Official Series Description


Lab Data Summary

Aggregate lab data for the LAKE CREEK soil series. This aggregation is based on all pedons with a current taxon name of LAKE 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 LAKE 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 LAKE 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 LAKE 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 LAKE 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 LAKE 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 flats position figure.

Competing Series

Soil series competing with LAKE 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 LAKE 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 LAKE 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.

Click the image to view it full size.

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 LAKE 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 LAKE 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
Lake creek-Rock outcrop complex, 35 to 65 percent slopes154840498378jqlqco63519791:24000
Lake creek loam, 15 to 50 percent slopes433503497868jq28co64919771:24000
Angostura-Lake creek-Pagosa complex, 3 to 65 percent slopes59113496892jp1sco68419841:24000
Angostura-Lake creek-Seitz complex, 3 to 60 percent slopes64559496903jp24co68419841:24000
McIntyre-Lake creek-Scout complex, 2 to 65 percent slopes704406496915jp2jco68419841:24000
Lake creek-Scout-Angostura complex, 5 to 65 percent slopes643833496908jp29co68419841:24000
Elve, extremely stony-Lake Creek, very stony-Comad, rubbly families, complex, 35 to 60 percent slopes1168F37330396602r6xsmt60219631:20000
Lake Creek, very stony-Findon-Redfern, extremely stony famiies, complex, 35 to 70 percent slopes2100G15030396692rf1xmt60219631:20000
Sebud, extremely stony-Lake Creek, very stony-Surdal, stony families, complex, 25 to 60 percent slopes1169F6930396622r6xvmt60219631:20000
Lake Creek, very stony-Elve, extremely stony, families-Rubble land, complex, 45 to 70 percent slopes1168G6530396802qbzwmt60219631:20000
Lake Creek, very stony-Elve, extremely stony-Comad, rubbly families, complex, 8 to 35 percent slopes1168E1630396612r6xtmt60219631:20000
Lake creek channery loam, 20 to 50 percent slopesLaF58101475114yhfmt60919711:24000
Passcreek-Lake Creek channery loams, 15 to 35 percent slopesPcE29351475304yj1mt60919711:24000
Sebud, extremely stony-Lake Creek, very stony-Surdal, stony families, complex, 25 to 60 percent slopes1169F5430448322r6xvmt61519921:24000
Libeg, bouldery-Findon-Lake Creek, extremely stony complex, 25 to 60 percent slopes740F3926946352l9y4mt62420211:24000
Sebud, extremely stony-Lake Creek, very stony-Surdal, stony families, complex, 25 to 60 percent slopes1169F6730940882r6xvmt63019911:24000
Elve, extremely stony-Lake Creek, very stony-Comad, rubbly families, complex, 35 to 60 percent slopes1168F3276426044412r6xsmt6321:24000
Lake Creek, very stony-Elve, extremely stony-Comad, rubbly families, complex, 8 to 35 percent slopes1168E1441426044422r6xtmt6321:24000
Sebud, extremely stony-Lake Creek, very stony-Surdal, stony families, complex, 25 to 60 percent slopes1169F1010926044432r6xvmt6321:24000
Sebud, very stony-Lake Creek, stony-Surdal, stony families, complex, 8 to 35 percent slopes1169E825126044402r6xrmt6321:24000
Lake Creek, very stony-Findon-Redfern, extremely stony famiies, complex, 35 to 70 percent slopes2100G723226274352rf1xmt6321:24000
Lake Creek-Surdal families, complex, 30 to 60 percent slopes, very stony1166F538027246362sh7wmt6321:24000
Findon-Lake Creek, very stony-Dailybasin families, complex, 8 to 35 percent slopes, landslides2100E440726274332rf1tmt6321:24000
Lake Creek, very stony-Elve, extremely stony, families-Rubble land, complex, 45 to 70 percent slopes1168G360726322652qbzwmt6321:24000
Worock-Lake Creek-Catlinsprings complex, 20 to 60 percent slopes, extremely stony7703F26342512879swnfmt6321:24000
Libeg, bouldery-Findon-Lake Creek, extremely stony complex, 25 to 60 percent slopes740F93623928322l9y4mt6321:24000
Lake Creek-Mawspring, stony families, complex, 2 to 15 percent slopes1147D29427246302sh7qmt6321:24000
Libeg, bouldery-Findon-Lake Creek, extremely stony complex, 25 to 60 percent slopes740F92816125541r3zwmt63720141:24000
Worock-Lake Creek-Catlinsprings complex, 20 to 60 percent slopes, extremely stony7703F52424860312pfxkmt63720141:24000
Sebud, extremely stony-Lake Creek, very stony-Surdal, stony families, complex, 25 to 60 percent slopes1169F24929796662r6xvmt63720141:24000
Elve, extremely stony-Lake Creek, very stony-Comad, rubbly families, complex, 35 to 60 percent slopes1168F5929796672r6xsmt63720141:24000
Sebud, very stony-Lake Creek, stony-Surdal, stony families, complex, 8 to 35 percent slopes1169E4729796742r6xrmt63720141:24000
Sebud, extremely stony-Lake Creek, very stony-Surdal, stony families, complex, 25 to 60 percent slopes1169F2730941232r6xvmt65719901:24000
Worock-Lake Creek-Catlinsprings complex, 20 to 60 percent slopes, extremely stony7703F2369741564swnfmt6691:24000

Map of Series Extent

Approximate geographic distribution of the LAKE 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 .