Official Series Description


Lab Data Summary

Aggregate lab data for the LONGCREEK soil series. This aggregation is based on all pedons with a current taxon name of LONGCREEK, 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 LONGCREEK 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 LONGCREEK 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 LONGCREEK 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 LONGCREEK 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 LONGCREEK 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 LONGCREEK 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 LONGCREEK 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 LONGCREEK 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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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 LONGCREEK, 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 LONGCREEK 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
Jellycamp-Karcal-Longcreek complex, cool, 2 to 15 percent slopes199im23414690001l9m3ca60319741:24000
Longcreek-Vansickle-Rock outcrop complex, 9 to 30 percent slopes235im10314690021l9m5ca60319741:24000
Jellycamp-Lassen-Longcreek complex, 2 to 15 percent slopes20022384486990jbrcca60419941:24000
Jellycamp-Karcal-Longcreek complex, cool, 2 to 15 percent slopes1995333486988jbr9ca60419941:24000
Longcreek-Vansickle-Rock outcrop complex, 9 to 30 percent slopes2354693487060jbtmca60419941:24000
Jellycamp-Karcal-Longcreek complex, 2 to 15 percent slopes1982304486986jbr7ca60419941:24000
Longcreek-Devada-Rubble land complex, 9 to 30 percent slopes27326916487578jccbca60820001:24000
Devada-Longcreek association, 2 to 30 percent slopes17512470487445jc71ca60820001:24000
Rubble land-Longcreek-Fivesprings association, 30 to 60 percent slopes3449141487687jcgvca60820001:24000
Fivesprings-Longcreek-Rubble land association 9 to 50 percent slopes2009062487482jc87ca60820001:24000
Fivesprings-Longcreek association, 9 to 30 percent slopes1986920487480jc85ca60820001:24000
Longcreek-Devada-Rubble land complex, 30 to 50 percent slopes2746064487580jccdca60820001:24000
Fivesprings-Longcreek association, 30 to 50 percent slopes1991511487481jc86ca60820001:24000
Longcreek-Vansickle-Rock outcrop complex, 9 to 30 percent slopes235im365189929021rcfca70319831:24000
Jellycamp-Lassen-Longcreek complex, 2 to 15 percent slopes200im64189921121r8wca70319831:24000
Jellycamp-Karcal-Longcreek complex, 2 to 15 percent slopes198im51189920921r8tca70319831:24000
Jellycamp-Lassen-Longcreek complex, 2 to 15 percent slopes200It3915281751n95zca70819841:24000
Jellycamp-Karcal-Longcreek complex, cool, 2 to 15 percent slopes199It2615281731n95xca70819841:24000
Longcreek-Devada association2805994954762w37bca72920061:24000
Longcreek-Hurryback-Succor complex, 3 to 40 percent slopes9520943486302jb15id67519921:24000
Willhill-Cottle-Longcreek complex, 3 to 35 percent slopes21117078486131j9vnid67519921:24000
Catchell-Longcreek complex, 3 to 25 percent slopes356517486178j9x5id67519921:24000
Longcreek-Rock outcrop complex5315574474755hy0pnv76019941:24000
Longcreek-Softscrabble-Anawalt association7583915474791hy1vnv76019941:24000
Longcreek-Cleavage association296555474716hxzfnv76019941:24000
Tunnison-Longcreek-Devada association750551024527362nb8jnv77219851:24000
Devada-Longcreek-Duco association164117024527032nb7gnv77219851:24000
Longcreek-Devada association280154816977932w37bnv77319811:24000
Longcreek-Menbo-Rock outcrop association134111370475498hysnnv77719931:24000
Longcreek-Zymans association13456793475501hysrnv77719931:24000
Longcreek-Softscrabble-Anawalt association13445039475500hysqnv77719931:24000
Menbo-Devada-Longcreek association15624602475571hyw0nv77719931:24000
Longcreek-Rock outcrop complex, 50 to 75 percent slopes13421059475499hyspnv77719931:24000
Mahoon-Brezniak-Longcreek complex, 2 to 20 percent slopes18714263490563jggmor62819971:24000
Longcreek-Rock outcrop complex, 40 to 70 percent south slopes1801533490556jggdor62819971:24000
Longcreek-Cleavage complex, 20 to 50 percent slopes1791466490553jgg9or62819971:24000
Longcreek-Hurryback-Succor complex, 3 to 40 percent slopesID009516922026337260kqor64420211:24000

Map of Series Extent

Approximate geographic distribution of the LONGCREEK 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 .