Official Series Description


Lab Data Summary

Aggregate lab data for the AMESHA soil series. This aggregation is based on all pedons with a current taxon name of AMESHA, 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 AMESHA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
43B88P033887MT031007Amesha6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9927788,-111.4033356
4488P033587MT031002Amesha5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7675018,-111.6763916
4488P033787MT031004Amesha5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8241653,-111.6247253
4440A3700S1970MT007003Amesha6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0674057,-111.5519638
4440A3699S1970MT007004Amesha6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5982361,-111.6164246

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AMESHA 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.

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Sibling Summary

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

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

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Geomorphic description summaries for the AMESHA 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 .

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

Competing Series

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

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

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Geomorphic description summaries for the AMESHA 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 .

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There are insufficient data to create the 3D mountains figure.

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

Soil series sharing subgroup-level classification with AMESHA, 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

No block diagrams are available.

Map Units

Map units containing AMESHA 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
Amesha loam, 0 to 4 percent slopes36B213411481334z4hmt60420011:24000
Amesha-Kalsted complex, 2 to 8 percent slopes136C113491481644z5hmt60420011:24000
Amesha-Bronec-Sappington complex, 4 to 15 percent slopes336D52201481854z65mt60420011:24000
Kounter-Amesha-Rock outcrop complex, 8 to 35 percent slopes36E2760609136nfvkmt60420011:24000
Amesha-Haxby-Rencot complex, 4 to 15 percent slopes436D18851482084z6xmt60420011:24000
Amesha loam, 4 to 8 percent slopes36C16911481344z4jmt60420011:24000
Bronec, Amesha, and Riverrun, occasionally flooded soils, 0 to 35 percent slopes41E427609142nfvrmt60420011:24000
Musselshell-Amesha, bedrock substratum, complex, cool, 8 to 25 percent slopes84111185964320f3hmt60520071:24000
Crago-Amesha complex, 2 to 8 percent slopes89C2524038322lpczmt60520071:24000
Scravo-Amesha-Scravo complex, 2 to 35 percent slopes355E1724064132ls27mt60520071:24000
Amesha loam, 1 to 4 percent slopesAoB306741474814yggmt60919711:24000
Amesha loam, 4 to 9 percent slopesAoC87421474824yghmt60919711:24000
Amesha sandy loam, 1 to 4 percent slopesAmB40711474784ygcmt60919711:24000
Amesha sandy loam, 4 to 9 percent slopesAmC12621474794ygdmt60919711:24000
Amesha cobbly sandy loam, 1 to 4 percent slopesAnB10921474804ygfmt60919711:24000
Amesha silt loam, 4 to 8 percent slopes11C3291475584yjymt60919711:24000
Sappington-Amesha complex, 2 to 8 percent slopes532C2181476164yltmt60919711:24000
Cabbart-Shoddy-Amesha complex, 8 to 15 percent slopes191D1971475934yl2mt60919711:24000
Cabbart-Shoddy-Amesha complex, 15 to 45 percent slopes191E1601475944yl3mt60919711:24000
Crago-Amesha complex, 2 to 8 percent slopes264C1181475994yl8mt60919711:24000
Amesha loam, 4 to 8 percent slopes32C10814765556ptmt60919711:24000
Bronec-Shoddy-Amesha complex, 15 to 35 percent slopes273E1041476054ylgmt60919711:24000
Amesha-Amesha, stony complex, 2 to 8 percent slopes113C851476644yncmt60919711:24000
Amesha gravelly loam, 2 to 8 percent slopes115C761475844yksmt60919711:24000
Amesha cobbly loam, 2 to 8 percent slopes118C711475874ykwmt60919711:24000
Bronec, Clunton, Channeled, and Amesha soils, 0 to 8 percent slopes4521475574yjxmt60919711:24000
Bronec-Amesha complex, 15 to 35 percent slopes271E331476034yldmt60919711:24000
Amesha-Crago-Shoddy complex, 4 to 15 percent slopes114D181475834ykrmt60919711:24000
Bronec-Amesha complex, 2 to 8 percent slopes271C171476024ylcmt60919711:24000
Amesha-Trimad complex, 15 to 45 percent slopes32E1614765756pwmt60919711:24000
Sappington-Amesha loams, 1 to 4 percent slopes3033B151476374ymhmt60919711:24000
Bronec, Amesha, and Riverrun, channeled soils, 0 to 35 percent slopes41151475714ykcmt60919711:24000
Amesha-Amesha, stony complex, 8 to 15 percent slopes113D151475824ykqmt60919711:24000
Cabbart-Amesha-Trimad complex, 15 to 45 percent slopes710E141476734ynnmt60919711:24000
Amesha loam, 2 to 8 percent slopes116C111475864ykvmt60919711:24000
Amesha loam, 8 to 15 percent slopes32D81476564yn3mt60919711:24000
Amesha gravelly loam, 8 to 15 percent slopes115D71475854yktmt60919711:24000
Cabbart-Shoddy-Amesha complex, 2 to 8 percent slopes191C71475924yl1mt60919711:24000
Amesha silt loam, 8 to 15 percent slopes11D51475594yjzmt60919711:24000
Bronec-Shoddy-Amesha complex, 4 to 15 percent slopes273D21476044ylfmt60919711:24000
Crago-Amesha complex, 35 to 60 percent slopes264F21476004yl9mt60919711:24000
Crago-Amesha complex, 2 to 8 percent slopes89C719522288582dt9nmt61220111:24000
Amesha-Bronec-Varney complex, 2 to 8 percent slopes42C259914074471j7kjmt61220111:24000
Amesha loam, 0 to 4 percent slopes36B1707798343vsr0mt61220111:24000
Scravo-Amesha-Scravo, escarpments complex, 2 to 35 percent slopes355E137922288612dt9rmt61220111:24000
Amesha-Yamacall complex, 2 to 8 percent slopes236C49824099902lwsmmt61220111:24000
Amesha-Bronec-Sappington complex, 4 to 15 percent slopes336D32025976644z65mt61220111:24000
Amesha loam, 4 to 8 percent slopes36C30425976534z4jmt61220111:24000
Amesha-Haxby-Rencot complex, 4 to 15 percent slopes436D6025976694z6xmt61220111:24000
Amesha-Kalsted complex, 2 to 8 percent slopes136C4725976584z5hmt61220111:24000
Bronec, Amesha, and Riverrun, occasionally flooded soils, 0 to 35 percent slopes41E132597683nfvrmt61220111:24000
Amesha loam, 0 to 4 percent slopes32B1067315539656psmt62219971:24000
Amesha loam, 4 to 8 percent slopes32C818615539756ptmt62219971:24000
Cabbart-Amesha-Trimad complex, 15 to 45 percent slopes710E759815567256zpmt62219971:24000
Amesha loam, 8 to 15 percent slopes32D666515539856pvmt62219971:24000
Amesha-Trimad complex, 15 to 45 percent slopes32E599915539956pwmt62219971:24000
Cabbart-Amesha loams, 2 to 8 percent slopes710C165615567056zmmt62219971:24000
Cabbart-Amesha loams, 8 to 15 percent slopes710D134115567156znmt62219971:24000
Amesha loam, 35 to 60 percent slopes32F115115540056pxmt62219971:24000
Amesha cobbly loam, 2 to 8 percent slopes232C112515533256mqmt62219971:24000
Rentsac-Amesha complex, 8 to 25 percent slopes412E85415546456rzmt62219971:24000
Cabbart, moist-Amesha-Trimad complex, 15 to 45 percent slopes810E555155734571pmt62219971:24000
Amesha-Musselshell complex, 2 to 4 percent slopes139B4325232291ncg1mt62420211:24000
Amesha loam, 2 to 8 percent slopes116C651715051951mgmt62719981:24000
Bronec-Amesha complex, 2 to 8 percent slopes271C6400150992523qmt62719981:24000
Sappington-Amesha complex, 2 to 8 percent slopes532C5014151112527lmt62719981:24000
Bronec-Shoddy-Amesha complex, 15 to 35 percent slopes273E4678150998523xmt62719981:24000
Bronec-Amesha complex, 8 to 15 percent slopes271D4545150993523rmt62719981:24000
Amesha gravelly loam, 2 to 8 percent slopes115C373015051051m5mt62719981:24000
Sappington-Amesha complex, 2 to 8 percent slopes, cobbly539B3716151123527ymt62719981:24000
Amesha silt loam, 4 to 8 percent slopes11C316815053551mzmt62719981:24000
Amesha loam, 0 to 2 percent slopes116A267015051851mfmt62719981:24000
Cabbart-Shoddy-Amesha complex, 15 to 45 percent slopes191E254415076251w9mt62719981:24000
Crago-Amesha complex, 2 to 8 percent slopes264C2204150964522tmt62719981:24000
Amesha silt loam, 1 to 4 percent slopes11B152015053451mymt62719981:24000
Bronec-Amesha cobbly loams, 2 to 8 percent slopes277C15061510085247mt62719981:24000
Bronec, Amesha, and Riverrun, channeled, soils, 0 to 35 percent slopes4114131510665263mt62719981:24000
Amesha-Crago-Shoddy complex, 15 to 45 percent slopes114E116215050051lvmt62719981:24000
Bronec, Riverrun, Channeled, and Amesha soils, 0 to 8 percent slopes9111115154252pgmt62719981:24000
Bronec, Clunton, Channeled, and Amesha soils, 0 to 8 percent slopes410081510635260mt62719981:24000
Bronec-Amesha-Rock outcrop complex, 35 to 60 percent slopes271F976150995523tmt62719981:24000
Crago-Amesha complex, 15 to 35 percent slopes264E968150966522wmt62719981:24000
Crago-Amesha complex, 8 to 15 percent slopes264D877150965522vmt62719981:24000
Cabbart-Shoddy-Amesha complex, 8 to 15 percent slopes191D75415076151w8mt62719981:24000
Amesha-Amesha, stony, complex, 2 to 8 percent slopes113C74215048951lhmt62719981:24000
Brocko-Amesha complex, 4 to 15 percent slopes182D71415072751v5mt62719981:24000
Sappington-Amesha loams, 1 to 4 percent slopes3033B70315165552t3mt62719981:24000
Bronec-Shoddy-Amesha complex, 4 to 15 percent slopes273D686150997523wmt62719981:24000
Sappington-Amesha complex, 0 to 2 percent slopes536A619151118527smt62719981:24000
Sappington-Amesha complex, 2 to 8 percent slopes, stony539C583151124527zmt62719981:24000
Amesha gravelly loam, 15 to 35 percent slopes115E57915051251m7mt62719981:24000
Haxby-Amesha-Rencot complex, 4 to 15 percent slopes511C5711511035279mt62719981:24000
Amesha loam, 8 to 15 percent slopes116D48515052051mhmt62719981:24000
Amesha silt loam, 8 to 15 percent slopes11D48315053651n0mt62719981:24000
Amesha gravelly loam, 0 to 2 percent slopes115A44815050951m4mt62719981:24000
Amesha cobbly loam, 2 to 8 percent slopes118C37915053251mwmt62719981:24000
Crago-Amesha cobbly loams, 2 to 8 percent slopes268C3301509785238mt62719981:24000
Amesha gravelly loam, 8 to 15 percent slopes115D32515051151m6mt62719981:24000
Amesha-Cabbart-Bronec cobbly loams, 4 to 25 percent slopes117E32515052651mpmt62719981:24000
Crago-Amesha complex, 35 to 60 percent slopes264F242150967522xmt62719981:24000
Amesha-Amesha, stony, complex, 8 to 15 percent slopes113D22915049051ljmt62719981:24000
Cabbart-Shoddy-Amesha complex, 2 to 8 percent slopes191C22415076051w7mt62719981:24000
Amesha-Crago-Shoddy complex, 4 to 15 percent slopes114D21415049951ltmt62719981:24000
Bronec-Amesha-Bronec complex, 15 to 35 percent slopes271E167150994523smt62719981:24000
Sappington-Amesha loams, 4 to 8 percent slopes3033C12215165452t2mt62719981:24000
Sappington-Amesha loams, 1 to 4 percent slopes33B157221477894ysdmt63019911:24000
Delpoint-Amesha loams, 2 to 8 percent slopes457C44731478224ytgmt63019911:24000
Amesha silt loam, 1 to 3 percent slopes136B23101476964ypdmt63019911:24000
Sappington-Amesha loams, 4 to 8 percent slopes33C22571477904ysfmt63019911:24000
Musselshell-Amesha, bedrock substratum, complex, cool, 8 to 25 percent slopes84350531465124xg6mt63619831:24000
Amesha loam, cool, bedrock substratum, 8 to 25 percent slopes483821464634xdmmt63619831:24000
Thess-Amesha loams, cool, 0 to 2 percent slopes13359811464074xbtmt63619831:24000
Amesha, bedrock substratum-Musselshell complex, cool, 2 to 8 percent slopes531231464744xdzmt63619831:24000
Amesha loam, cool, 2 to 8 percent slopes327661464524xd8mt63619831:24000
Bronec-Amesha complex, 2 to 8 percent slopes2171681465814xjfmt63619831:24000
Amesha silt loam, 1 to 4 percent slopes209601465774xj9mt63619831:24000
Bronec-Amesha complex, 15 to 35 percent slopes219431465834xjhmt63619831:24000
Bronec-Amesha-Rock outcrop complex, 35 to 60 percent slopes220351465844xjjmt63619831:24000
Bronec-Amesha complex, 8 to 15 percent slopes218121465824xjgmt63619831:24000
Amesha silt loam, 4 to 8 percent slopes21071465784xjbmt63619831:24000
Amesha-Musselshell complex, cool, 2 to 4 percent slopes129B12351479834yznmt63720141:24000
Amesha silt loam, cool, 1 to 4 percent slopes29B11601480154z0pmt63720141:24000
Amesha-Musselshell complex, 2 to 4 percent slopes139B65415303471ncg1mt63720141:24000
Amesha silt loam, 1 to 4 percent slopes39B37715308581nczjmt63720141:24000

Map of Series Extent

Approximate geographic distribution of the AMESHA 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 .