Official Series Description


Lab Data Summary

Aggregate lab data for the ANGELPEAK soil series. This aggregation is based on all pedons with a current taxon name of ANGELPEAK, 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 ANGELPEAK 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
43C95P0902S1995OR023001Angelpeak6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7561111,-118.3427811

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ANGELPEAK 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 ANGELPEAK 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 ANGELPEAK 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 ANGELPEAK 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with ANGELPEAK 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 ANGELPEAK 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 ANGELPEAK 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with ANGELPEAK, 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 ANGELPEAK 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
Angelpeak-Vandamine complex, 30 to 60 percent slopes7806CO15825939501sghror60419881:24000
Angelpeak gravelly silt loam, 30 to 80 percent north slopes3F466220922qror60419881:24000
Angelpeak-Vandamine complex, 30 to 60 percent slopes7806CO766931206711sghror60720181:24000
Angelpeak-Bordengulch complex, 15 to 30 percent slopes7794BO697431206631sghgor60720181:24000
Towermountain-Angelpeak-Bordengulch complex, 0 to 15 percent slopes1328AO440231202711q718or60720181:24000
Angelpeak-Vandamine-Towermountain complex, 15 to 30 percent slopes1325BO428131203851qyz6or60720181:24000
Bordengulch-Angelpeak complex, 0 to 15 percent slopes7558AO367131206212pgszor60720181:24000
Angelpeak gravelly ashy silt loam, 15 to 30 percent slopes7768BO158231206531sgg0or60720181:24000
Towermountain-Angelpeak complex, 0 to 15 percent slopes1340AO139531203881qzf7or60720181:24000
Angelpeak-Bordengulch complex, 30 to 60 percent slopes1322CO130431203841qyz5or60720181:24000
Bordengulch-Angelpeak-Vandamine complex, 15 to 30 percent slopes7727BO9513120230qsqhor60720181:24000
Bordengulch-Angelpeak complex, 15 to 30 percent slopes7341BO77331206082pgssor60720181:24000
Angelpeak-Towermountain-Eastlakesbasin complex, 15 to 30 percent slopes1343BO75431203911qzfbor60720181:24000
Angelpeak-Bordengulch complex, 0 to 15 percent slopes7794AO66331207861v6m6or60720181:24000
Bordengulch-Angelpeak-Blackgulch complex, 30 to 60 percent slopes7363CO54831206152pgswor60720181:24000
Angelpeak-Bordengulch-Rock outcrop complex, 30 to 60 percent slopes7361CO33831206131sgbjor60720181:24000
Angelpeak-Bordengulch-Rock outcrop complex, 15 to 30 percent slopes7361BO32231206121sgbhor60720181:24000
Angelpeak-Bordengulch-Blackgulch complex, 0 to 15 percent slopes7362AO31831206141sgbkor60720181:24000
Angelpeak-Vandamine complex, 0 to 30 percent slopes1318NO28231203821qyz3or60720181:24000
Angelpeak-Bordengulch complex, sandstone substratum, frost, 0 to 15 percent slopes2012AF19731204241r00qor60720181:24000
Angelpeak-Towermountain complex, mass failure, 15 to 30 percent slopes1329BM19231203861qyzpor60720181:24000
Angelpeak-Vandamine complex, landslide, 15 to 30 percent slopes1318BL11931203811qyz2or60720181:24000
Angelpeak-Bordengulch complex, sandstone substratum, 30 to 60 percent slopes2012CO4931204251r00ror60720181:24000
Bordengulch-Angelpeak-Vandamine complex, 60 to 90 percent north slopes7727DN2731206351sgdpor60720181:24000
Angelpeak-Vandamine complex, 30 to 60 percent slopes7806CO77431224421sghror62620181:24000
Bordengulch-Angelpeak complex, 15 to 30 percent slopes7341BO44231223982pgssor62620181:24000
Bordengulch-Angelpeak-Vandamine complex, 15 to 30 percent slopes7727BO2623122089qsqhor62620181:24000
Bordengulch-Angelpeak complex, mass failure, 15 to 30 percent slopes7341BM14531223971sg9wor62620181:24000
Bordengulch-Angelpeak complex, 0 to 15 percent slopes7558AO10431224062pgszor62620181:24000
Angelpeak-Vandamine complex, 30 to 60 percent slopes7806CO820924869031sghror63120181:24000
Bordengulch-Angelpeak-Vandamine complex, 60 to 90 percent north slopes7727DN547624868911sgdpor63120181:24000
Bordengulch-Angelpeak-Vandamine complex, 15 to 30 percent slopes7727BO49942437485qsqhor63120181:24000
Angelpeak-Bordengulch complex, 15 to 30 percent slopes7794BO102424375051sghgor63120181:24000
Angelpeak gravelly ashy silt loam, 0 to 15 percent slopes7739AO73224374961sgf3or63120181:24000
Angelpeak-Fruitcreek complex, 30 to 60 percent slopes7738CO70424374951sgf2or63120181:24000
Angelpeak-Towermountain-Eastlakesbasin complex, 15 to 30 percent slopes1343BO68824861901qzfbor63120181:24000
Bordengulch-Angelpeak complex, 0 to 15 percent slopes7558AO47224868812pgszor63120181:24000
Angelpeak-Vandamine-Towermountain complex, 15 to 30 percent slopes1325BO27624861851qyz6or63120181:24000
Towermountain-Angelpeak complex, 0 to 15 percent slopes1340AO25324861881qzf7or63120181:24000
Angelpeak-Fruitcreek complex, 15 to 30 percent slopes7738BO21924374941sgf1or63120181:24000
Angelpeak-Bordengulch-Blackgulch complex, 0 to 15 percent slopes7362AO21124868771sgbkor63120181:24000
Angelpeak-Bordengulch complex, 30 to 60 percent slopes1322CO9224861841qyz5or63120181:24000
Towermountain-Angelpeak-Bordengulch complex, 0 to 15 percent slopes1328AO8824861861q718or63120181:24000
Bordengulch-Angelpeak complex, 15 to 30 percent slopes7341BO724868752pgssor63120181:24000
Bordengulch-Angelpeak-Blackgulch complex, 30 to 60 percent slopes7363CO324868782pgswor63120181:24000
Angelpeak-Vandamine-Towermountain complex, 15 to 30 percent slopes1325BO8831214561qyz6or66719841:20000

Map of Series Extent

Approximate geographic distribution of the ANGELPEAK 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 .