Official Series Description


Lab Data Summary

Aggregate lab data for the RUMBLECREEK soil series. This aggregation is based on all pedons with a current taxon name of RUMBLECREEK, 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 RUMBLECREEK 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
4489P035188MT077855Rumblecreek6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0750008,-113.0824966

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RUMBLECREEK 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 RUMBLECREEK 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 RUMBLECREEK 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 RUMBLECREEK 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 hills figure.

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

Competing Series

Soil series competing with RUMBLECREEK 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 RUMBLECREEK 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 RUMBLECREEK 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 RUMBLECREEK, 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 RUMBLECREEK 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
Rumblecreek-Sol families, complex, colluvial aprons and alluvial fans, very stony15JB2429728090402tr3wmt60319891:24000
Rumblecreek gravelly loam, 35 to 60 percent slopes395F51129955344wmhmt60319891:24000
Winfall-Rumblecreek gravelly loams, 2 to 8 slopes171C28129955214wgtmt60319891:24000
Winfall-Rumblecreek gravelly loams, 8 to 25 slopes171E23229955224wgvmt60319891:24000
Courville-Rumblecreek complex, 4 to 15 percent slopes39D1852995451mgb5mt60319891:24000
Winfall-Rumblecreek gravelly loams, 25 to 50 percent slopes171F10329955234wgwmt60319891:24000
Rumblecreek gravelly loam, 15 to 35 percent slopes395E9829955334wmgmt60319891:24000
Rumblecreek gravelly loam, 15 to 30 percent slopes36E41299559857bvmt60319891:24000
Rumblecreek gravelly loam, dry, 15 to 30 percent slopes37E33299560057c4mt60319891:24000
Rumblecreek gravelly loam, 4 to 15 percent slopes36D16299559757bsmt60319891:24000
Rumblecreek-Courville complex, dry, 4 to 15 percent slopes40D6385579796mgb3mt61820081:24000
Courville-Rumblecreek complex, 4 to 15 percent slopes39D1271579798mgb5mt61820081:24000
Rumblecreek-Courville complex, dry, 15 to 30 percent slopes40E759579797mgb4mt61820081:24000
Courville, dry-Rumblecreek, dry-Lozeau, deep complex, 30 to 60 percent slopes41F485512822k6mnmt61820081:24000
Rumblecreek-Sol families, complex, colluvial aprons and alluvial fans, very stony15JB029952862tr3wmt61820081:24000
Rumblecreek gravelly loam, 15 to 30 percent slopes15237201450524vy3mt62919911:20000
Rumblecreek gravelly loam, 30 to 60 percent slopes15335161450534vy4mt62919911:20000
Rumblecreek gravelly loam, 8 to 15 percent slopes15121441450514vy2mt62919911:20000
Courville-Rumblecreek complex, 8 to 30 percent slopes347401451424w10mt62919911:20000
Rumblecreek gravelly loam, 2 to 8 percent slopes1506871450494vy0mt62919911:20000
Rumblecreek gravelly loam, 15 to 30 percent slopes, lake effect20733117160021vlmxmt62919911:20000
Rumblecreek gravelly loam, 4 to 30 percent slopes95152871455184wf4mt63819851:24000
Rumblecreek-Sol families, complex, colluvial aprons and alluvial fans, very stony15JB13029953262tr3wmt63819851:24000
Winfall-Rumblecreek gravelly loams, 8 to 25 slopes171E49851455714wgvmt64419951:24000
Winfall-Rumblecreek gravelly loams, 2 to 8 slopes171C46301455704wgtmt64419951:24000
Rumblecreek gravelly loam, 15 to 35 percent slopes395E34001457144wmgmt64419951:24000
Rumblecreek gravelly loam, 35 to 60 percent slopes395F23221457154wmhmt64419951:24000
Rumblecreek-Water complex, 2 to 8 percent slopes271C13751456324wjtmt64419951:24000
Winfall-Rumblecreek gravelly loams, 25 to 50 percent slopes171F10711455724wgwmt64419951:24000
Rumblecreek-Water complex, 8 to 25 percent slopes271E10241456344wjwmt64419951:24000
Bignell-Rumblecreek complex, 15 to 35 percent slopes999E6571459914wxdmt64419951:24000
Rumblecreek gravelly loam, 8 to 15 percent slopes395D2801457134wmfmt64419951:24000
Bignell-Rumblecreek complex, 8 to 15 percent slopes999D2451459904wxcmt64419951:24000
Rumblecreek-Water complex, 25 to 50 percent slopes271F1101456364wjymt64419951:24000
Bignell-Rumblecreek complex, 35 to 60 percent slopes999F421459924wxfmt64419951:24000
Rumblecreek-Sol families, complex, colluvial aprons and alluvial fans, very stony15JB629953762tr3wmt64419951:24000
Rumblecreek gravelly loam, dry, 4 to 15 percent slopes37D627215602657c3mt65119971:24000
Rumblecreek gravelly loam, dry, 15 to 30 percent slopes37E299015602757c4mt65119971:24000
Rumblecreek gravelly loam, 15 to 30 percent slopes36E220715601857bvmt65119971:24000
Rumblecreek gravelly loam, 4 to 15 percent slopes36D163315601657bsmt65119971:24000
Rumblecreek gravelly loam, 8 to 15 percent slopes, stony392D115815603557cdmt65119971:24000
Rumblecreek gravelly loam, dry, 30 to 50 percent slopes37F100615602957c6mt65119971:24000
Rumblecreek gravelly loam, 30 to 50 percent slopes36F93615602057bxmt65119971:24000
Rumblecreek gravelly loam, 15 to 30 percent slopes, stony392E27215603757cgmt65119971:24000
Rumblecreek-Sol families, complex, colluvial aprons and alluvial fans, very stony15JB2929954012tr3wmt65119971:24000

Map of Series Extent

Approximate geographic distribution of the RUMBLECREEK 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 .