Official Series Description


Lab Data Summary

Aggregate lab data for the RIDGECREST soil series. This aggregation is based on all pedons with a current taxon name of RIDGECREST, 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 RIDGECREST 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 RIDGECREST 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 RIDGECREST 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 RIDGECREST 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 RIDGECREST 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 RIDGECREST 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 RIDGECREST 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 RIDGECREST 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 RIDGECREST, 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 RIDGECREST 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
Ridgecrest-Firading-Rock outcrop complex, 12 to 60 percent slopes43B72042424204102m7mrid65020111:24000
Hymas, extremely stony surface-Ridgecrest, stony surface-Wahtigup complex, 30 to 60 percent slopes233905731635082v068id70919761:24000
Ricrest-Ridgecrest, stony surface, complex, 20 to 60 percent slopes812781931635102v06did70919761:24000
Cedarhill, high precipitation-Hondoho-Ridgecrest complex, 20 to 50 percent slopes11180826832s16id70919761:24000
Ridgecrest-Hymas very cobbly loams, steepRGG7546828092s58id71019681:24000
Ridgecrest-Hymas gravelly loams, hillyREF2103828072s56id71019681:24000
Ridgecrest-Hymas very cobbly loams, hillyRGF1515828082s57id71019681:24000
Ridgecrest-Hymas complex, very steep, extremely stonyRHG1455828102s59id71019681:24000
Ricrest-Ridgecrest cobbly loams, steepRDG1189828062s55id71019681:24000
Ricrest-Ridgecrest gravelly loams, hillyRCF971828052s54id71019681:24000
Hymas, extremely stony surface-Ridgecrest, stony surface-Wahtigup complex, 30 to 60 percent slopes2319131636292v068id71019681:24000
Ricrest-Ridgecrest, stony surface, complex, 20 to 60 percent slopes814731732302v06did71019681:24000
Cedarhill, high precipitation-Hondoho-Ridgecrest, extremely stony surface, complex, 20 to 50 percent slopes35540331635302v06lid71119831:24000
Cedarhill-Hondoho-Ridgecrest complex, 25 to 55 percent slopes2096331732412rfzvid71119831:24000
Ridgecrest-Hondoho-Lizdale association, 30 to 60 percent slopes108-O74431733212v07did71220081:24000
Ridgecrest-Hymas association, 30 to 60 percent slopes109422226198402v07fid7131:24000
Hondoho-Ridgecrest-Hades association, 12 to 50 percent slopes43204326198472v06wid7131:24000
Ridgecrest-Hondoho-Lizdale association, 30 to 60 percent slopes108157426198392v07did7131:24000
Cedarhill-Hondoho-Ridgecrest complex, 25 to 55 percent slopes20948426198592rfzvid7131:24000
Ricrest-Ridgecrest, stony surface, complex, 20 to 60 percent slopes8128726198332v06did7131:24000
Cedarhill-Hondoho-Ridgecrest complex, 20 to 60 percent slopesBHG1672965723n4b8id7131:24000
Cedarhill, high precipitation-Hondoho-Ridgecrest, extremely stony surface, complex, 20 to 50 percent slopes3514625202152v06lid7131:24000
Hymas, extremely stony surface-Ridgecrest, stony surface-Wahtigup complex, 30 to 60 percent slopes23-P10326198302v068id7131:24000
Ridgecrest-Hondoho complex, 30 to 60 percent slopes1061226198772v07cid7131:24000
Cedarhill-Hondoho, stony surface-Ridgecrest, extremely stony surface complex, 20 to 50 percent slopes36514485280j8z6id71419971:24000
Ridgecrest-Hymas association, 30 to 60 percent slopes109-O2831733302v07fid71419971:24000
Ridgecrest-Hymas association, 30 to 60 percent slopes1093865231636102v07fid71519941:24000
Ridgecrest-Hondoho complex, 30 to 60 percent slopes1063046731636082v07cid71519941:24000
Hondoho-Ridgecrest-Hades association, 12 to 50 percent slopes432522331635922v06wid71519941:24000
Ridgecrest-Hondoho-Lizdale association, 30 to 60 percent slopes1081021931636092v07did71519941:24000
Ridgecrest-Hondoho-Hymas association, 30 to 60 percent slopes1079349485574j98pid71519941:24000
Calpac-Ridgecrest-Ireland association, 40 to 70 percent slopes178290485608j99sid71519941:24000
Cedarhill-Hondoho-Ridgecrest complex, 20 to 60 percent slopesBHG974599982n4b8id7161:24000
Ridgecrest-Hondoho-Lizdale association, 30 to 60 percent slopes108631365462v07did7161:24000
Ridgecrest-Firading-Rock outcrop complex, 12 to 60 percent slopes43B72094225185682qf5kid75819981:24000
Ridgecrest-Bickmore families association, 30 to 60 percent slopes7028335481282j4t7ut60119851:24000
Hymas, extremely bouldery-Ridgecrest families, complex, 8 to 25 percent slopes46A2542800714vw6hut6511:24000

Map of Series Extent

Approximate geographic distribution of the RIDGECREST 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 .