Official Series Description


Lab Data Summary

Aggregate lab data for the ALTICREST soil series. This aggregation is based on all pedons with a current taxon name of ALTICREST, 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 ALTICREST 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
12586P005785KY095007Alticrest6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9661102,-83.0999985
12597P040097TN035003Alticrest7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.02631,-85.1202393
12597P040597TN035008Alticrest7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8455544,-85.0654984
12597P040697TN035009Alticrest7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8455544,-85.0654984
12597P040797TN035010Alticrest7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.851265,-85.0702896
128VPI0133V1992-VA005-133Alticrest2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6891667,-80.1416667
147VPI0140V1992-VA005-140Alticrest2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8294444,-79.895
147VPI0141V1992-VA005-141Alticrest2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8313889,-79.8933333
147VPI0148V1992-VA005-148Alticrest2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6963889,-80.2747222
n/a94KY-133-00194KY-133-001Alticrest1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ALTICREST 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 ALTICREST 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 ALTICREST 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 ALTICREST 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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Competing Series

Soil series competing with ALTICREST 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 ALTICREST 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 ALTICREST 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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Click the image to view it full size.

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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 ALTICREST, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. KY-2010-09-03-14 | Knott and Letcher Counties - 2004

    Typical pattern of soils and their relationship to geology and topography in the Alticrest-Varilla-Shelocta-Jefferson general soil map unit and the Cloverlick-Highsplint-Guyandotte-Shelocta general soil map unit in Letcher County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).

  2. KY-2010-09-03-32 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Carpenter-Bledsoe-Berks general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  3. KY-2010-09-03-33 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Bledsoe-Gilpin general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  4. KY-2010-09-03-34 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Helechawa-Alticrest-Gilpin-Rock outcrop general soil map unit in Lee County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  5. KY-2010-09-03-35 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Gilpin-Latham general soil map unit in Lee County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  6. KY-2010-09-03-45 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Rigley-Bledsoe-Alticrest-Berks general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  7. KY-2012-02-01-41 | Powell and Wolfe Counties - September 1993

    Typical pattern of soils and parent material in the Carpenter-Bledsoe-Berks general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).

  8. KY-2012-02-01-44 | Powell and Wolfe Counties - September 1993

    Typical pattern of soils and parent material in the Helechawa-Alticrest-Gilpin-Rock outcrop general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).

  9. KY-2012-02-01-45 | Powell and Wolfe Counties - September 1993

    Typical pattern of soils and parent material in the Sheloctal-Gilpin-Latham general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).

  10. VA-2010-11-05-14 | Dickenson County - 2009

    An idealized cross-section of the north-central section of the survey area showing the relationship among landforms, geology, and soils. Geology adapted from "Geology of the Virginia Portion of the Clintwood and Jenkings East Quadrangles" (Diffenbach, 1988) (Soil Survey of Dickenson County, Virginia; 2009).

  11. VA-2010-11-05-26 | Lee County - 2006

    Typical pattern of soils in the Appalachian Plateau portion of Lee County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

  12. VA-2012-05-11-04 | Dickenson County - 2009

    An idealized cross-section of the north-central section of the survey area showing the relationship among landforms, geology, and soils. Geology adapted from “Geology of the Virginia Portion of the Clintwood and Jenkins East Quadrangles” (Diffenbach, 1988) (Soil Survey of Dickenson County, Virginia; 2009).

  13. VA-2012-05-11-07 | Lee County - 2006

    Typical pattern of soils in the Appalachian Plateau portion of Lee County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

Map Units

Map units containing ALTICREST 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
Helechawa-Alticrest-Rock outcrop complex, 30 to 50 percent slopesHeF90117275311vzmtky01120061:12000
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF1841929970762qyt0ky19919691:12000
Gilpin-Latham-Alticrest complex, 15 to 35 percent slopes, rockyGlE7131557794lqfcky61620041:24000
Alticrest-Ramsey-Rock outcrop complex, 20 to 65 percent slopesArF3251557748lqcwky61620041:24000
Alticrest-Ramsey-Wallen complex, 20 to 55 percent slopes, rockyAtF3825550721lh26ky62619971:24000
Varilla-Jefferson-Alticrest complex, 35 to 75 percent slopes, very rockyVaF3439550751lh35ky62619971:24000
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF1976129970772qyt0ky62819731:20000
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF2404029970782qyt0ky63019661:15840
Wallen-Ramsey-Alticrest complex, 15 to 60 percent slopes, very rocky5E2007740290svbbky63019661:15840
Latham-Gilpin-Alticrest complex, 20 to 65 percent slopesLeF29468550841lh62ky63419891:20000
Alticrest-Ramsey-Rock outcrop complex, 20 to 65 percent slopesArF13594550820lh5dky63419891:20000
Alticrest-Totz-Helechawa complex, rocky, 20 to 55 percent slopesAtF36395552108ljhyky63819891:24000
Alticrest-Ramsey complex, rocky, 20 to 60 percent slopesArF2308550926lh8tky64119941:24000
Ramsey-Alticrest-Rock outcrop complex, 5 to 20 percent slopesRaD5976624391782w2mktn70119851:24000
Dekalb-Alticrest complex, 35 to 55 percent slopes, very stony16E10787834339x065va00520031:24000
Dekalb-Alticrest complex, 15 to 35 percent slopes, very stony16D2321834338x064va00520031:24000
Alticrest-Dekalb complex, 8 to 15 percent slopes, very stony3C303834318x05hva00520031:24000
Dekalb-Alticrest complex, 35 to 55 percent slopes, very stony12E527014514681kqckva01720051:24000
Dekalb-Alticrest complex, 15 to 35 percent slopes, very stony12D257014514671kqcjva01720051:24000
Alticrest-Dekalb complex, 8 to 15 percent slopes, very stony3C51714514661kqchva01720051:24000
Ramsey-Alticrest-Rock outcrop complex, 35 to 80 percent slopes21F674423998812lk8jva05120081:24000
Alticrest fine sandy loam, 15 to 35 percent slopes, rocky1D220523998512lk7kva05120081:24000
Alticrest fine sandy loam, 35 to 55 percent slopes, rocky1E147723998522lk7lva05120081:24000
Dekalb-Alticrest complex, 35 to 55 percent slopes, very stony11F70225120342q7vfva09120101:24000
Dekalb-Alticrest complex, 15 to 35 percent slopes, very stony11E53025120332q7vdva09120101:24000
Alticrest-Dekalb complex, 8 to 15 percent slopes, very stony2C9325086302q7v0va09120101:24000
Wallen-Alticrest complex, 35 to 55 percent slopes, very stony34E5199521753khxrva10519971:24000
Wallen-Alticrest complex, 15 to 35 percent slopes, very stony34D1860521752khxqva10519971:24000
Alticrest-Gilpin complex, 15 to 35 percent slopes2D1251521763khy2va10519971:24000
Alticrest fine sandy loam, 25 to 40 percent slopes2E8618522161kjbxva18519961:24000
Alticrest fine sandy loam, 15 to 25 percent slopes2D1624522160kjbwva18519961:24000
Cedarcreek-Alticrest-Rock outcrop complex, 15 to 40 percent slopes, very stony14E1508522174kjcbva18519961:24000
Alticrest fine sandy loam, 7 to 15 percent slopes2C209522159kjbvva18519961:24000
Cedarcreek-Alticrest-Rock outcrop complex, 5 to 15 percent slopes, very stony14C98522173kjc9va18519961:24000
Varilla-Jefferson-Alticrest complex, 35 to 75 percent slopes, very rocky80G258225086192q7s3va19520101:24000
Ramsey-Alticrest-Rock outcrop complex, 35 to 80 percent slopes66G225825086042q7rkva19520101:24000
Wallen-Alticrest complex, 35 to 55 percent slopes, very stony82F154425086232q7ttva19520101:24000
Alticrest-Gilpin complex, 15 to 35 percent slopes4E98225074692q2y5va19520101:24000
Alticrest fine sandy loam, 35 to 55 percent slopes, rocky3F93925074682q2y4va19520101:24000
Alticrest fine sandy loam, 15 to 35 percent slopes, rocky3E92625074672q2y3va19520101:24000
Wallen-Alticrest complex, 15 to 35 percent slopes, very stony82E52725086222q7s4va19520101:24000
Alticrest-Ramsey-Wallen complex, 20 to 55 percent slopes, rocky5F31625074702q7nzva19520101:24000
McClung-Alticrest complex, 35 to 55 percent slopes, very rocky53F11125085832q7r1va19520101:24000
McClung-Alticrest complex, 35 to 55 percent slopes, stony52F6925085822q7r0va19520101:24000

Map of Series Extent

Approximate geographic distribution of the ALTICREST 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 .