Official Series Description


Lab Data Summary

Aggregate lab data for the COUGARROCK soil series. This aggregation is based on all pedons with a current taxon name of COUGARROCK, 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 COUGARROCK 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
43C97P0540S1997OR023001COUGARROCK7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5922203,-118.7930527

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COUGARROCK 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 COUGARROCK 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 COUGARROCK 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 COUGARROCK 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 terrace figure.

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

Competing Series

Soil series competing with COUGARROCK 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 COUGARROCK 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 COUGARROCK 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 COUGARROCK, 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 COUGARROCK 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
Dunstan-Cougarrock complex, 15 to 30 percent slopes3376BO95931204441r03for60720181:24000
Cougarrock-Dunstan-Kamela complex, 15 to 30 percent slopes3375BO89631204431r03cor60720181:24000
Cougarrock-Dunstan complex, 30 to 60 percent slopes3360CO72131204351r02lor60720181:24000
Dunstan-Cougarrock-Fivebeaver complex, 15 to 30 percent slopes3355BO57431204331r02gor60720181:24000
Cougarrock-Dunstan-Btree complex, 0 to 30 percent slopes3359NO37031207061shmqor60720181:24000
Dunstan-Cougarrock complex, 30 to 60 percent slopes3356CO34131203241qy1lor60720181:24000
Cougarrock-Dunstan complex, 0 to 15 percent slopes3358AO25231204341r02jor60720181:24000
Cougarrock-Dunstan-Kamela complex, 0 to 15 percent slopes3375AO14631204421r02xor60720181:24000
Sharpridge-Cougarrock-Grubcreek complex, 15 to 30 percent slopes3421BO14431204561r052or60720181:24000
Sharpridge-Fourbeaver-Cougarrock complex, 0 to 15 percent slopes3474AO5231204611r05mor60720181:24000
Dunstan-Cougarrock-Fivebeaver complex, 15 to 30 percent slopes3355BO453931222301r02gor62620181:24000
Sharpridge-Cougarrock-Grubcreek complex, 15 to 30 percent slopes3421BO385031222561r052or62620181:24000
Cougarrock-Dunstan complex, 30 to 60 percent slopes3360CO369231222321r02lor62620181:24000
Dunstan-Cougarrock complex, 30 to 60 percent slopes3356CO351531221601qy1lor62620181:24000
Cougarrock-Dunstan-Btree complex, 0 to 30 percent slopes3359NO338831224711shmqor62620181:24000
Dunstan-Cougarrock-Fivebeaver complex, 0 to 15 percent slopes3355AO135831220991q6shor62620181:24000
Cougarrock-Dunstan complex, 0 to 15 percent slopes3358AO38631222311r02jor62620181:24000
Sharpridge-Fourbeaver-Cougarrock complex, 0 to 15 percent slopes3474AO16531222641r05mor62620181:24000
Dunstan-Cougarrock-Fivebit, moist complex, 0 to 15 percent slopes3355AO121534294992l101or6271:24000
Dunstan-Cougarrock-Fivebeaver complex, 15 to 30 percent slopes3355BO56734298021r02gor6271:24000
Cougarrock-Dunstan complex, 30 to 60 percent slopes3360CO38834298031r02lor6271:24000
Dunstan-Cougarrock complex, 30 to 60 percent slopes3356CO35134319111qy1lor6271:24000
Sharpridge-Cougarrock-Grubcreek complex, 15 to 30 percent slopes3421BO6434298041r052or6271:24000
Cougarrock-Dunstan-Btree complex, 0 to 30 percent slopes3359NO2734319101shmqor6271:24000
Dunstan-Cougarrock complex, 15 to 30 percent slopes3376BO7024867251r03for63120181:24000
Cougarrock-Dunstan-Kamela complex, 15 to 30 percent slopes3375BO6724867241r03cor63120181:24000
Dunstan-Cougarrock complex, 30 to 60 percent slopes3356CO5424867191qy1lor63120181:24000
Dunstan-Cougarrock-Fivebeaver complex, 15 to 30 percent slopes3355BO2424867181r02gor63120181:24000
Cougarrock-Dunstan complex, 30 to 60 percent slopes3360CO1624867201r02lor63120181:24000
Cougarrock-Dunstan-Kamela complex, 0 to 15 percent slopes3375AO224867231r02xor63120181:24000

Map of Series Extent

Approximate geographic distribution of the COUGARROCK 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 .