Official Series Description


Lab Data Summary

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

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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 ANGELBASIN 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 ANGELBASIN 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 ANGELBASIN 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 hills figure.

Click the image to view it full size.

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 ANGELBASIN, 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 ANGELBASIN 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
Angelbasin-Typic Haplocryands-Lithic Dystrocryepts families, complex, glaciated ridges, belt geology2lg0q628508332lg0qid60419811:24000
Angelbasin-Typic Haplocryands-Lithic Dystrocryepts families, complex, glaciated ridges, belt geology220416723967562lg0qid6701:24000
Angelbasin family, glacial-valley floors, extremely bouldery46KA228628090912tr5kmt60319891:24000
Angelbasin family, moderately steep glacial-valley trains, extremely bouldery47KA39028090932tr5mmt60319891:24000
Angelbasin family, glacial-valley floors, extremely bouldery46KA5129953462tr5kmt63819851:24000
Angelbasin-Elkhorncrest-Muddycreek complex, 60 to 90 percent north slopes0819DN11625938481qyd7or60419881:24000
Bucketlake-Angelbasin-Rock outcrop complex, 0 to 30 percent slopes9399NO94631206851sglcor60720181:24000
Angelbasin-Mudlakebasin-Rock outcrop complex, 15 to 30 percent slopes9379BO73631206771sgkror60720181:24000
Angelbasin-Marblepoint-Rock outcrop complex, 30 to 90 percent slopes9402UR51831206862mtg1or60720181:24000
Angelbasin-Elkhorncrest-Rock outcrop complex, 30 to 60 percent slopes0821CR26231203431qyd9or60720181:24000
Angelbasin-Clarkscreek-Marblepoint complex, 15 to 60 percent slopes9404XO18231206881sglgor60720181:24000
Angelbasin-Elkhorncrest-Rock outcrop complex, 15 to 30 percent slopes0820BR7631203421qyd8or60720181:24000
Marblepoint-Angelbasin complex, 30 to 60 percent slopes9417CO3031206911sgn1or60720181:24000
Elkhorncrest-Angelbasin-Rock outcrop complex, 60 to 90 percent slopes0822DR1531203441qydbor60720181:24000
Muddycreek-Angelbasin complex, 30 to 60 percent south slopes0815CS53120231qv89or60720181:24000
Angelbasin-Elkhorncrest-Rock outcrop complex, 30 to 60 percent slopes0821CR53631221751qyd9or62620181:24000
Angelbasin-Elkhorncrest-Rock outcrop complex, 15 to 30 percent slopes0820BR43831221741qyd8or62620181:24000
Muddycreek-Angelbasin complex, 30 to 60 percent south slopes0815CS3303122090qv89or62620181:24000
Angelbasin-Mudlakebasin-Rock outcrop complex, 15 to 30 percent slopes9379BO12131224461sgkror62620181:24000
Elkhorncrest-Angelbasin-Rock outcrop complex, 60 to 90 percent slopes0822DR4031221761qydbor62620181:24000
Angelbasin-Marblepoint-Rock outcrop complex, 30 to 90 percent slopes9402UR2831224532mtg1or62620181:24000
Marblepoint-Angelbasin complex, 30 to 60 percent slopes9417CO2431224561sgn1or62620181:24000
Mudlakebasin-Angelbasin-Bucketlake complex, 15 to 30 percent slopes9413BO1117724375341sglnor63120181:24000
Angelbasin-Elkhorncrest-Rock outcrop complex, 30 to 60 percent slopes0821CR804924369891qyd9or63120181:24000
Muddycreek-Angelbasin complex, 30 to 60 percent south slopes0815CS63102436982qv89or63120181:24000
Mudlakebasin-Angelbasin-Marblepoint complex, 0 to 15 percent slopes0823AO60152436991qtywor63120181:24000
Angelbasin-Elkhorncrest-Rock outcrop complex, 15 to 30 percent slopes0820BR480724369881qyd8or63120181:24000
Elkhorncrest-Angelbasin-Rock outcrop complex, 60 to 90 percent slopes0822DR299824369901qydbor63120181:24000
Marblepoint-Angelbasin complex, 30 to 60 percent slopes9417CO267024375371sgn1or63120181:24000
Angelbasin-Marblepoint-Bucketlake complex, 60 to 90 percent north slopes9412DO152624869041sglmor63120181:24000
Angelbasin-Elkhorncrest-Muddycreek complex, 60 to 90 percent south slopes0816DS130124845581qyd2or63120181:24000
Angelbasin-Elkhorncrest-Muddycreek complex, 60 to 90 percent north slopes0819DN64524369871qyd7or63120181:24000
Angelbasin-Marblepoint-Rock outcrop complex, 30 to 90 percent slopes9402UR2624375312mtg1or63120181:24000
Angelbasin-Typic Haplocryands-Lithic Dystrocryepts families, complex, glaciated ridges, belt geology2lg0q8628509292lg0qwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the ANGELBASIN 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 .