My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
04-08-1996 Council Packet
Orono
>
City Council
>
1996
>
04-08-1996 Council Packet
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
12/4/2025 1:27:47 PM
Creation date
8/31/2023 4:24:58 PM
Metadata
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
245
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
nrTABLE 10.-SOILS ClASSIHED ACCORDING TO THE CURRIOT SYSTEM OF CLASSIFICATICN-Continued the <br />tre <br />Series <br />Rasset ........ <br />Seiide.......... <br />Shields U/ <br />Shorewood--* <br />Ziaier«en*- <br />Fasiily 1/ <br />Coerse-loasry» odxed, aesic--* <br />Sandy-skeletel » mixed, mesic- <br />Fine« montmorillonitic, inesic <br />Fine, aontaorillonitic, iiesic <br />Sandy, mixed, frigid ............... <br />Subgroup <br />Typic Argiudolls-- <br />Entic Hapludolls-- <br />Md IU c Albaqualfs- <br />Aquic Argiudolls-- <br />Alfic Udipsanuncnts <br />Order <br />Mollisols. <br />Mollisols. <br />Mollisols. <br />Mollisols. <br />Entisols. <br />Hennepin County has soil temperatures on the border between the mesic and frigid soil ter’.perature <br />classes; therefore, soils in both classes occur in the county. However, these tewpercturc differences are <br />idlior and arc usually not significant to growing crops in the county. <br />These soils are taxadjuncts of the Anoka series because the surface layer is thicker and darker <br />and the sand fraction is dominantly fine sand. <br />3/ <br />These soils are taxadjuncts of the Chaska series because they contain less fine sand than the de <br />fined range for the series. <br />4/ <br />These soils are taxadjuncts of the Dakota series because they have less translocated clay in the B <br />horizon than the defined range for the series. <br />5/ <br />These soils are taxadjuncts of the Dorchester series because they have darker colored upper hori- <br />tons vid contain more sand than the defined range for the series. <br />i/ <br />Some of these soils are taxadjuncts of the Isan series because the C horizon is loam or heavv <br />sandy loam. <br />IJ <br />These soils are taxadjuncts of the Langola series because they have more silt and clay in the solun <br />and some have grayer colors than the defined range for the series. <br />y <br />These soils are taxadjuncts of the Lerdal series because the A horizon is thicker than the defined <br />range for the series. <br />I! <br />These soils arc taxadjuncts of the Litchfield series because they have a thinner, darker colored A <br />horizon and contain more medium and coarse sand than the defined range for the series. <br />,10/ <br />Organic soils that have not been classified at the series level <br />JLL/ <br />These soils are taxadjuncts of the Shields series because the upper part of the B horizon is darker <br />than the defined range for the series. <br />sub <br />ist <br />gre <br />the <br />The <br />mai <br />abs <br />ini <br />gre <br />sec <br />hoi <br />cl; <br />cor <br />roc <br />the <br />at\ <br />se <br />al <br />an <br />us <br />n' <br />na <br />we <br />St <br />th <br />di <br />of <br />lo <br />a <br />Fc <br />th <br />an <br />nu <br />HU <br />Mi <br />ir <br />pa <br />St <br />ap <br />be <br />ce <br />th. <br />cc <br />cc <br />Pc <br />1)
The URL can be used to link to this page
Your browser does not support the video tag.