Official Series Description


Lab Data Summary

Aggregate lab data for the GOOSEROCK soil series. This aggregation is based on all pedons with a current taxon name of GOOSEROCK, 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 GOOSEROCK were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
1099P0255S1998OR023001GOOSEROCK6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5808334,-119.6413879

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GOOSEROCK 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 GOOSEROCK series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the GOOSEROCK series and siblings. 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 GOOSEROCK 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 .

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.

Competing Series

Soil series competing with GOOSEROCK 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 GOOSEROCK 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 GOOSEROCK 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 .

Click the image to view it full size.

Click the image to view it full size.

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 GOOSEROCK, 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 GOOSEROCK 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
Gooserock-Lickskillet-Rock outcrop complex, 30 to 60 percent north slopes107E868342501226h0or6271:24000
Gooserock-Drinkwater-Simas complex, 30 to 60 percent slopes105E5353425112nfp2or6271:24000
Gooserock-Brisbois-Badland complex, 40 to 60 percent north slopes124EG49134251132dv1vor6271:24000
Gooserock-Drinkwater-Bakeoven complex, 5 to 25 percent slopes102D327342505126gwor6271:24000
Gooserock-Meadowridge complex, 15 to 40 percent north slopes107D315342501726h1or6271:24000
Gooserock-Brisbois-Badland complex, 15 to 40 percent north slopes124D2073425072nfpror6271:24000
Simas-Gooserock complex, 20 to 50 percent north slopes145E2053425020nfq5or6271:24000
Gooserock complex, benched, 2 to 60 percent slopes106E2043425158nfp3or6271:24000
Gooserock-Drinkwater-Bakeoven complex, 40 to 60 percent slopes102E183342516326gvor6271:24000
Gooserock-Brisbois-Badland complex, 60 to 90 percent north slopes124F1113432226nfpsor6271:24000
Gooserock-Exfo-Rock outcrop complex, 30 to 50 percent north slopes100E10534251221hh1ror6271:24000
Gooserock-Exfo-Rock outcrop complex, 50 to 90 percent north slopes100F103342504926gror6271:24000
Gooserock gravelly ashy loam, 2 to 15 percent slopes107C513425074nfp4or6271:24000
Gooserock-Lickskillet-Rock outcrop complex, 30 to 60 percent north slopes107E10539342170026h0or6771:24000
Gooserock-Meadowridge complex, 15 to 40 percent north slopes107D7039342173026h1or6771:24000
Simas-Gooserock complex, 20 to 50 percent north slopes145E52153421743nfq5or6771:24000
Gooserock-Exfo-Rock outcrop complex, 50 to 90 percent north slopes100F1397342192126gror6771:24000
Gooserock-Drinkwater-Bakeoven complex, 5 to 25 percent slopes102D1331342193226gwor6771:24000
Gooserock-Brisbois-Badland complex, 15 to 40 percent north slopes124D6553424475nfpror6771:24000
Gooserock gravelly ashy loam, 2 to 15 percent slopes107C5893424483nfp4or6771:24000
Gooserock-Drinkwater-Simas complex, 30 to 60 percent slopes105E4573424542nfp2or6771:24000
Gooserock-Brisbois-Badland complex, 40 to 60 percent north slopes124EG42934245482dv1vor6771:24000
Gooserock-Exfo-Rock outcrop complex, 30 to 50 percent north slopes100E34134246091hh1ror6771:24000
Gooserock-Drinkwater-Bakeoven complex, 40 to 60 percent slopes102E102342477326gvor6771:24000
Gooserock complex, benched, 2 to 60 percent slopes106E543424754nfp3or6771:24000

Map of Series Extent

Approximate geographic distribution of the GOOSEROCK 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 .