Official Series Description


Lab Data Summary

Aggregate lab data for the CASTLECREST soil series. This aggregation is based on all pedons with a current taxon name of CASTLECREST, 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 CASTLECREST 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
304N039003OR035016Castlecrest6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8701057,-122.1652908
304N102104OR035001Castlecrest7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0486107,-122.1180573

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CASTLECREST 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 CASTLECREST 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 CASTLECREST 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 CASTLECREST 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 hills figure.

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

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Competing Series

Soil series competing with CASTLECREST 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 CASTLECREST 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 CASTLECREST 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.

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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 CASTLECREST, 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 CASTLECREST 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
Castlecrest ashy loamy sand, 0 to 8 percent slopes239447259343943830k99or6571:24000
Castlecrest-Lavaflat complex, 0 to 20 percent slopes239455586343944730k9por6571:24000
Castlecrest-Cinder land complex, 0 to 30 percent slopes, high elevation239331888343944330k9gor6571:24000
Castlecrest gravelly ashy sandy loam, 2 to 10 percent slopes422980627755p275or68220011:24000
Llaorock-Castlecrest complex, 15 to 30 percent slopes3517420628217p2q2or68220011:24000
Castlecrest-Llaorock complex, 2 to 25 percent slopes912320627769p27mor68220011:24000
Unionpeak-Castlecrest-Sunnotch complex, 0 to 15 percent slopes678900628250p2r4or68220011:24000
Llaorock-Castlecrest complex, 0 to 15 percent slopes346420628216p2q1or68220011:24000
Llaorock-Castlecrest-Rock outcrop complex, 30 to 60 percent south slopes376130854812vygor68220011:24000
Castlecrest ashy loamy sand, dry, 0 to 15 percent slopes56000627757p277or68220011:24000
Castlecrest ashy loamy sand, low, 0 to 7 percent slopes65700627758p278or68220011:24000
Timbercrater-Llaorock-Castlecrest complex, 30 to 60 percent slopes604960628243p2qxor68220011:24000
Llaorock-Castlecrest-Rock outcrop complex, 30 to 60 percent north slopes364700628218p2q3or68220011:24000
Timbercrater-Castlecrest complex, dry, 15 to 30 percent south slopes553450628238p2qror68220011:24000
Castlecrest-Badland complex, 60 to 100 percent slopes83250627763p27for68220011:24000
Unionpeak-Castlecrest-Llaorock complex, 15 to 30 percent slopes663000628249p2r3or68220011:24000
Timbercrater-Sunnotch-Castlecrest complex, 0 to 10 percent slopes612870628244p2qyor68220011:24000
Timbercrater-Castlecrest complex, dry, 2 to 15 percent slopes542450628237p2qqor68220011:24000
Timbercrater-Castlecrest-Llaorock complex, 10 to 30 percent south slopes562260628239p2qsor68220011:24000
Cleetwood-Castlecrest-Llaorock complex, 5 to 30 percent slopes131950627774p27sor68220011:24000
Cleetwood-Sunnotch-Castlecrest complex, high elevation, 15 to 30 percent slopes161200627801p28nor68220011:24000
Timbercrater-Castlecrest complex, 0 to 10 percent slopes531020628236p2qpor68220011:24000
Castlecrest-Sunnotch complex, 5 to 45 percent slopes10800627770p27nor68220011:24000
Cleetwood-Castlecrest complex, dry, 10 to 30 percent slopes12800627773p27ror68220011:24000
Unionpeak-Castlecrest complex, dry, 5 to 15 percent slopes65590628248p2r2or68220011:24000
Castlecrest gravelly ashy loamy sand, high elevation, 5 to 45 percent slopes7400627760p27bor68220011:24000

Map of Series Extent

Approximate geographic distribution of the CASTLECREST 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 .