Official Series Description


Lab Data Summary

Aggregate lab data for the LEDGEFORK soil series. This aggregation is based on all pedons with a current taxon name of LEDGEFORK, 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 LEDGEFORK 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 LEDGEFORK 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 LEDGEFORK 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 LEDGEFORK 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 LEDGEFORK 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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Competing Series

Soil series competing with LEDGEFORK 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 LEDGEFORK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the LEDGEFORK 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

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

Soil series sharing subgroup-level classification with LEDGEFORK, 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 LEDGEFORK 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
Ledgefork family, 10 to 35 percent slopes, extremely stony surface80616826634342rq53id7131:24000
Como-Wander-Ledgefork families, complex, valley trough walls228X14581485584zl6mt60520071:24000
Ledgefork-Dunkleber-Wichup, rarely flooded families, complex, ice-margin slopes468G143314933650d9mt60520071:24000
Kamack-Ledgefork-Wander families, complex, valley trough walls227C74514933750dbmt60520071:24000
Marcetta-Ledgefork-Ledgefork, moderately deep, families, complex, steep mountain slopes541C566149198507vmt60520071:24000
Marcetta-Bearmouth-Branham families complex, steep mountain slopes541C1917079911vb9hmt62319881:24000
Cuberant-Ledgefork-Rock outcrop association, 15 to 70 percent slopes, extremely stony9311592757996tfrhut6471:24000
Cuberant-Ledgefork-Rubble land, talus association, 15 to 70 percent slopes, extremely stony1003557757997tfrjut6471:24000
Ledgefork very gravelly loamy fine sand, 20 to 60 percent slopes462431758304tg2fut6471:24000
Ledgefork-Kamack association, 20 to 60 percent slopes46-471739758308tg2kut6471:24000
Rock outcrop-Ledgefork family, very stony complex, 10 to 55 percent slopes98561758336tg3gut6471:24000
Ledgefork family, 5 to 30 percent slopes, very stony27555758307tg2jut6471:24000
Ledgefork, extremely stony-Ledgefork complex, 20 to 80 percent slopes45-46521758306tg2hut6471:24000
Ledgefork very stony loamy fine sand, 40 to 80 percent slopes, extremely stony45471758305tg2gut6471:24000
Cuberant, extremely stony-Ledgefork association, 30 to 70 percent slopes43-46421757995tfrgut6471:24000
Ledgefork cobbly sandy loam, 3 to 5 percent slopesNS7488532540372zw70ut6471:24000
Kimpton, extremely stony-Foxpoint, rubbly-Ledgefork families, complex, 8 to 25 percent slopes771874815230wc9rut6511:24000
Ledgefork cobbly sandy loam, 3 to 5 percent slopes143635503993jxfvwy63819901:24000
Ledgefork-Como-Targhee families, complex, 7 to 40 percent slopes309L1410016855821tkzmwy65620081:24000
Ledgefork-Como families-Rock outcrop complex, 7 to 40 percent slopes317L308216855841tkzpwy65620081:24000
Bullflat-Ledgefork families, complex, 7 to 40 percent slopes44L11491577595950wy65620081:24000
Ledgefork family, 7 to 40 percent slopes306L160185758220bz0wy65620081:24000
Ledgefork family-Aquic Cumulic Haplocryolls complex, 0 to 5 percent slopes130659151946533hwy66320121:24000
Como-Ledgefork families-Typic Cryaquepts, complex12673081730564972xtrgwy66519961:62500
Como-Matcher-Ledgefork families, complex1822656830564862xtr7wy66519961:62500
Idmonton, Ledgefork families and Typic Cryaquolls, soils22612296630565162xtscwy66519961:62500
Kangas, Ledgefork families and Typic Cryaquolls, soils82611813230565502xtt9wy66519961:62500
Midfork-Ledgefork families, complex2207461330565172xts5wy66519961:62500

Map of Series Extent

Approximate geographic distribution of the LEDGEFORK 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 .