Official Series Description


Lab Data Summary

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

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Competing Series

Soil series competing with SHEEP CREEK 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 SHEEP CREEK 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 SHEEP CREEK 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.

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Click the image to view it full size.

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

Soil series sharing subgroup-level classification with SHEEP CREEK, 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 SHEEP CREEK 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
Sheep Creek-Taylow-Dry Canyon complex, dry, 5 to 60 percent slopes185264915451055s6id71220081:24000
Pinehollow-Ant Flat-Sheep Creek complex, 2 to 35 percent slopes161146915894461qbygid71220081:24000
Dipcreek-Cutoff-Sheep Creek complex, 5 to 50 percent slopes68146115471801nxz1id71220081:24000
Chokecherry-Tubbs Hollow-Sheep Creek, dry complex, 3 to 60 percent slopes54113415451255s8id71220081:24000
Chokecherry-Slights-Sheep Creek complex, 5 to 40 percent slopes5358315897071qc6wid71220081:24000
Lonjon-Sheep Creek-Dipcreek complex, 10 to 50 percent slopes14348815471671nxymid71220081:24000
Lonjon-Sheep Creek-Dipcreek complex, 10 to 50 percent slopes143130939071nxymid7131:24000
Wanrhodes, very stony-Picayune-Sheep Creek, extremely stony complex, 10 to 60 percent slopesVVF3840749111t4hwut0131:24000
Agassiz-Rock outcrop-Sheep Creek association, 25 to 75 percent slopes, extremely stonySRG68714260641jvy2ut0131:24000
BICKMORE-SHEEP CREEK ASSOCIATION, ERODEDBLG28423482675j685ut60319681:20000
SHEEP CREEK-AGASSIZ ASSOCIATION, ERODEDSOG26259482826j6f1ut60319681:20000
SHEEP CREEK COBBLY LOAM, 30 TO 70 PERCENT SLOPES,ERODEDSNG24320482825j6f0ut60319681:20000
SHEEP CREEK-MAUGHAN ASSOCIATION, ERODEDSRG22853482828j6f3ut60319681:20000
SHEEP CREEK-DESPAIN ASSOCIATION, ERODEDSPG22015482827j6f2ut60319681:20000
Sheep Creek very cobbly loam, 30 to 70 percent slopesShF10983482618j66but60819811:24000
Rock outcrop-Sheep Creek complex, 30 to 70 percent slopesRnF8750482600j65rut60819811:24000
Sheep Creek very cobbly loam, 10 to 30 percent slopesShE6617482617j669ut60819811:24000
Sheep Creek-Flygare complex, 8 to 30 percent slopesSmE3775482620j66dut60819811:24000
Sheep Creek very cobbly loam, dry, 30 to 70 percent slopesSkF2866482619j66cut60819811:24000

Map of Series Extent

Approximate geographic distribution of the SHEEP CREEK 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 .