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Table 2.04.9-20 Soil Map Unit Descriptions (continued) <br />tS' 3' iq <br />0lo;i <br />S oil <br />Subsoil <br />Lfnutin $F..SurfText <br />_ ;.rd, <br />.i,. qr <br />'e`Si`:�t" <br />.,#IW <br />.'� <br />,To <br />-�': �lM:��. <br />.. <br />_ •td'. -ii v:.:,..;P:'.W+.W:SmJ• ,^GAJ., <br />9 „_. <br />Huai rock content in the subsoil <br />Typic Haplustolls and Pachic sods ( Weed & Shawa) <br />This unit occurs in the northern portion ofthe project <br />30 <br />0-35 <br />Maudlin <br />75 <br />Loam <br />8 <br />16 <br />and below Especially hr`li rock <br />are likely present to a hunted extent Bedrock outcrop <br />area on stable surfaces with weathered sandstone and <br />content m subsoil of steeper <br />occurs in less than 5% ofthe unit. <br />siltstone Loess influence is noted on the steeper north <br />slopes <br />facing slopes with rocky colluvium in the subsoil <br />Loam. Silt <br />Very high clay content, shale, and <br />Where bedrock is present at depths between 20 and <br />These soils develop from weathered shale residuum <br />Morapos <br />60 <br />Loam. & <br />10 <br />20 <br />carbonates are present in the <br />40 inches Maudlin is present Sods formed in clay <br />and colluvium on ridge tops and gentle slopes. The <br />31 <br />0-20 <br />Clay Loam <br />subsoil and below <br />over sandstone bedrock (e g, Nortez), small resistant <br />begmining of the subsoil is marked by the notable <br />Campspass <br />25 <br />Clay Loam <br />6 <br />20 <br />Very high clay content in the <br />subsoil with additional clay and <br />sandstone outcrops. and Tomorthent inclusions are <br />increase in clay content The argillic horizons ofthis <br />carbonates at eater de th <br />also present. <br />unit are very well developed <br />These soils develop from weathered shale residuum <br />Loam, Silt <br />Very high clay content, shale and <br />Where bedrock is present at depths between 20 and <br />and colluvium on ridge tops and gentle slopes The <br />32 <br />0-20 <br />Morapos <br />70 <br />Loam, & <br />10 <br />20 <br />carbonates are present in the <br />40 inches Maudlin is present. Some sods in this unit <br />beginning ofthe subsoil is marked by the notable <br />Clay Loam <br />subsoil and below <br />do not exhibit mottle colors (Campspass). <br />increase in clay content The ar&nllic horizons of this <br />unit are very well developed. <br />Non-lumting inclusions are more loamy textured <br />Higher clay content and coarse <br />(Maud![), deeper (Morapos), and shallower (Owen <br />This unit is located on ridge tops and formed from thin <br />33 <br />0-35 <br />Nortez <br />65 <br />Loam <br />8 <br />16 <br />fragments at seater depth <br />Creek) MolisBedrock outcrop is present, but <br />loess deposits over shale with sandstone bedrock at <br />occurs in lessthan than 2%ofthis unit <br />depths generally less than 40 inches <br />Weed <br />55 <br />Loam <br />16 <br />24 <br />High clay and rock content in the <br />This unit is located on ridge tops and swales and <br />subsoil and below <br />Finer textured sods without a pathic horizon <br />developed from l weathered shale residuum with <br />34 <br />0-20 <br />(Morapos) and sods without an aranlltc honzon <br />a notable loess andrid alluvial influence accounting for <br />(Shawa and Typic Haplustolls) may be present to a <br />High rock content in the subsoil <br />limited extent <br />loamy textures Loess influence is especially notable <br />Maudlin <br />30 <br />Loam <br />8 <br />16 <br />and below <br />on the steeper north facing slopes <br />Sods without a pathic epipedon (Morapos) and <br />This unit is located on ridge tops and swales and <br />35 <br />0-20 <br />Weed <br />70 <br />Loam <br />16 <br />24 <br />High clay and carbonates are <br />shallower sods (Maudlin) are likely present in thus <br />developed from highly weathered shale residuum with <br />present deeper in the soil <br />notable loess and alluvial influence accounting for <br />unita <br />loamy textures <br />Danavore <br />40 <br />Learn <br />3 <br />10 <br />Steep slopes, mumnal profile development Most of <br />36 <br />25-60 <br />High rock content at depth <br />Some thin loess deposits creating Haplo/.4rgtcryolls <br />the argillic horizons are weak and border on cambic <br />Ustic Haplocryalfs/Haplocryepts <br />40 <br />Loam <br />3 <br />10 <br />(Haplocryepts) <br />Danavore <br />40 <br />Loam <br />3 <br />10 <br />Ridge tops with some loess accumulation, but many <br />37 <br />0-25 <br />High rock/shale content at depth <br />Areas with thinner or no loess may develop Cryalfs <br />wind swept areas. Opportunities for suitable salsage <br />Thornburgh <br />40 <br />Loam <br />10 <br />t0 <br />are highly variable <br />38 <br />0-35 <br />Wa be <br />50 <br />Clay <br />8 <br />0 <br />Hio clay content <br />Tomonhents occur to a limited extent, other soils are <br />Ridge Tops and upper slopes on the south end Very <br />Other Haplocryepts <br />35 <br />Loam <br />15 <br />0 <br />High rock and clay content - <br />similar to primary components <br />tittle, of any, subsoil <br />bedrock <br />This unit occurs to a very hinted extent in as cryic <br />39 <br />10-25 <br />Loamy -Skeletal Ustic Haplocryept <br />70 <br />Gravelly- <br />4 <br />15 <br />Weak profile development and <br />Eutrocryalfs and similar Mollisols (Thornburgh) are <br />alluvial deposits with materials originating from bare <br />Loam <br />high rock content at depth <br />present in this unit <br />Haplocryept/Tomorthent slopes in the southern <br />