Official Series Description


Lab Data Summary

Aggregate lab data for the TEPECREEK soil series. This aggregation is based on all pedons with a current taxon name of TEPECREEK, 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 TEPECREEK 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
n/a93P067293MT043002Tepecreek6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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

Soil series sharing subgroup-level classification with TEPECREEK, 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 TEPECREEK 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
Rubble land-Tepecreek family, very rubbly, complex, 20 to 70 percent slope5401G2030396682r88jmt60219631:20000
Tepecreek-Comad-Libeg families, complex, gentle mountain slopes528P53361490495031mt60520071:24000
Tepecreek-Libeg families-Rock outcrop complex, steep mountain slopes548Pr5223149092504fmt60520071:24000
Tepecreek-Ellena-Libeg families, complex, steep mountain slopes548P3585149091504dmt60520071:24000
Comad family-Rock outcrop-Tepecreek family, complex, moderately steep mountain slopes538Pr35451490555037mt60520071:24000
Bearmouth-Gateview-Tepecreek families, complex, glacial moraines348X33111485914zm8mt60520071:24000
Bearmouth-Howardsville-Tepecreek families, complex, glacial moraines348P28911485884zm5mt60520071:24000
Libeg-Tepecreek families-Rock outcrop complex, steep mountain slopes548X2857149094504hmt60520071:24000
Tepecreek-Beeftrail-Bearmouth families, complex, gentle mountain slopes528X22911490525034mt60520071:24000
Ellena-Tepecreek families, complex, steep mountain slopes548E6331490885049mt60520071:24000
Tepecreek-Comad-Libeg families, complex, gentle mountain slopes528P16215312161ndc2mt61020051:24000
Tepecreek-Ellena-Libeg families, complex, steep mountain slopes548P12815902431qcs5mt61020051:24000
Bearmouth-Gateview-Tepecreek families, complex, glacial moraines348X30825977004zm8mt61220111:24000
Tepecreek-Beeftrail-Bearmouth families, complex, gentle mountain slopes528X20925977525034mt61220111:24000
Bearmouth-Howardsville-Tepecreek families, complex, glacial moraines348P10925976994zm5mt61220111:24000
Tepecreek-Libeg families-Rock outcrop complex, steep mountain slopes548Pr372597754504fmt61220111:24000
Tepecreek-Ellena-Caseypeak complex, 35 to 60 percent slopes, very bouldery5030F172154873564xmt61620031:24000
Tepecreek, stony-Caseypeak, very bouldery-Rock outcrop complex, 15 to 35 percent slopes1735E152415070251tcmt62719981:24000
Tepecreek, stony-Caseypeak, very stony-Rock outcrop complex, 35 to 60 percent slopes1735F117615070351tdmt62719981:24000
Tepecreek, very bouldery-Caseypeak, very bouldery-Rock outcrop complex, 35 to 60 percent slopes1732F115815070051t9mt62719981:24000
Tepecreek, bouldery-Caseypeak, very bouldery-Rock outcrop complex, 8 to 35 percent slopes1731E76415069751t6mt62719981:24000
Tepecreek, very bouldery-Caseypeak, rubbly-Rock outcrop complex, 35 to 60 percent slopes1731F39915069851t7mt62719981:24000
Bobowic, very bouldery-Rock outcrop-Tepecreek, very bouldery, complex, 25 to 60 percent slopes1990F32515078851x4mt62719981:24000
Rubble land-Tepecreek family, very rubbly, complex, 20 to 70 percent slope5401G58026098382r88jmt6321:24000
Tepecreek, very bouldery-Caseypeak, very bouldery-Rock outcrop complex, 35 to 60 percent slopes1732F40017030741v55wmt63520061:24000
Bobowic, very bouldery-Rock outcrop-Tepecreek, very bouldery, complex, 25 to 60 percent slopes1990F7517030861v568mt63520061:24000
Tepecreek-Wix complex, 15 to 40 percent slopes7504540925547192rbzwwy6351:24000
Tepecreek-Wix complex, 15 to 40 percent slopes75041029251072rbzwwy71319861:24000

Map of Series Extent

Approximate geographic distribution of the TEPECREEK 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 .