Official Series Description


Lab Data Summary

Aggregate lab data for the TRAPPIST soil series. This aggregation is based on all pedons with a current taxon name of TRAPPIST, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to TRAPPIST were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
114BJE70011970IN079001Trappist2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.96915,-85.5865639
114BJE70021970IN079002Trappist2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9172389,-85.5574278
114BJF76071976IN077007Trappist2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7019222,-85.5417472
114B87P000386IN143001Trappist6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8052788,-85.7258301
114B92P013488IN143058Trappist4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7138901,-85.7355576
114B92P013588IN143059Trappist4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7144432,-85.7272186
114B90P029089IN143001Trappist6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6775017,-85.585556
12190P06611990KY137012Trappist6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4838905,-84.6388855
12190P06641990KY137015Trappist6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4272232,-84.7794418
12287P07111987KY045006Trappist3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4749985,-84.9338913
12287KY-045-00687KY-045-006Trappist4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.475,-84.9338889
12484KY-069-UK584KY-069-UK5Trappist3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4197845,-83.6116791
12490KY-135-02690KY-135-026Trappist1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6292152,-83.5107193
12491P050191KY135001Trappist6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6300011,-83.5130539
12491P050291KY135002Trappist7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6291656,-83.5136108
12584KY-197-UK284KY-197-UK2Trappist3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8139496,-83.9532318
12587P046486KY197004Trappist6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8138885,-83.953331
n/aAD-w041962-OH001-W04Trappist3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aLG-0201969-OH091-020Trappist4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a79KY-173-00379KY-173-003Trappist3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a79KY-173-00479KY-173-004Trappist4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83P089883KY155001Trappist1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83KY-155-00183KY-155-001Trappist3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83P090283KY155005Trappist1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83KY-155-00583KY-155-005Trappist3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a87P025785KY069014Trappist5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-135-01294KY-135-012Trappist1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-135-01394KY-135-013Trappist1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-135-03094KY-135-030Trappist1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TRAPPIST soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the TRAPPIST series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the TRAPPIST series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the TRAPPIST series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with TRAPPIST share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the TRAPPIST series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the TRAPPIST series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with TRAPPIST, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. IN-2010-09-24-22 | Scott County -

    Typical pattern of soils and parent material in the Nabb-Cincinnati-Blocher association (Soil Survey of Scott County, Indiana).

  2. KY-2010-09-03-07 | Garrard and Lincoln Counties - 2006

    Typical pattern of soils and underlying material in the Trappist-Tilsit-Lenberg general soil map unit (Soil Survey of Garrard and Lincoln Counties, Kentucky; 2006).

  3. KY-2010-09-03-21 | Lewis County - 2004

    Typical pattern of soils and parent material in the Covedale-Trappist general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

  4. KY-2010-09-03-29 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Jessietown-Rohan-Allegheny-Muse general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  5. KY-2010-09-03-31 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Jessietown-Muse-Rohan general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  6. KY-2012-01-26-17 | Bath County - September 1963

    Typical landscape in the knobby areas of the county showing the topography, the relationship of some of the principal soils, and the parent rocks (Soil Survey of Bath County, Kentucky; September 1963).

  7. KY-2012-01-26-25 | Bath County - September 1963

    Cross section of Bath County showing the major soils and their relationship to the rock formations and to relief (Soil Survey of Bath County, Kentucky; September 1963).

  8. KY-2012-01-26-37 | Boyle and Mercer Counties - April 1983

    Typical pattern of soils and underlying material in the Trappist-McAfee-Colyer map unit (Soil Survey of Boyle and Mercer Counties, Kentucky; April 1983).

  9. KY-2012-01-27-02 | Bullitt and Spencer Counties - September 1986

    The relationship of soils to topography and underlying material in the Trappist-Lenberg-Carpenter general soil map unit (Soil Survey of Bullitt and Spencer Counties, Kentucky; September 1986).

  10. KY-2012-01-27-28 | Casey County - August 1994

    Typical pattern of soils and underlying materials in the Faywood-Lowell-Fairmount general soil map unit (Soil Survey of Casey County, Kentucky; August 1994).

  11. KY-2012-01-27-29 | Casey County - August 1994

    Typical pattern of soils and underlying materials in the Colyer-Faywood-Nolin general soil map unit (Soil Survey of Casey County, Kentucky; August 1994).

  12. KY-2012-01-27-43 | Clark County - 1964

    Major soil series in soil association 10, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

  13. KY-2012-01-27-45 | Clark County - 1964

    Geolgic cross section of Clark County, showing some of the principal soils and their relation to the rock formations (Soil Survey of Clark County, Kentucky; 1964).

  14. KY-2012-01-27-60 | Estill and Lee Counties - August 1974

    Pattern of soils and underlying material in the Colyer-Shrouts-Allegheny association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

  15. KY-2012-01-27-74 | Fleming County - October 1993

    Typical pattern of soils and parent material in the Muse-Blairton-Brownsville soil map unit (Soil Survey of Fleming County, Kentucky; October 1993).

  16. KY-2012-02-01-10 | Marion County - August 1991

    Typical pattern of soils and parent material in the Carpenter-Garmon-Rohan general soil map unit (Soil Survey of Marion County, Kentucky; August 1991).

  17. KY-2012-02-01-11 | Marion County - August 1991

    Typical pattern of soils and parent material in the Trappist-Crider-Faywood general soil map unit (Soil Survey of Marion County, Kentucky; August 1991).

  18. KY-2012-02-01-17 | McCreary-Whitley Area - 1970

    General location of the Muse and Shelocta soils in a typical area of the Jellico Mountains. Small areas of sandstone cliffs are common (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  19. KY-2012-02-01-18 | McCreary-Whitley Area - 1970

    General location of the Muse, Wellston, and Trappist soils on ridgetops and side slopes in association 3 (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  20. KY-2012-02-01-20 | McCreary-Whitley Area - 1970

    General location of the Tate and Trappist soils on ridgetops and long, steep side slopes in association 5 (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  21. KY-2012-02-01-24 | McCreary-Whitley Area - 1970

    The relationship of rock formations and relief to some of the soil associations on the general soil map of the McCreary-Whitley Area (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  22. KY-2012-02-01-34 | Montgomery County - January 1986

    The pattern of soils and relationship to topography and underlying material in the Tilsit-Morehead-Tyler general soil map unit (Soil Survey of Montgomery County, Kentucky; January 1986).

Map Units

Map units containing TRAPPIST as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Deputy-Trappist silt loams, 6 to 12 percent slopes, erodedDtvC228492011096r8din01920011:12000
Trappist-Deputy complex, 6 to 12 percent slopes, severely erodedTsaC3272418515966nwin01920011:12000
Trappist-Rohan silt loams, 12 to 25 percent slopesThdD263621083072czin01920011:12000
Trappist-Rohan complex, 12 to 25 percent slopes, severely erodedThcD3210718516166nyin01920011:12000
Trappist silty clay loam, 6 to 18 percent slopes, gulliedThbD516318516066nxin01920011:12000
Trappist silt loam, 6 to 12 percent slopes, erodedThaC26710581rvdzin01920011:12000
Trappist silty clay loam, 6 to 12 percent slopes, severely erodedThbC31710582rvf0in01920011:12000
Trappist-Rohan silt loams, 12 to 25 percent slopes, erodedThdD23922201662dj88in07119851:15840
Trappist-Rohan complex, 12 to 25 percent slopes, severely erodedThcD31202423825yd0in07119851:15840
Trappist silt loam, 12 to 18 percent slopes, erodedTrD260796468311cttin07719821:15840
Trappist silty clay loam, 12 to 25 percent slopes, severely erodedTtD353996468511ctwin07719821:15840
Trappist silty clay loam, 6 to 12 percent slopes, severely erodedTtC350496468411ctvin07719821:15840
Trappist silt loam, 6 to 12 percent slopes, erodedTrC235396468211ctsin07719821:15840
Deputy-Trappist silty clay loams, 6 to 15 percent slopes, severely erodedDtzC3329616514501sfglin07920101:12000
Trappist-Rohan silt loams, 12 to 25 percent slopes, erodedThdD272517168101vmgzin07920101:12000
Trappist-Rohan complex, 12 to 25 percent slopes, severely erodedThcD327317168091vmgyin07920101:12000
Trappist silty clay loam, 6 to 18 percent slopes, very severely erodedThbD45017168111vmh0in07920101:12000
Trappist-Rohan silt loams, 12 to 25 percent slopesThdD11871658015kjfin14319951:12000
Trappist silt loam, 6 to 12 percent slopes, erodedThaC210491657975kj9in14319951:12000
Trappist silty clay loam, 6 to 12 percent slopes, severely erodedThbC39771657985kjbin14319951:12000
Trappist-Rohan complex, 12 to 25 percent slopes, severely erodedThcD38071658005kjdin14319951:12000
Trappist silty clay loam, 6 to 18 percent slopes, gulliedThbD51801657995kjcin14319951:12000
Trappist-Muse silt loams, 20 to 60 percent slopes, erodedTsF2711117275221vzmjky01120061:12000
Rohan-Trappist complex, 12 to 60 percent slopes, erodedRoF2230317275251vzmmky01120061:12000
Covedale-Trappist silt loams, 12 to 30 percent slopesCpD159617275211vzmhky01120061:12000
Covedale-Trappist silt loams, 6 to 12 percent slopesCpC71617275201vzmgky01120061:12000
Trappist silt loam, 6 to 12 percent slopes, erodedTrC241217275241vzmlky01120061:12000
Trappist silt loam, 2 to 6 percent slopes, erodedTrB237817275231vzmkky01120061:12000
Colyer-Trappist complex, 12 to 20 percent slopesCpD5490548884lf4yky04519891:20000
Trappist silt loam, 6 to 12 percent slopesTrC1630548913lf5wky04519891:20000
Trappist silt loam, 2 to 6 percent slopesTrB660548912lf5vky04519891:20000
Trappist silt loam, 6 to 12 percent slopes, erodedTtC21006550229lgkbky04919621:15840
Trappist silt loam, 2 to 6 percent slopesTtB655550228lgk9ky04919621:15840
Trappist-Rohan complex, rocky, 12 to 25 percent slopes, erodedTpD2220551477lhvlky05719911:20000
Trappist silt loam, 6 to 12 percent slopes, erodedToC2105551476lhvkky05719911:20000
Muse-Trappist complex, 20 to 55 percent slopes, erodedMuF218179552727lk4xky06919891:20000
Colyer-Trappist complex, 12 to 55 percent slopes, erodedCoF2878552701lk42ky06919891:20000
Covedale-Trappist silt loams, 20 to 55 percent slopes, erodedCtF226731550293lgmdky13519981:20000
Colyer-Trappist silt loams, 12 to 60 percent slopes, erodedCkF21482550288lgm7ky13519981:20000
Covedale-Trappist silt loams, 12 to 20 percent slopes, erodedCtD21296550292lgmcky13519981:20000
Trappist silt loam, 2 to 6 percent slopesTtB100550329lgnkky13519981:20000
Trappist silt loam, 6 to 12 percent slopesTrC148613979231hxn9ky15119681:20000
Trappist silt loam, 2 to 6 percent slopesTrB95513979221hxn8ky15119681:20000
Trappist silty clay loam, 6 to 12 percent slopes, severely erodedTsC339613979251hxncky15119681:20000
Trappist silt loam, 12 to 20 percent slopesTrD23313979241hxnbky15119681:20000
Trappist-Rohan-Greenbriar complex, 12 to 20 percent slopes, eroded, rockyTrD211590552376ljslky15519861:20000
Trappist-Jessietown complex, 6 to 12 percent slopes, erodedTeC26670552375ljskky15519861:20000
Rohan-Trappist complex, 20 to 50 percent slopes, eroded, very rockyRtF26640552367ljs9ky15519861:20000
Rohan-Trappist complex, 6 to 20 percent slopes, eroded, very rockyRtD25065552366ljs8ky15519861:20000
Trappist-Rohan-Greenbriar complex, 12 to 25 percent slopes, severely eroded, rockyTrD32680552377ljsmky15519861:20000
Jessietown-Trappist complex, 2 to 6 percent slopesJeB1620552341ljrgky15519861:20000
Colyer-Trappist complex, 25 to 60 percent slopes, erodedCoF4684550514lgvjky17319831:20000
Trappist-Colyer-Shelocta complex, 12 to 30 percent slopes, erodedTsE2200550548lgwmky17319831:20000
Trappist silt loam, 6 to 12 percent slopes, erodedTrC732550547lgwlky17319831:20000
Trappist silt loam, 6 to 12 percent slopes, erodedTpC25200550008lgb6ky17919671:15840
Trappist silt loam, 2 to 6 percent slopesTpB1850550005lgb3ky17919671:15840
Trappist silt loam, 12 to 20 percent slopes, erodedTpD21840550010lgb8ky17919671:15840
Trappist silt loam, 6 to 12 percent slopesTpC1765550007lgb5ky17919671:15840
Trappist silt loam, 12 to 20 percent slopesTpD1220550009lgb7ky17919671:15840
Trappist silt loam, 2 to 6 percent slopes, erodedTpB21150550006lgb4ky17919671:15840
Trappist silty clay loam, 12 to 20 percent slopes, severely erodedTrD3700550012lgbbky17919671:15840
Trappist silty clay loam, 6 to 12 percent slopes, severely erodedTrC3455550011lgb9ky17919671:15840
Colyer-Trappist silt loams, 12 to 30 percent slopesCoD2550551530lhx9ky60619791:20000
Trappist silt loam, 6 to 12 percent slopesTpC926551565lhyfky60619791:20000
Trappist silt loam, 2 to 6 percent slopesTpB804551564lhydky60619791:20000
Trappist silt loam, 12 to 30 percent slopes, erodedTrD9074551017lhcrky60819831:20000
Trappist silt loam, 6 to 12 percent slopes, erodedTrC1205551016lhcqky60819831:20000
Rohan-Trappist complex, 6 to 25 percent slopesRtD3975557795lqfdky61620041:24000
Trappist silt loam, 6 to 12 percent slopesTrC1917557804lqfpky61620041:24000
Trappist silt loam, 2 to 6 percent slopesTrB191557803lqfnky61620041:24000
Trappist-Colyer complex, 12 to 25 percent slopes, erodedTrD25988553003lkftky61819931:12000
Trappist silty clay loam, 6 to 12 percent slopes, erodedTpC22518553002lkfsky61819931:12000
Colyer-Trappist complex, 25 to 60 percent slopes, eroded, very rockyCpF21192552930lkcgky61819931:12000
Trappist silt loam, 2 to 6 percent slopesTpB483553001lkfrky61819931:12000
Muse-Trappist stony silt loams, 30 to 60 percent slopesMtF372014788091lmtjky64519711:20000
Trappist silt loam, 8 to 15 percent slopesTrC10521701265q0yoh00119871:15840
Trappist silt loam, 3 to 8 percent slopesTrB2611701255q0xoh00119871:15840
Trappist silt loam, 15 to 25 percent slopes, erodedTrD22231701275q0zoh00119871:15840
Trappist-Shelocta association, steepTsF56189588021mtfoh00119871:15840
Colyer-Trappist complex, 35 to 50 percent slopesCoG240414203971jp18oh07119731:15840
Colyer-Trappist complex, 18 to 35 percent slopesCoF145714203961jp17oh07119731:15840
Trappist silt loam, 18 to 25 percent slopesTrE66714205291jp5joh07119731:15840
Trappist-Shelocta association, steepTwE65214206961jpbxoh07119731:15840
Trappist-Muse silt loams, 6 to 12 percent slopes, moderately erodedTsC244314205311jp5loh07119731:15840
Trappist-Muse silt loams, 12 to 18 percent slopes, moderately erodedTsD239114205321jp5moh07119731:15840
Trappist-Muse silt loams, 2 to 6 percent slopesTsB18014205301jp5koh07119731:15840
Colyer-Trappist complex, 12 to 18 percent slopes, moderately erodedCoD211314203951jp16oh07119731:15840
Trappist silt loam, 15 to 25 percent slopes, erodedToD26614206831jpbhoh07119731:15840
Trappist silt loam, 8 to 15 percent slopesToC414206821jpbgoh07119731:15840
Trappist silt loam, 15 to 25 percent slopesToD214206951jpbwoh07119731:15840
Trappist-Shelocta association, steepTsF18045537739l1kfoh13119841:15840
Trappist silt loam, 15 to 25 percent slopesTrD458537738l1kdoh13119841:15840
Trappist-Muse silt loams, 6 to 12 percent slopes, moderately erodedTtC2416890291tpktoh13119841:15840
Trappist silt loam, 7 to 15 percent slopes56C638520789kgxnva17119881:15840
Trappist silt loam, 2 to 7 percent slopes56B563520788kgxmva17119881:15840

Map of Series Extent

Approximate geographic distribution of the TRAPPIST soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .