Official Series Description


Lab Data Summary

Aggregate lab data for the ELVICK soil series. This aggregation is based on all pedons with a current taxon name of ELVICK, 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 ELVICK 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
43B93P068193MT043011Elvick6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.047123,-112.0255966

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ELVICK 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 ELVICK 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 ELVICK 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 ELVICK 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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Competing Series

Soil series competing with ELVICK 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 ELVICK 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 ELVICK 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 .

There are insufficient data to create the 2D hillslope position figure.

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 ELVICK, 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 ELVICK 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
Elvick family-Fluvaquentic Cryaquepts, complex, stream bottoms10UC1002628090322tr3mmt60319891:24000
Typic Cryaquepts-Elvick family, complex, outwash terraces73UB330228091322trb3mt60319891:24000
Evaro-Holloway-Elvick families, complex, nivational mountain slopes and ridges71NDB14300507350kfmt60319891:24000
Como-Elvick-Worock families, complex, cirque basins258U69391485724zlnmt60520071:24000
Como-Elvick-Lowder, frequently flooded families, complex, alluvial-colluvial deposits618U629149071503rmt60520071:24000
Klutch family-Rock outcrop-Elvick family, complex, steep glaciated mountain slopes and ridges15UE3357185959520f1ymt60520071:24000
Worock-Evaro-Elvick families, complex, nivational mountain slopes and ridges71UDB11185961120f2gmt60520071:24000
Evaro-Holloway-Elvick families, complex, high relief mountain slopes and ridges71ND33185960920f2dmt60520071:24000
Mooseflat-Elvick loams, 1 to 4 percent slopes2332B3891509095211mt62719981:24000
Lowder-Elvick very cobbly loams, 2 to 15 percent slopes, very bouldery2501D3241509435224mt62719981:24000
Elvick-Lowder complex, 8 to 25 percent slopes, very bouldery2472E284150933521tmt62719981:24000
Elve, very stony-Rock outcrop-Rubble land complex, 4 to 35 percent slopes2488D1001509425223mt62719981:24000
Garlet-Cowood-Elvick families complex, steep glaciated mountain slopes and ridges15VD365617035171v5n5mt63119881:24000
Elve-Evaro-Elvick families complex, high relief mountain slopes and ridges71NB37017035351v5nrmt63119881:24000
Finn-Elvick families-Water complex, moderately steep young moraines21GJ2217035221v5nbmt63119881:24000
Elvick-Como, very stony-Chillybu families, complex, 2 to 25 percent slopes2260E359925128902qbz9mt6321:24000
Evaro-Holloway-Elvick families, complex, high relief mountain slopes and ridges71ND33239414949450kdmt63520061:24000
Garlet-Cowood-Elvick families, complex, steep glaciated mountain slopes and ridges15VD31477314939150g2mt63520061:24000
Loberg-Elvick-Garlet families, complex, moderately steep old moraines22UD21288314941250grmt63520061:24000
Evaro-Holloway-Elvick families, complex, nivational mountain slopes and ridges71NDB790814949550kfmt63520061:24000
Klutch family-Rock outcrop-Elvick family, complex, steep glaciated mountain slopes and ridges15UE3504614938850fzmt63520061:24000
Elve-Evaro-Elvick families, complex, high relief mountain slopes and ridges71NB3458914949150k9mt63520061:24000
Worock-Evaro-Elvick families, complex, nivational mountain slopes and ridges71UDB291314950450kqmt63520061:24000
Garlet-Bata-Elvick families, complex, nivational mountain slopes and ridges15UDB209814938650fxmt63520061:24000
Garlet-Worock-Elvick families, complex, moderately steep trough bottoms37UC2115114943350hfmt63520061:24000
Loberg-Danaher-Elvick families, complex, low relief mountain slopes and ridges75DCD67114953250lmmt63520061:24000
Gambler-Elve-Elvick families, complex, moderately steep young moraines21UA266014939850g9mt63520061:24000
Finn-Elvick families-Water complex, moderately steep young moraines21GJ259014939750g8mt63520061:24000
Yreka-Winkler-Elvick families, complex, moderately steep young moraines21UCF38214940150gdmt63520061:24000
Evaro-Holloway-Elvick families, complex, high relief mountain slopes and ridges27095817034501v5l0mt63619831:24000
Elve-Evaro-Elvick families, complex, high relief mountain slopes and ridges26794217034471v5kxmt63619831:24000
Elvick-Como, very stony-Chillybu families, complex, 2 to 25 percent slopes2260E729796792qbz9mt63720141:24000
Typic Cryaquepts-Elvick family, complex, outwash terraces73UB123829953722trb3mt63819851:24000
Elvick family-Fluvaquentic Cryaquepts, complex, stream bottoms10UC11829953192tr3mmt63819851:24000
Typic Cryaquepts-Elvick family, complex, outwash terraces73UB11129953902trb3mt64419951:24000
Elvick family-Fluvaquentic Cryaquepts, complex, stream bottoms10UC5329953742tr3mmt64419951:24000
Garlet-Worock-Elvick families complex, moderately steep trough bottoms37UC22917044891v6njmt64419951:24000
Elvick family-Fluvaquentic Cryaquepts, complex, stream bottoms10UC24229953962tr3mmt65119971:24000
Moose River-Elvick families, complex, 3 to 25 percent slopes302L20090186032320ftfwy65620081:24000
Subsummit Uplands, Tundra-Willow-Rock Outcrop Complex24612046815183352zvwy66219981:24000
Subsummit Uplands, Rock Outcrop-Tundra-Willow Complex24011755515182952zqwy66219981:24000
Alpine Cirques, Rock Outcrop-Tundra-Willow Complex17011377215182452zkwy66219981:24000

Map of Series Extent

Approximate geographic distribution of the ELVICK 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 .