Official Series Description


Lab Data Summary

Aggregate lab data for the ROCKISLAND soil series. This aggregation is based on all pedons with a current taxon name of ROCKISLAND, 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 ROCKISLAND 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.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ROCKISLAND 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 ROCKISLAND 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 ROCKISLAND 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 ROCKISLAND 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 ROCKISLAND 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 ROCKISLAND 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 ROCKISLAND 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 ROCKISLAND, 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 ROCKISLAND 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
Quietus-Rockisland, very stony surface-Davtone families, complex, 15 to 40 percent slopes1075b666429808582x00nid7131:24000
Philipsburg-Rockisland complex, 8 to 35 percent slopes138E33028208402lwskmt60420011:24000
Bronec, stony-Rockisland association, 15 to 50 percent slopes85F28428208382djf1mt60420011:24000
Philipsburg-Rockisland complex, 8 to 35 percent slopes138E58326334332lwskmt60520071:24000
Rockisland, stony-Levengood-Cheadle, very stony complex, 15 to 35 percent slopes914E41025980212ppbcmt60520071:24000
Tibson, stony-Levengood complex, 15 to 50 percent slopes185F34024038052lpc3mt60520071:24000
Bronec-Tibson association, 15 to 50 percent slopes, stony85F17724037902lpbmmt60520071:24000
Rockisland, stony-Cheadle, very stony-Rock outcrop complex, 35 to 60 percent slopes914F7325980222ppbdmt60520071:24000
Rockisland gravelly loam, dry, 1 to 8 percent slopes285C3726334442pgdkmt60520071:24000
Rockisland gravelly loam, 1 to 8 percent slopes185C1326334452pgdlmt60520071:24000
Tibson-Rockisland-Philipsburg association, 15 to 50 percent slopes285F424962832lwsfmt60520071:24000
Bronec, stony-Rockisland association, 15 to 50 percent slopes85F1510722203142djf1mt61220111:24000
Tibson-Rockisland-Philipsburg association, 15 to 50 percent slopes285F1412824099842lwsfmt61220111:24000
Philipsburg-Rockisland complex, 8 to 35 percent slopes138E484824099882lwskmt61220111:24000
Rockisland gravelly loam, dry, 1 to 8 percent slopes285C445824864962pgdkmt61220111:24000
Maciver, very stony-Rockisland, stony complex, 15 to 50 percent slopes194F394324834192pc69mt61220111:24000
Rockisland gravelly loam, 1 to 8 percent slopes185C299624864972pgdlmt61220111:24000
Rockisland, stony-Levengood complex, 15 to 50 percent slopes185F284722203152djf2mt61220111:24000
Scravo-Rockisland association, 4 to 35 percent slopes455E149724099912lwsnmt61220111:24000
Rockisland-Shineberger, very stony complex, 4 to 15 percent slopes888D59424850182pdvwmt61220111:24000
Donald, very stony-Rockisland, very stony-Scudder, stony complex, 15 to 50 percent slopes360F55124253072mdqqmt61220111:24000
Maciver, very stony-Rockisland, stony complex, 15 to 50 percent slopes194F96325207272pc69mt61420121:24000
Rockisland, stony-Cheadle, very stony-Rock outcrop complex, 35 to 60 percent slopes914F71025187292ppbdmt61420121:24000
Rockisland, stony-Levengood-Cheadle, very stony complex, 15 to 35 percent slopes914E58425187282ppbcmt61420121:24000
Rockisland, very bouldery-Levengood-Farlin, very stony complex, 4 to 15 percent slopes883D33225187382ppbmmt61420121:24000
Bronec, stony-Rockisland association, 15 to 50 percent slopes85F28525208402djf1mt61420121:24000
Tibson-Rockisland-Philipsburg association, 15 to 50 percent slopes285F3425207282lwsfmt61420121:24000
Rockisland-Shineberger, very stony complex, 4 to 15 percent slopes888D2925416382pdvwmt61420121:24000
Philipsburg-Rockisland complex, 8 to 35 percent slopes138E1225207252lwskmt61420121:24000
Owenspring-Cheadle, extremely stony-Rockisland, stony families, complex, 4 to 25 percent slopes1175E589824376192mtjwmt6321:24000
Rockisland, stony-Wineglass families, complex, 4 to 35 percent slopes1127E40725128712qbyxmt6321:24000
Rockisland-Poso families, complex, 2 to 35 percent slopes2005E3384053316lzmt6331:24000
Owenspring-Cheadle, extremely stony-Rockisland, stony families, complex, 4 to 25 percent slopes1175E229796762mtjwmt63720141:24000
Morset-Rockisland complex, 1 to 6 percent slopes5261187725160502qftpwy6301:24000
Morset-Rockisland complex, 6 to 15 percent slopes527356125160512qftqwy6301:24000

Map of Series Extent

Approximate geographic distribution of the ROCKISLAND 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 .