Official Series Description


Lab Data Summary

Aggregate lab data for the ESCALANTE soil series. This aggregation is based on all pedons with a current taxon name of ESCALANTE, 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 ESCALANTE 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
28A85P093685UT021005Escalante7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.75,-113.25
28A90P103490UT027003Escalante8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9916649,-112.4197235
28A70C0044S1968UT027059Escalante7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0466652,-112.4488907
28A70C0045S1968UT027060Escalante7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0466652,-112.4488907
n/a40A1137S1977UT021003ESCALANTE8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ESCALANTE 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 ESCALANTE 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 ESCALANTE 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 ESCALANTE 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 ESCALANTE 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 ESCALANTE 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 ESCALANTE 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 mountains figure.

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Soil series sharing subgroup-level classification with ESCALANTE, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. ID-2010-08-31-01 | Owyhee County Area - 2003

    Typical pattern of soils in map unit 5 (Soil Survey of Owyhee County Area, Idaho; 2003).

Map Units

Map units containing ESCALANTE 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
Escalante-Tindahay-Ornea complex, 1 to 12 percent slopes5515005486220j9yjid67519921:24000
Escalante sandy loam, 1 to 12 percent slopes542439486218j9ygid67519921:24000
Escalante sandy loam, 0 to 1 percent slopes224215823542rplid70719761:24000
Escalante sandy loam, 1 to 3 percent slopes231732823552rpmid70719761:24000
Escalante sandy loam, 3 to 7 percent slopes24557823562rpnid70719761:24000
Escalante fine sandy loam, 1 to 3 percent slopes585833825312rw9id70819871:24000
Escalante sandy loam, 4 to 8 percent slopes57975825302rw8id70819871:24000
Kecko-Escalante complex, 2 to 4 percent slopes255625825992ryhid70919761:24000
Kecko-Escalante complex, 8 to 12 percent slopes271483826012rykid70919761:24000
Kecko-Escalante complex, 4 to 8 percent slopes26838826002ryjid70919761:24000
Escalante fine sandy loam, 4 to 12 percent slopes1213363248311g0id71019681:24000
Escalante sandy loam 0 to 2 percent slopesEnA3093827172s29id71019681:24000
Escalante sandy loam, undulatingEOC2100827162s28id71019681:24000
Escalante sandy loam, 2 to 4 percent slopesEnB1187827182s2bid71019681:24000
Escalante sandy loam, saline-alkali, 0 to 2 percent slopesEsA609827202s2did71019681:24000
Escalante sandy loam, saline-alkali, 2 to 4 percent slopesEsB400827212s2fid71019681:24000
Escalante sandy loam, 4 to 8 percent slopesEnC372827192s2cid71019681:24000
Escalante-Summermute-Jericho association306019913480004j3h0nv77920041:24000
Rouette-Ursine-Escalante association322117433637446pd9snv77920041:24000
Linoyer-Escalante association317010033480012j3h8nv77920041:24000
Jericho-Summermute-Escalante association13209387479963j3fpnv77920041:24000
Jericho-Escalante-Dakent association41301682480128j3m0nv77920041:24000
Atlanta-Escalante association50211400637449pd9wnv77920041:24000
Ursine-Escalante association13821389637445pd9rnv77920041:24000
Sycomat-Escalante-Timpie association31741215480013j3h9nv77920041:24000
Armespan-Escalante association101026430481094j4m5nv78420061:24000
Ursine-Escalante association103023336481099j4mbnv78420061:24000
Eastmore-Escalante association10031975216011861qr55nv78420061:24000
Sycomat-Escalante-Gravier association124016353481150j4nznv78420061:24000
Cath-Watoopah-Escalante association, warm17331086615474761ny8lnv78420061:24000
Cath-Watoopah-Escalante association17325673481175j4psnv78420061:24000
Rouette-Ursine-Escalante association3221400213956301hv8bnv78420061:24000
Ursine-Escalante-Lien association10503214481107j4mlnv78420061:24000
Linoyer-Escalante association317069013956291hv89nv78420061:24000
Atlanta-Escalante association502168114452417dz4nv78420061:24000
Sycomat-Escalante-Timpie association8321513897161hn3kut61119921:24000
Escalante sandy loam, 2 to 5 percent slopes438409481836j5d3ut61819951:24000
Escalante sandy loam, 0 to 2 percent slopes426501481835j5d2ut61819951:24000
Medburn-Berent-Escalante complex, 0 to 8 percent slopes915160481892j5fxut61819951:24000
Escalante-Berent-Escalante complex, 2 to 15 percent slopes442390481837j5d4ut61819951:24000
Escalante sandy loam, 3 to 15 percent slopes137157922204602djkrut6261:24000
Escalante gravelly sandy loam, gravelly substratum, 2 to 5 percent slopes1281387483448j723ut6281:24000
Escalante sandy loam, gravelly substratum, 2 to 4 percent slopes130697483446j721ut6281:24000
Escalante sandy loam, 1 to 4 percent slopes129359483444j71zut6281:24000
Hiko Peak-Escalante complex, 2 to 5 percent slopesHgC4841504682jy52ut6291:24000
Escalante gravelly sandy loam, very gravelly substratum, 2 to 5 percent slopes12830825105842r80wut6291:24000
Escalante-Yenrab complex, undulatingEYC1846482393j5z2ut63219701:20000
Escalante sandy loam, 1 to 5 percent slopesESB637482392j5z1ut63219701:20000
Escalante sandy loam, 0 to 5 percent slopes37532816483902j7jrut63419971:24000
Escalante sandy loam, 1 to 5 percent slopes37610924483903j7jsut63419971:24000
Taylorsflat-Escalante sandy loams, 2 to 5 percent slopes4923856484035j7p1ut63419971:24000
Escalante sandy loam, 2 to 10 percent slopes, erodedECD26310484588j87wut64019671:20000
Escalante-Hiko Peak complex, 2 to 10 percent slopes, erodedESD24820484589j87xut64019671:20000
Spager-Escalante families, complex, 15 to 30 percent slopes203625278nzn8ut6491:24000
Escalante family, 15 to 30 percent slopes150625235nzlwut6491:24000
Escalante-Berent-Crestline families, complex, 2 to 30 persent slopes152625234nzlvut6491:24000
Spager-Escalante families, complex, 2 to 15 percent slopes202625279nzn9ut6491:24000
Crestline-Heist-Escalante families complex, 2 to 8 percent slopes135625208nzl0ut6491:24000
Escalante-Annabella-Berent families, complex, 5 to 30 percent slopes151581649mj7wut6491:24000

Map of Series Extent

Approximate geographic distribution of the ESCALANTE 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 .