Official Series Description


Lab Data Summary

Aggregate lab data for the GEOHROCK soil series. This aggregation is based on all pedons with a current taxon name of GEOHROCK, 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 GEOHROCK 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
4492P050291MT049004Geohrock7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7299004,-112.1442184

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GEOHROCK 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 GEOHROCK 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 GEOHROCK 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 GEOHROCK 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 GEOHROCK 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 GEOHROCK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the GEOHROCK 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.

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 GEOHROCK, 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 GEOHROCK 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
Geohrock-Bronec-Geohrock, stony complex, 8 to 45 percent slopes289E63631481904z6bmt60420011:24000
Geohrock, bouldery-Sappington, stony-Bronec, bouldery complex, 8 to 35 percent slopes189E43841482254z7gmt60420011:24000
Varney-Delpoint, stony-Geohrock complex, 4 to 35 percent slopes333E20671482664z8smt60420011:24000
Sappington-Geohrock-Delpoint, stony complex, 4 to 25 percent slopes278D15191482194z78mt60420011:24000
Geohrock very cobbly loam, very stony, 15 to 35 percent slopes49E10791481684z5mmt60420011:24000
Geohrock, stony-Bronec-Geohrock, extremely stony complex, 8 to 45 percent slopes288E101024508402n89cmt60420011:24000
Faith, rarely flooded-Geohrock, stony-Beavrock, occasionally flooded complex, 2 to 15 percent slopes9103D8001482514z89mt60420011:24000
Bronec, bouldery-Geohrock, extremely bouldery-Kalsted, stony complex, 4 to 35 percent slopes192E78624508382n899mt60420011:24000
Varney-Udecide-Geohrock complex, 4 to 15 percent slopes433D5831481864z66mt60420011:24000
Geohrock-Bronec gravelly loams, 2 to 8 percent slopes331C2711483794zdfmt60420011:24000
Bronec-Kalsted-Geohrock, very stony complex, 4 to 15 percent slopes628D3524508412n89dmt60420011:24000
Faith, rarely flooded-Geohrock, stony-Beavrock, occasionally flooded complex, 2 to 15 percent slopes9103D50185950720dz3mt60520071:24000
Bronec, bouldery-Geohrock, extremely bouldery-Kalsted, stony complex, 4 to 35 percent slopes192E2824038362n899mt60520071:24000
Bronec-Kalsted-Geohrock, very stony complex, 4 to 15 percent slopes628D806816875901tn2dmt61220111:24000
Geohrock, stony-Bronec-Geohrock, extremely stony complex, 8 to 45 percent slopes288E5914188701521blgmt61220111:24000
Bronec, bouldery-Geohrock, extremely bouldery-Kalsted, stony complex, 8 to 35 percent slopes192E4424185737220br7mt61220111:24000
Geohrock-Bronec complex, 2 to 8 percent slopes331C2673798352vsr9mt61220111:24000
Geohrock very cobbly loam, 15 to 35 percent slopes, very stony49E1531798347vsr4mt61220111:24000
Varney-Geohrock complex, 4 to 15 percent slopes, stony433D914798353vsrbmt61220111:24000
Geohrock, very stony-Dyce-Blackleaf, very stony complex, 2 to 8 percent slopes330C427189577821mq4mt61220111:24000
Geohrock, very stony-Dyce-Blackleaf, very stony complex, 8 to 25 percent slopes330E4081907071220gfmt61220111:24000
Varney-Delpoint, stony-Geohrock complex, 4 to 35 percent slopes333E7125976754z8smt61220111:24000
Geohrock-Bronec gravelly loams, 2 to 8 percent slopes331C18151510395257mt62719981:24000
Sappington-Geohrock complex, 2 to 8 percent slopes534C1382151116527qmt62719981:24000
Geohrock cobbly clay loam, 15 to 35 percent slopes, stony33E1366151044525dmt62719981:24000
Sappington-Geohrock complex, 8 to 15 percent slopes534D1020151117527rmt62719981:24000
Bronec-Geohrock-Rock outcrop complex, 15 to 45 percent slopes272E635150996523vmt62719981:24000
Geohrock, stony-Bronec, very stony, complex, 4 to 15 percent slopes334D501151042525bmt62719981:24000
Geohrock-Bronec gravelly loams, 8 to 15 percent slopes331D4561510405258mt62719981:24000
Geohrock cobbly clay loam, 1 to 4 percent slopes, stony451A453151089526vmt62719981:24000
Geohrock-Sappington complex, 4 to 15 percent slopes, stony332D2731510415259mt62719981:24000
Geohrock gravelly loam, 2 to 8 percent slopes3532B13115166652tgmt62719981:24000
Geohrock-Crago very cobbly loams, 2 to 8 percent slopes3233C4415165952t7mt62719981:24000
Geohrock-Tolman channery loams, 4 to 35 percent slopes163D90681477124ypxmt63019911:24000
Geohrock gravelly loam, 2 to 8 percent slopes532B89741478434yv4mt63019911:24000
Geohrock channery loam, cool, 4 to 25 percent slopes89D27521479344yy2mt63019911:24000
Geohrock-Crago very cobbly loams, 2 to 8 percent slopes233C25011477474yr1mt63019911:24000
Nippt-Geohrock gravelly loams, 2 to 4 percent slopes232B12461477464yr0mt63019911:24000
Geohrock family, moist, extremely stony-Gralic family, dry association, 30 to 70 percent slopes626518512416k66kut6461:24000
Geohrock-Foreleft complex, 5 to 30 percent slopesO40131709292z1yxwy6031:24000
Bonfri-Foreleft-Geohrock complex, 6 to 35 percent slopesS40131709272z1ywwy6031:24000
Zillman-Geohrock, stony-Amalia-like complex, 6 to 20 percent slopes931432066752zc61wy6291:24000
Hawksell-Hawksell-like-Geohrock, extremely bouldery complex, 6 to 20 percent slopes234932504652zv6pwy6291:24000
Birney, stony-Geohrock-Shermap-like, complex 10 to 40 percent slopes945132030652zbrwwy6291:24000
Evanston-Weed-Geohrock complex, 6 to 30 percent slopes241231368862ypppwy6291:24000
Kellycreek-Scotty-Geohrock complex, 1 to 25 percent slopes931131709512z1zfwy6291:24000
Foreleft-Bronec, very stony-Geohrock, stony complex, 20 to 50 percent slopes950231709532z1zhwy6291:24000
Geohrock, very stony-Swingstation-Bronec complex, 2 to 15 percent slopes931231709542z1zjwy6291:24000
Geohrock, very stony-Foreleft-Zillman complex, 4 to 30 percent slopes944131709952z20vwy6291:24000
Coyoteflats, stony-Geohrock-Pachel complex, 4 to 40 percent slopes945032030582zbrnwy6291:24000
Geohrock, very stony-Bronec-Foreleft complex, 6 to 55 percent slopes580432066712zc5xwy6291:24000
Mantlemine-Geohrock complex, 4 to 20 percent slopes931332066732zc5zwy6291:24000
Notter-Geohrock complex, 1 to 10 percent slopes8583365730312frwy6301:24000
Seminoe-Geohrock complex, 2 to 12 percent slopes70630038382x7bdwy6301:24000
Rock outcrop-Geohrock-Qcreek complex, 3 to 25 percent slopes880341043431g78wy6301:24000
Geohrock very gravelly sandy loam, 10 to 35 percent slopes8563365728312ftwy6301:24000
Geohrock gravelly sandy loam, 1 to 4 percent slopes2211246016722501t43kwy6351:24000
Foreleft-Bronec, very stony-Geohrock, stony complex, 20 to 50 percent slopes950232505392z1zhwy65620081:24000
Twinadams-Geohrock families, complex, 10 to 30 percent slopes4045579157882598zwy65620081:24000
Cusheet-Brickner-Geohrock family, complex, 15 to 45 percent slopes, rubbly surface4318340644731fxhwy7371:24000

Map of Series Extent

Approximate geographic distribution of the GEOHROCK 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 .