Official Series Description


Lab Data Summary

Aggregate lab data for the EASTRIDGE soil series. This aggregation is based on all pedons with a current taxon name of EASTRIDGE, 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 EASTRIDGE 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 EASTRIDGE 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 EASTRIDGE 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 EASTRIDGE 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 EASTRIDGE 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 EASTRIDGE 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 EASTRIDGE 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 EASTRIDGE 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 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 EASTRIDGE, 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 EASTRIDGE 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
Loberg, very stony-Eastridge, very stony-Hairpin, frequently ponded, stony complex, 8 to 35 percent slopes, landslides707E226324377642mtpkmt61220111:24000
Ermont, extremely stony-Rock outcrop-Eastridge, very stony complex, 15 to 50 percent slopes799F109224263462mft7mt61220111:24000
Sicklesteets, stony-Eastridge, very stony-Rooset, very stony complex, 8 to 35 percent slopes, landslides806E60024270552mgk3mt61220111:24000
Rock outcrop-Doolittle-Eastridge complex, 20 to 60 percent slopes, landslides705F46424365562msflmt61220111:24000
Ermont, extremely stony-Rock outcrop-Eastridge, very stony complex, 15 to 50 percent slopes799F46825207432mft7mt61420121:24000
Evaro-Eastridge-Vitroff complex, 20 to 50 percent slopes548F41717031881v59kmt63520061:24000
Eastridge-Germangulch complex, 25 to 60 percent slopes, very stony516F31017031771v596mt63520061:24000
Eastridge-Euell complex, 15 to 40 percent slopes570E21717031941v59rmt63520061:24000
Eastridge-Hungryhill-Poin complex, 20 to 50 percent slopes, very stony515F16317031761v595mt63520061:24000
Evaro-Eastridge complex, 20 to 50 percent slopes567F11717031931v59qmt63520061:24000
Eastridge-Judco complex, 20 to 60 percent slopes508F10917031741v593mt63520061:24000
Bridger-Eastridge-Hungryhill complex, 25 to 60 percent slopes, very stony503F9217031721v591mt63520061:24000
Poin, very stony-Rubble land-Eastridge, very stony complex, 25 to 70 percent slopes562G6017031921v59pmt63520061:24000
Eastridge gravelly ashy loam, 45 to 75 percent slopes525G5417031811v59bmt63520061:24000
Eastridge-Euell, cool, complex, 8 to 30 percent slopes559E4417031901v59mmt63520061:24000
Germangulch-Eastridge-Euell complex, 25 to 60 percent slopes, very stony518F2817031781v597mt63520061:24000
Evaro-Eastridge-Vitroff complex, 20 to 50 percent slopes548F2761361830d4hymt67020071:24000
Eastridge-Euell complex, 15 to 40 percent slopes570E2424361843d4jcmt67020071:24000
Eastridge-Germangulch complex, 25 to 60 percent slopes, very stony516F2303361839d4j7mt67020071:24000
Eastridge-Hungryhill-Poin complex, 20 to 50 percent slopes, very stony515F1562362007d4pnmt67020071:24000
Eastridge-Judco complex, 20 to 60 percent slopes508F1498361832d4j0mt67020071:24000
Germangulch-Eastridge-Euell complex, 25 to 60 percent slopes, very stony518F1321361838d4j6mt67020071:24000
Eastridge-Euell complex, 15 to 30 percent slopes, very stony519E1146361840d4j8mt67020071:24000
Bridger-Eastridge-Hungryhill complex, 25 to 60 percent slopes, very stony503F972361845d4jfmt67020071:24000
Poin, very stony-Rubble land-Eastridge, very stony complex, 25 to 70 percent slopes562G740320503brhtmt67020071:24000
Eastridge-Euell, cool complex, 8 to 30 percent slopes559E469361837d4j5mt67020071:24000
Evaro-Eastridge complex, 20 to 50 percent slopes567F377361825d4hsmt67020071:24000
Eastridge gravelly ashy loam, 45 to 75 percent slopes525G286361833d4j1mt67020071:24000

Map of Series Extent

Approximate geographic distribution of the EASTRIDGE 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 .