Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CASHMONT 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 CASHMONT 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 CASHMONT 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 CASHMONT 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 CASHMONT 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 CASHMONT 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 CASHMONT 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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Click the image to view it full size.

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with CASHMONT, 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. WA-2010-11-05-06 | Douglas County - 2008

    Cross-section view of the Moses Coulee area (Soil Survey of Douglas County, Washington; 2008).

  2. WA-2012-05-11-39 | Douglas County - May 2008

    Cross-section of the Moses Coulee area (Soil Survey of Douglas County, Washington; May 2008).

Map Units

Map units containing CASHMONT 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
Cashmont sandy loam, 3 to 8 percent slopes901134699602rgztwa01719981:12000
Cashmont gravelly sandy loam, 3 to 8 percent slopes87883699509rgwtwa01719981:12000
Cashmont gravelly sandy loam, 8 to 15 percent slopes88801699510rgwvwa01719981:12000
Cashmont sandy loam, 8 to 15 percent slopes9177699600rgzrwa01719981:12000
Cashmont sandy loam, 0 to 3 percent slopes8936699562rgyjwa01719981:12000
Cashmont sandy loam, 3 to 8 percent slopesCcB2704733052g8pwa60719691:20000
Cashmont sandy loam, 0 to 3 percent slopesCcA2179733042g8nwa60719691:20000
Cashmont gravelly sandy loam, 8 to 15 percent slopesCdC1400733062g8qwa60719691:20000
Cashmont stony sandy loam, 0 to 25 percent slopesCeD923733082g8swa60719691:20000
Cashmont gravelly sandy loam, 15 to 25 percent slopesCdD612733072g8rwa60719691:20000
Cashmont sandy loam, 0 to 8 percent slopes562056802528scwa60819951:24000
Cashmont gravelly sandy loam, 8 to 25 percent slopes571046802628sdwa60819951:24000
Cashmont gravelly sandy loam, fan, 3 to 15 percent slopes712583707102ckzwa64819871:24000
Cashmont gravelly sandy loam, fan, 15 to 30 percent slopes72312707112cl0wa64819871:24000
Lithic Haploxerepts-Cashmont complex, 15 to 45 percent slopes33822715189979021rwkwa64920081:24000
Cashmont sandy loam, 25 to 45 percent slopes, extremely stony23411665189973021rtmwa64920081:24000
Cashmont sandy loam, 0 to 25 percent slopes, extremely stony23310990189972921rtlwa64920081:24000
Cashmont sandy loam, 8 to 15 percent slopes2304480189972421rtfwa64920081:24000
Cashmont sandy loam, 3 to 8 percent slopes2294320189972321rtdwa64920081:24000
Cashmont sandy loam, 15 to 25 percent slopes2311220189972521rtgwa64920081:24000
Cashmont sandy loam, 0 to 3 percent slopes228800189972121rtbwa64920081:24000
Cashmont gravelly sandy loam, 0 to 8 percent slopes232610189972721rtjwa64920081:24000

Map of Series Extent

Approximate geographic distribution of the CASHMONT 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 .