 15' ) Prevalence Index Worksheet
1 Total%Cover of:
2 OBL species 5 x 1 = 5
3 FACW species 95 x 2= 190
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: 5' ) Column totals 100 (A) 195 (B)
1 Phalaris arundinacea 90 Y FACW Prevalence Index=B/A= 1.95
2 Eupatorium maculatum 5 N OBL
3 Solidago gigantea 5 N FACW Hydrophytic Vegetation Indicators:
4 Rapid test for hydrophytic vegetation
5 X Dominance test is>50%
6 X Prevalence index is 53.0*
� Morphogical adaptations"(provide
8 supporting data in Remarks or on a
9 separate sheet)
10 Problematic hydrophytic vegetation*
100 =Total Cover (explain)
Woodv vine stratum (PIOt SIZe: 30' ) •Indicators of hydric soil and weUand hydrology must be
1 present,unless disturbed or problematic
2 y rop yt�c
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: SP 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
0-7 10YR 2/1 90 2.5Y 5/3 10 C PL Loam clay
7-15 10YR 2/1 97 10YR 3/4 3 C PUM Clay loam redox in soft masses
15-24 10YR 2/1 80 10YR 6/2 20 D PUM Clay loam redox in sand soft masses
*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) 5 cm Mucky Peat or Peat(S3)(LRR K,L,R)
Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Iron-Manganese Masses(F12)(LRR K,L,R)
Stratified Layers(A5) Loamy Gleyed Matrix(F2) Very Shallow Dark Surface(TF12)
2 cm Muck(A10) Depleted Matrix(F3) Other(explain in remarks)
Depleted Below Daric Surface(A11) X Redox Dark Surface(F6)
Thidc Dark Surface(Al2) Depleted Dark Surface(F7) *Indicators of hydrophytic vegetation and weltand
Sandy Mudcy Mineral(S1) X 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):
Remarks:
HYDROLOGY
Wetland Hydrology Indicators:
Primarv Indicators(minimum of one is reauired;chedc all that applv) Seconda Indicators minimum of two re uired
Surtace Water(A1) Aquatic Fauna(B13) Surface Soil Cracks(B6)
High Water Table(A2) True Aquatic Plants(614) Drainage Patterns(B10)
Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season WaterTable(C2)
Water Marks(B1) Oxidized Rhizospheres on Living Roots Cra�sh 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 X Geomorphic Position(D2)
Iron Deposits(65) (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(69) Other(Explain in Remarks)
ie d bservations:
Surface water present? Yes No X Depth(inches): Wetland
Water table present? Yes No X Depth(inches): hydrology
Saturation present? Yes No X Depth(inches): 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
Project/Site 185 Old Crystal Bay Rd City/County: Orono/Hennepin Sampling Date: 10/9/14
ApplicanUOwner: Lillian Stubbs State: MN Sampling Point: SP 2-1 Up
Investigator(s): FJS, DR 3ection,Township, Range: T118N R23W S33
Landform(hillslope,terrace,etc.): hillslope Local relief(concave, convex, none): none
Slope(%): 2-3 Lat: Long: Datum: NAD83
Soil Map Unit NameShorewood silty clay loam,3 to 6 percent slopes VWI Classification: none
Are climatiGhydrologic 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? N Is the sampled area within a wetlarn N
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: 30' ) %Cover t Species Staus Number of Dominant Species
1 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
Saalina/Shrub straturc (Plot size: 15' ) Prevalence Index Worksheet
1 Total%Cover of:
2 OBL species 0 x 1 = 0
3 FACW species 30 x 2= 60
4 FAC species 40 x 3= 120
5 FACU species 30 x 4= 120
0 =Total Cover UPL species 0 x 5= 0
Herb stratum (Plot size: 5' ) Column totals 100 (A) 300 (B)
1 Poa pratensis 40 Y FAC Prevalence Index=B/A= 3.00
2 Phalaris arundinacea 30 Y FACW
3 Taraxacum o�cinale 20 Y FACU Hydrophytic Vegetation Indicators:
4 Glechoma hederacea 10 N FACU Rapid test for hydrophytic vegetation
5 X Dominance test is>50%
6 X Prevalence index is 53.0*
� Morphogical adaptations*(provide
8 supporting data in Remarks or on a
9 separate sheet)
10 Problematic hydrophytic vegetation'
100 =Total Cover (explain)
Woodv vine stratum (PIOt SiZe: 30' ) •Indicators of hydric soil and wetland hydrology must be
1 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: SP 2-1 Up
Pro�le Description: (Describe to the depth needed to document the indicator or confirtn the absence of indicators.)
Depth Matrix Redox Features
(Inches) Color(moist) % Color(moist) % Type* Loc*' Texture Remarks
0-6 10YR 3/2 97 10YR 3/3 3 C PL Loam
6-24 10YR 3/1 98 10YR 3/2 2 PL Loam
*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)
Bladc Histic(A3) Stripped Matrix(S6) 5 cm Mucky Peat or Peat(S3)(LRR K,L,R)
Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Iron-Manganese Masses(F12)(LRR K,L,R)
Stratified Layers(A5) Loamy Gleyed Matrix(F2) Very Shallow Dark Surface(TF12)
2 cm Muck(A10) Depleted Matrix(F3) Other(explain in remarks)
Depleted Below Dark Surface(A11) Redox Daric Surface(F6)
Thick Dark Surface(Al2) Depleted Daric 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? N
Depth(inches):
emarks:
HYDROLOGY
WeUand Hydrology Indicators:
Primarv Indicators(minimum of one is reauired:check all that ao�lvl 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(B1) Oxidized Rhizospheres on Living Roots Cra�sh 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(64) 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)
ie servations:
Surface water present? Yes No X Depth(inches): WeUand
Water table present? Yes No X Depth(inches): hydrology
Saturation present? Yes No X Depth(inches): present? N
(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 185 Old Crystal Bay Rd City/County: Orono/Hennepin Sampling Date: 10/9/14
ApplicanUOwner: Lillian Stubbs State: MN Sampling Point: SP 2-1 Wet
Investigator(s): FJS, DR 3ection,Township, Range: T118N R23W S33
Landform(hillsiope,terrace,etc.): depression Local relief(concave,convex, none): concave
Slope(%): 0 Lat: Long: Datum:
Soil Map Unit Name Shorewood silty clay loam,3 to 6 percent slopes VWI Classification: none
Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarics)
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 weUarn Y
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: 30' ) %Cover t Species Staus Number of Dominant Species
1 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: 15' ) Prevalence Index Worksheet
1 Total%Cover of:
2 OBL species 0 x 1 = 0
3 FACW species 70 x 2= 140
4 FAC species 30 x 3= 90
5 FACU species 0 x 4= 0
0 =Total Cover UPL species 0 x 5= 0
Herb stratum (Plot size: 5' ) Column totals 100 (A) 230 (B)
1 Phalaris arundinacea 70 Y FACW Prevalence Index=B/A= 2.30
2 Poa pratensis 30 Y FAC
3 Hydrophytic Vegetation Indicators:
4 Rapid test for hydrophytic vegetation
5 X Dominance test is>50%
6 X Prevalence index is 53.0"
� Morphogical adaptations*(provide
8 supporting data in Remarks or on a
9 separate sheet)
10 Problematic hydrophytic vegetation*
100 =Total Cover (explain)
Woodv vine stratum (Plot size: 30' ) *Indicators of hydric soil and weUand hydrology must be
1 present,unless disturbed or problematic
2 y rop yt�c
0 =Total Cover vegetation
present7 Y
Remarks:(Include photo numbers here or on a separate sheet)
US Amy Corps of Engineers Midwest Region
SOIL Sampling Point: SP 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
0-5 10YR 2/1 100 Loam clay
5-21 10YR 2/1 90 10YR 6/1 5 D PL Loam clay
5-21 10YR 3/3 5 C PL Loam clay
21-28 10YR 6/2 90 Clay
21-28 10YR 2/1 10
*Type: C=Concentration, D=Depletion, RM=Reduced Matrix, MS=Masked Sand Grains. **Location: PL=Pore Lining, M=Matrix
Hydric Soil Indicators: Indicators for Problematic Hydrlc 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) 5 cm Mucky Peat or Peat(S3)(LRR K,L,R)
Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Iron-Manganese Masses(F12)(LRR K,L,R)
Stratified Layers(A5) Loamy Gleyed Matrix(F2) Very Shallow Dark Surface(TF12)
2 cm Muck(A10) Depleted Matrix(F3) Other(explain in remarks)
Depleted Below Dark Surface(A11) X Redox Dark Surface(F6)
X Thidc 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 aaplv) Secondan Indicators minimum of two re uired
Surface Water(A1) Aquatic Fauna(B13) Surface Soil Cradcs(66)
High Water Table(A2) True Aquatic Plants(B14) Drainage Patterns(670)
Saturation(A3) Hydrogen Sulfide Odor(C1) Dry-Season Water Table(C2)
Water Marks(61) Oxidized Rhizospheres on Living Roots Cra�sh 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 X Geomorphic Position(D2)
Iron Deposits(65) (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(69) Other(Explain in Remarks)
ield servat ons:
Surface water present? Yes No X Depth(inches): Wetland
Water table present? Yes No X Depth(inches): hydrology
Saturation present? Yes No X Depth(inches): present� Y
(includes capillary fringe)
Describe recorded data(stream gauge, monitoring well,aerial photos,previous inspections), if available:
Remarks:
US Army Corps of Engineers Midwest Region
WETLAND DETERMINATION DATA FORM -Midwest Region
Project/Site 185 Old Crystal Bay Rd City/County: Orono/Hennepin Sampling Date: 10/9/14
ApplicanUOwner: Lillian Stubbs State: MN Sampling Point: SP A
Investigator(s): FJS, DR 5ection,Township, Range: T118N R23W S33
Landform(hillslope,terrace,etc.): hillslope Local relief(concave, convex, none): none
Slope(%): 3-5 Lat: Long: Datum: NAD83
Soil Map Unit Name Hamel-Glencoe,depressional,complex,0 to 3 percent slopes VWI Classification: none
Are climatiGhydrologic 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 weUan� N
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: 30' ) %Cover t Species Staus Number of Dominant Species
1 that are OBL,FACW,or FAC: 1 (A)
Z 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
Saalina/Shrub straturc (Plot size: 15' ) Prevalence Index Worksheet
1 Total%Cover of:
2 OBL species 0 x 1 = 0
3 FACW species 7 x 2= 14
4 FAC species 80 x 3= 240
5 FACU species 13 x 4= 52
0 =Total Cover UPL species 0 x 5= 0
Herb stratum (Plot size: 5' ) Column totals 100 (A) 306 (B)
1 Poa pratensis 80 Y FAC Prevalence Index=B/A= 3.06
2 Cirsium arvense 8 N FACU
3 Fraxinus pennsylvanica 5 N FACW Hydrophytic Vegetation Indicators:
4 G/echoma hederacea 3 N FACU Rapid test for hydrophytic vegetation
5 Taraxacum o�cinale 2 N FACU X Dominance test is>50%
6 Phalaris arundinacea 2 N FACW Prevalence index is<_3.0"
� Morphogical adaptations"(provide
8 supporting data in Remarks or on a
9 separate sheet)
10 Problematic hydrophytic vegetation'
100 =Total Cover (explain)
Woodv vine stratum (PIOt SiZ@: 30' ) *Indicators of hydric soil and wetland hydrology must be
1 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: SP A
Profile Description: (Describe to the depth needed to document the indicator or confrtn the absence of indicators.)
Depth Matrix Redox Features
(Inches) Color(moist) % Color(moist) % Type* Loc** Texture Remarks
0-3 10YR 3/2 90 10YR 6/3 8 C M Loam
0-3 10YR 8/1 2 D PL Loam
3-7 10YR 3/2 60 10YR 6/4 20 C PUM Loam Redox in soft masses
3-7 10YR 2/1 20 Loam
7-11 10YR 2/1 90 10YR 3/4 10 C PUM �oam Redox in soft masses
11-
`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)
Bladc Histic(A3) Stripped Matrix(S6) 5 cm Mucky Peat or Peat(S3)(LRR K,L,R)
Hydrogen Sulfide(A4) Loamy Mucky Mineral(F1) Iron-Manganese Masses(F12)(LRR K,L,R)
Stratified Layers(A5) Loamy Gleyed Matrix(F2) Very Shallow Daric Surface(TF12)
2 cm Muck(A10) Depleted Matrix(F3) Other(explain in remarks)
Depleted Below Dark Surface(A11) Redox Daric Surface(F6)
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):
Remarks:
HYDROLOGY
Wetland Hydrology Indicators:
Primarv Indicators(minimum of one is reauired:check all that a�plv) Seconda Indicators minimum of two re uired
Surface Water(A1) Aquatic Fauna(B13) Surface Soil Cradcs(66)
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 Cra�sh 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(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)
Field bservations:
Surface water present? Yes No X Depth(inches): Wetland
Water table present? Yes No X Depth(inches): hydrology
Saturation present? Yes No X Depth(inches): presentT N
(inGudes capillary fringe)
Describe recorded data(stream gauge, monitoring well,aerial photos, previous inspections), if available:
emarks:
US Army Corps of Engineers Midwest Region
THE TECHNICAL DOCUMENTATION SECTION
P1antIndicator 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 probabi[ity
34% -66%).
Facultative Upland (FACi�—Usually occur in non-wetlands (estimated probability 67%-
99%), but occasionally found in wetlands (estimated probability 1% -33%).
Obligate Upland(UPL)—Occur in wetlands in another region,but occur almost always
(estimated probability >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
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.
TAXONOMIC 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 1. 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, Comfrev, Delft, Gielow, James Can.�,
Keddie, Kimmerlin�, Konner, McClave, Peoh, Romnell, Shandep, and Wenas 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 ti1L 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, Clarion, HarpS,
Nicollet, and Webster 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 Ha•�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.T'heir 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 (lOYR 3/1)clay loam, dark grayish brown(lOYR
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(lOYR 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, Clackamas, Cordova, Forestcitv, Jameston, Maren�o, Mill�rove,Navan,
Nosoni, Rensselaer, 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 Jamestown 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 Ha•�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 farest. 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 Btg 1);
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.
SHOREWOOD SERIES
T'he Shorewood series consists of very deep,moderately well drained and somewhat poorly drained soils
that formed in a mantle of clayey glacial lacustrine sediments and underlying loamy calcareous till or that
formed entirely in lacustrine sediments.These soils are in glacial lake plains and moraines.Permeability is
moderately slow or slow. Slopes range from 0 to 12 percent.Mean annual precipitation is about 28 inches.
Mean annual temperature is about 47 degrees F.
TAXONOMIC CLASS: Fine, smectitic, mesic Aquertic Argiudolls
TYPICAL PEDON: Shorewood silty clay loam with a slightly convex 3 percent slope in
a cultivated field. (Colors are for moist soil unless otherwise noted.)
Ap--O to 8 inches; black (lOYR 2/1) silty clay loam, dark gray (lOYR 4/1) dry; weak
very fine and fine subangular blocky structure; friable; many roots; neutral; abrupt
smooth boundary.
A--8 to 11 inches; black(lOYR 2/1) silty clay loam; weak and moderate very fine and
fine subangular blocky structure; friable; many roots; neutral; clear smooth boundary.
(Combined thickness of A horizons is 8 to 16 inches thick)
AB--11 to 17 inches; very dark gray (lOYR 3/1) grading to very dark grayish brown
(lOYR 3/2) in lower part, silty clay loam, dark gray(lOYR 4/1) dry; moderate very fine
and fine subangular and angular blocky structure; friable; many faint gray (lOYR 5/1)
coatings of clean silt and sand on faces of peds; few roots; slightly acid; clear smooth
boundary. (0 to 10 inches thick)
Bt1--17 to 24 inches; dark grayish brown(lOYR 4/2) silty clay; weak and moderate fine
and medium prismatic structure; firm; many faint very dark grayish brown(lOYR 3/2)
clay films on faces of peds; few distinct light gray (lOYR 6/1) coatings of clean sand and
silt on faces of peds; strongly acid; clear smooth boundary.
Bt2--24 to 33 inches; dark grayish brown(2.SY 4/2) clay; common fine distinct olive
brown(2.SY 4/4) Fe concentrations; weak and moderate medium and coarse prismatic
structure; firm; many faint very dark grayish brown(2.SY 3/2) and few prominent black
(lOYR 2/1) clay films on faces of peds and in root channels; strongly acid; clear smooth
boundary.
Btg--33 to 39 inches; grayish brown(2.SY 5/2) silty clay; common fine distinct light
olive brown(2.SY 5/6) Fe concentrations; weak coarse prismatic structure parting to
weak and moderate fine and very fine subangular blocky; friable; common prominent
black(lOYR 2/1) clay fillings in root channels; slightly effervescent; neutral; clear
smooth boundary. (Combined thickness of the Bt horizon is 18 to 38 inches)
2BCg--39 to 45 inches; grayish brown(2.SY 5/2) clay loam; common fine distinct olive
brown(2.SY 4/4) and light olive brown(2.SY 5/4) Fe concentrations; weak fine
subangular blocky structure; friable; few faint dark grayish brown(2.SY 4/2) and few
prominent black(l 0YR 2/1) clay fillings in root channels; about 3 percent gravel;
strongly effervescent; slightly alkaline; clear smooth boundary.
2Cg--45 to 60 inches; grayish brown(2.SY 5/2) loam; common fine distinct light olive
brown(2.SY 5/6) Fe concentrations; massive with some horizontal cleavages; about 5
percent gravel; strongly effervescent; slightly alkaline.
TYPE LOCATION: Blue Earth County, Minnesota; about 4 miles southeast of
Mankato; 2300 feet east and 100 feet north of the southwest corner of sec. 34, T. 108 N.,
R. 26 W.; USGS Beauford quadrangle; lat. 44 degrees 6 minutes 33 seconds N. and long.
93 degrees 56 minutes 22 seconds W., NAD27.
RANGE IN CHARACTERISTICS: The depth to free carbonates range from 28 to 50
inches. The thickness of the mollic epipedon ranges from 10 to 22 inches. The lacustrine
mantle is 30 or more inches thick. The lacustrine sediments lack or have a trace of rock
fragments. The glacial till has 2 to 8 percent rock fragments by volume of mixed
lithology.
The Ap or A horizon has hue of lOYR, value of 2 or 3 and chroma of 1 or 2. It is silty
clay loam or silty clay. It is moderately acid to neutral. Most pedons have evidence of
eluviation similar to the AB horizon or in the upper part of the Bt horizon. A few pedons
have an indistinct E horizon with value of 3.
The Bt horizon has hue of lOYR or 2.SY, value of 3 to 6 and chroma of 2 to 4. The low
chroma is either a redox feature or the matrix in the upper part of Bt. The upper 20 inches
of the Bt horizon typically averages between 38 and 50 percent clay. B/A clay ratios
range from 1.2 to 1.4. The Bt horizon typically is silty clay loam or silty clay,but, in
some pedons is silt loam at depths below 30 inches. It is neutral to strongly acid.
Some pedons have a loam or clay loam 2BC horizon.
Some pedons have a Bk horizon.
The 2C horizon has hue of 2.SY, value of 5 or 6 and chroma of 2 to 4. It is loam or clay
loam.
Some pedons lack 2C horizons. The profile has formed entirely in lacustrine sediments
that lack rock fragments. It is silt loam, silty clay loam, silty clay, or clay.
COMPETING SERIES: These are the Arisbur�, Arispe, Chase, Flana�an, Greenton,
Grundy, Herrick, Ipava, La�onda, Lamoni, Martin, Mavberry, Pawnee, Rutland,
Sevmour, Tina and W.ymore soils. The Arisburg soils do not have free carbonates in the
lower third of the series control section. The Lagonda and Pawnee soils have sola with a
higher content of sand. The Arispe, Grundy, Herrick, Ipava and Seymour soils have
thicker sola formed in loess. The Chase and Tina soils have thicker mollic epipedons. The
Flanagan soils typically have thicker sola and formed in loess and the underlying till. The
Greenton and Martin soils have their lower B or C horizons formed in residuum from
limestone or shale. Also, the Greenton soils have redder hue in their lower B horizons
and Martin soils have thicker mollic epipedons. The Lamoni soils have thicker sola with
the upper part formed in loess or a mixture of loess and pedisediment and part of the B
horizon is in a paleosol. The Mayberry soils have redder hue. The Rutland soils have
thicker sola and strongly gleyed lower B horizons. The Wymore soils have thicker sola
formed in loess, lack carbonates at depths of less than 40 inches and are on a warmer
climate.
GEOGRAPHIC SETTING: Shorewood soils have plane or slightly convex slopes on
glacial lake plains and moraines. Slopes generally are about 100 to 250 feet in length with
gradients of 0 to 12 percent. The Shorewood soils formed in clayey lacustrine material
commonly 30 to 60 inches or more in thickness over friable loam or clay loam glacial till.
In some pedons a silty layer up to 3 feet thick is between the clayey layer and the
underlying deposits. Mean annual temperature is about 45 to 50 degrees F. Mean annual
precipitation is about 25 to 32 inches. Frost free days range from 124 to 165. Elevations
above sea level range from 900 to 1200 feet.
GEOGRAPHICALLY ASSOCIATED SOILS: These are the Minnetonka, Barbert,
and Lura soils which are members of a hydrosequence with Shorewood soils. Poorly
drained Minnetonka soils are on nearby level terrain. Very poorly drained Barbert and
Lura soils are in depressions and swales.
DRAINAGE AND PERMEABILITY: Moderately well and somewhat poorly drained.
Surface runoff is medium or high. Permeability is moderately slow or slow. The perched
water table for the moderately well drained phase is 2.5 to 4.0 April to June, and 1.5 to
2.5 for the moderately wet phase in most years.
USE AND VEGETATION: Most of this soil is cropped to corn, soybeans, small grains,
and hay. Small acreage is in farest and a few areas are in orchard. Native vegetation
apparently was savanna.
DISTRIBUTION AND EXTENT: South central and southeastern Minnesota.
Inextensive.
MLRA OFFICE RESPONSIBLE: St. Paul, Minnesota
SERIES ESTABLISHED: Hennepin County, Minnesota, 12/5/69.
REMARKS: Diagnostic horizons and features recognized in this pedon are: Mollic
epipedon - the zone from the surface of the soil to 17 inches (Ap, A and AB horizons);
argillic horizon- the zone from 17 to 39 inches (the Btl, Bt2, and Btg harizons); aquertic
subgroup - a LE of 6.0 cm or more from the surface to 100 cm. A moderately wet phase
is also recognized.
ADDITIONAL DATA: See MAES CFC# 968 for data on this pedon.
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Overview wetland 1 — IMG_1766 — View of larger section of wetland showing
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taken facing northwest.
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