Official Series Description


Lab Data Summary

Aggregate lab data for the YEATES HOLLOW soil series. This aggregation is based on all pedons with a current taxon name of YEATES HOLLOW, 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 YEATES HOLLOW 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
4772C0087S1972UT057003Yeates Hollow7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3082657,-111.6330185

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the YEATES HOLLOW 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 YEATES HOLLOW 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 YEATES HOLLOW 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 YEATES HOLLOW 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 YEATES HOLLOW 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 YEATES HOLLOW 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 YEATES HOLLOW 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 flats position figure.

Soil series sharing subgroup-level classification with YEATES HOLLOW, 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-2010-08-30-08 | Franklin County Area - 2008

    Typical pattern of soils and underlying material in general soil map units 8 (Yeates Hollow-Vitale-Northwater) and 9 (Yeates Hollow-Manila-Softback) (Soil Survey of Franklin County Area, Idaho; 2008).

  2. UT-2012-03-22-09 | Rich County - July 1982

    Typical pattern of soils in general map unit 9 (Soil Survey of Rich County, UT; 1982).

  3. UT-2012-05-10-08 | Rich County - July 1982

    Typical pattern of soils in general map unit 9 (Soil Survey of Rich County, Utah; July 1982).

Map Units

Map units containing YEATES HOLLOW 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
Yeates Hollow-Chen-Povey complex, 25 to 55 percent slopes1637739824832rtrid70819871:24000
Yeates Hollow-Hades complex, 10 to 40 percent slopes1643880824842rtsid70819871:24000
Yeates Hollow, extremely stony surface-Manila-Softback complex, 12 to 40 percent slopes162664229170582sltqid7131:24000
Yeates Hollow family, extremely stony surface-Manila family, very stony surface, perched water table-Booneville complex, 5 to 35 percent slopes108894929809162x029id7131:24000
Vitale, extremely stony surface-Yeates Hollow, extremely stony surface-Northwater complex, 12 to 40 percent slopes145-F56426198862v083id7131:24000
Yeates Hollow, extremely stony surface-Manila-Softback complex, 12 to 40 percent slopes1622225131635822sltqid71419971:24000
Vitale, extremely stony surface-Yeates Hollow, extremely stony surface-Northwater complex, 12 to 40 percent slopes145464531635812v083id71419971:24000
Yeates Hollow-Vitale complex, 25 to 50 percent slopes1633737485257j8ygid71419971:24000
Manila-Yeates Hollow complex, 6 to 20 percent slopes941862485345j919id71419971:24000
Yeates Hollow cobbly loam, 12 to 35 percent slopes, extremely stony1611350485255j8ydid71419971:24000
Yeates Hollow family, extremely stony surface-Manila family, very stony surface, perched water table-Booneville complex, 5 to 35 percent slopes1088931734032x029id71419971:24000
Yeates Hollow, extremely stony surface-Manila-Softback complex, 12 to 40 percent slopes16223329844012sltqid7161:24000
Faim-Yeates Hollow complex, 5 to 40 percent slopes, very stony554614924989292pzwkut0131:24000
Manila-Yeates Hollow complex, 4 to 40 percent slopes, very stonyTVD101414840571lt8tut0131:24000
Yeates Hollow cobbly loam, 20 to 60 percent slopes, very stonyYHE25514755971ljgxut0131:24000
Yeates Hollow cobbly clay loam, 30 to 60 percent slopesYHG5036481528j525ut60219691:20000
Yeates Hollow-Goring association, steepYRE2124481529j526ut60219691:20000
Goring-Yeates Hollow association, moderately steepGLE2085481364j4wwut60219691:20000
Yeates Hollow cobbly clay loam, 20 to 30 percent slopesYHE1101481527j524ut60219691:20000
GORING-OBRAY ASSOCIATION, ERODEDGOE28438482719j69lut60319681:20000
YEATES HOLLOW COBBLY SILTY CLAY LOAM, 3 TO 30 PERCENT SLOPES, ERODEDYLE28092482864j6g8ut60319681:20000
YEATES HOLLOW COBBLY SILT LOAM, 6 TO 30 PERCENT SLOPESYHE5428482862j6g6ut60319681:20000
YEATES HOLLOW COBBLY SILT LOAM, 30 TO 70 PERCENT SLOPESYHG4372482863j6g7ut60319681:20000
Yeates Hollow-Obray complex, 6 to 25 percent slopesYBD8000503928jxcrut60419801:24000
Yeates Hollow gravelly loam, 25 to 40 percent slopesYAE760503927jxcqut60419801:24000
Yeates Hollow very stony loam, 25 to 40 percent slopesYaE11811482650j67cut60819811:24000
Wallsburg-Yeates Hollow complex, 40 to 70 percent slopesWdF9954482641j672ut60819811:24000
Yeates Hollow very stony loam, 10 to 25 percent slopesYaD3563482649j67but60819811:24000
Yeates Hollow very stony loam, 40 to 70 percent north slopesYbF2709482651j67dut60819811:24000
Wallsburg-Yeates Hollow complex, 25 to 40 percent slopesWdE2624482640j671ut60819811:24000
Yeates Hollow very stony loam, 6 to 10 percent slopesYaC1525482648j679ut60819811:24000
Yeates Hollow very stony loam, 10 to 30 percent slopesYcD9310506643k06but60919741:24000
Yeates Hollow-Smarts complex, 30 to 70 percent slopesYdG4640506644k06cut60919741:24000
Manila-Yeates Hollow complex, 10 to 25 percent slopesMcD1875506584k04fut60919741:24000
Manila-Yeates Hollow complex, 25 to 70 percent slopesMcG1520506585k04gut60919741:24000
Yeates Hollow cobbly loam, 6 to 10 percent slopesYbC705506642k069ut60919741:24000
Yeates Hollow loam, 2 to 5 percent slopesYaA265506641k068ut60919741:24000
Yeates Hollow cobbly loam, 6 to 20 percent slopes715965482182j5r8ut61119921:24000
Yeates Hollow very cobbly loam, 6 to 40 percent slopes723776482183j5r9ut61119921:24000
Yeates Hollow-Henefer complex, 30 to 60 percent slopes18217780508223k1v9ut61319991:24000
Yeates Hollow-Henefer complex, 15 to 30 percent slopes18113630508224k1vbut61319991:24000
Fewkes-Yeates Hollow complex, 15 to 30 percent slopes1356394508172k1snut61319991:24000
Fewkes-Yeates Hollow complex, 5 to 15 percent slopes1344004508179k1swut61319991:24000
Yeates Hollow-Henefer complex, 3 to 15 percent slopes1801591508225k1vcut61319991:24000
Yeates Hollow very cobbly loam, 15 to 25 percent slopesYED2468504320jxsdut62219671:24000
Yeates Hollow-Henefer association, moderately steepYTC749504321jxsfut62219671:24000
Yeates Hollow loam, 2 to 5 percent slopesYaB414504323jxshut62219671:24000
Yeates Hollow-Henefer association, hillyYTD259504322jxsgut62219671:24000
Yeates Hollow very cobbly loam, 6 to 15 percent slopesYEC200504319jxscut62219671:24000
Yeates Hollow stony silt loam, 20 to 40 percent slopesYHE11170482367j5y7ut62719711:24000
Bradshaw, moist-Yeates Hollow-Dunford families complex, 30 to 60 percent slopes145A32432842zsd2ut6451:24000
Cristo-Yeates Hollow families complex, 15 to 40 percent slopes15196732432862zsd4ut6451:24000
Collard-Yeates Hollow families complex, 15 to 40 percent slopes280621331285930gw3ut6451:24000
Yeates Hollow family, 30 to 50 percent slopes220625262nzmrut6491:24000
Yeates Hollow family, 15 to 30 percent slopes219625263nzmsut6491:24000
Yeates Hollow-Yeates Hollow, moderately deep families, complex, 15 to 40 percent slopes, stony222625260nzmput6491:24000
Yeates Hollow-Ostler, stony families, complex, 5 to 25 percent slopes221625261nzmqut6491:24000
Valmar, extremely stony-Yeates Hollow, rubbly families. complex, 25 to 60 percent slopes1351830791158vk87ut6511:24000
Rob Roy-Yeates Hollow-Goring families, complex, 3 to 15 percent slopes1361159791161vk8but6511:24000
Yeates Hollow-Henefer complex, 15 to 30 percent slopes5218714802421lp9rwy0411:24000

Map of Series Extent

Approximate geographic distribution of the YEATES HOLLOW 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 .