Official Series Description


Lab Data Summary

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

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 FIVEBLOCK, 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-2010-09-03-12 | Knott and Letcher Counties - 2004

    Typical pattern of soils and their relationship to geology and topography in the Handshoe-Cloverlick-Fedscreek-Marrowbone general soil map unit in Knott County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).

  2. 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).

  3. KY-2010-09-03-16 | Knott and Letcher Counties - 2004

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

  4. KY-2010-09-03-18 | Lawrence and Martin Counties - 2005

    Typical pattern of soils, parent material, and topography in the Hazleton-Shelocta-Fiveblock and Grigsby-Shelocta-Orrville general soil map units. The Hazleton-Shelocta-Fiveblock general soil map unit is on the mountains and in the surface mined areas, and the Grigsby-Shelocta-Orrville general soil map unit is in the valleys (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).

  5. KY-2010-09-03-39 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Helechawa-Gilpin-Hazleton general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  6. KY-2010-09-03-41 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Kimper-Shelocta-Fedscreek-Gilpin general soil map unit in Magoffin County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  7. KY-2010-09-03-42 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Gilpin-Latham-Marrowbone general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  8. VA-2010-11-05-07 | Buchanan County -

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia).

  9. VA-2010-11-05-16 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  10. VA-2012-05-10-04 | Buchanan County - 2009

    An illustration of an area that has been surface-mined for coal that shows a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia; 2009).

  11. VA-2012-05-11-02 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  12. WV-2010-11-08-11 | Logan and Mingo Counties - 2008

    Typical relationship of the soils and the underlying parent material in the Matewan-Highsplint-Guyandotte general soil map unit. Surface coal mining is in scattered areas throughout the map unit. The terraced area on the right of the diagram illustrates a valley fill, which is a common method of disposal and reclamation of overburden from coal mining activities. The flat area on the upper left illustrates mountaintop removal (Soil Survey of Logan and Mingo Counties, West Virginia; 2008).

  13. WV-2010-11-08-12 | Logan and Mingo Counties - 2008

    Typical relationship of the soils and the underlying parent material in the Matewan-Pineville-Guyandotte general soil map unit (Soil Survey of Logan and Mingo Counties, West Virginia; 2008).

  14. WV-2012-03-23-01 | Boone County - June 1994

    Typical pattern of soils and parent material in the Dekalb-Pineville-Guyandotte general soil map unit (Soil Survey of Boone County, WV; 1994).

Map Units

Map units containing FIVEBLOCK 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
Kaymine, Fairpoint, and Fiveblock soils, benched, 2 to 70 percent slopes, very stonyKfF51793550742lh2wky62619971:24000
Fiveblock and Kaymine soils, 0 to 30 percent slopes, stonyFkE10364550731lh2jky62619971:24000
Fiveblock, Fairpoint, and Kaymine soils, 30 to 80 percent slopes, stonyFiF39182550903lh82ky64019961:24000
Fiveblock, Fairpoint, and Kaymine soils, 6 to 30 percent slopes, stonyFiD12417550902lh81ky64019961:24000
Fiveblock, Fairpoint, and Kaymine soils, 0 to 6 percent slopes, stonyFiB3697550901lh80ky64019961:24000
Kaymine, Bethesda, and Fiveblock soils, benched, 2 to 70 percent slopes, stonyKbF16828550940lh98ky64119941:24000
Kaymine, Bethesda, and Fiveblock soils, 0 to 20 percent slopes, stonyKbD3656550939lh97ky64119941:24000
Cedarcreek, Fiveblock, and Kaymine soils, 55 to 80 percent slopes, extremely stony3F1273216708821t2pfva02720061:24000
Fiveblock-Sewell complex, 0 to 15 percent slopes, extremely stony8C169216708961t2pwva02720061:24000
Kaymine-Fiveblock-Cedarcreek complex, 0 to 15 percent slopes, extremely stony15C168116709541t2rrva02720061:24000
Kaymine-Fiveblock-Cedarcreek complex, 0 to 15 percent slopes, extremely stony16C341523998732lk88va05120081:24000
Kaymine, Cedarcreek, and Fiveblock soils, 55 to 80 percent slopes, extremely stony15F324223998722lk87va05120081:24000
Kaymine-Fiveblock-Cedarcreek complex, 0 to 15 percent slopes, extremely stony34C202916718971t3r5va16720061:24000
Kaymine-Fiveblock complex, 55 to 80 percent slopes, extremely stony33F80816719001t3r8va16720061:24000
Kaymine and Fiveblock soils, 55 to 80 percent slopes, extremely stony39G1676825085652q7qgva19520101:24000
Kaymine-Fiveblock-Cedarcreek complex, 0 to 15 percent slopes, extremely stony42C729525085682q7qjva19520101:24000
Kaymine-Fiveblock-Rock outcrop complex, 0 to 15 percent slopes, very stony43C541525085692q7qkva19520101:24000
Fiveblock very channery sandy loam, very steep, extremely stonyFvF1295514856k8r8wv00519881:24000
Cedarcreek and Fiveblock soils, 25 to 75 percent slopes, very stony, reclaimedCfF647230548882xph3wv03919761:20000
Cedarcreek and Fiveblock soils, 8 to 25 percent slopes, very stony, reclaimedCfD440930548872xph2wv03919761:20000
Cedarcreek and Fiveblock soils, 0 to 8 percent slopes, very stony, reclaimedCfB307730548862xph1wv03919761:20000
Cedarcreek and Fiveblock soils, 25 to 75 percent slopes, very stony, unreclaimedCcF183730548732xb0lwv03919761:20000
Cedarcreek and Fiveblock soils, 25 to 75 percent slopes, very stony, unreclaimed, highwallChF133530548792xpgwwv03919761:20000
Cedarcreek and Fiveblock soils, 8 to 25 percent slopes, very stony, reclaimed, highwallCkD49630548822xpgzwv03919761:20000
Cedarcreek and Fiveblock soils, 25 to 75 percent slopes, very stony, reclaimed, highwallCkF38130548832xph0wv03919761:20000
Cedarcreek and Fiveblock soils, 8 to 25 percent slopes, very stony, unreclaimedCcD21730548722xpgtwv03919761:20000
Cedarcreek and Fiveblock soils, 8 to 25 percent slopes, very stony, unreclaimed, highwallChD14330548782xpgywv03919761:20000
Cedarcreek and Fiveblock soils, 0 to 8 percent slopes, very stony, unreclaimedCcB4830548712xpgvwv03919761:20000
Kaymine and Fiveblock soils, 35 to 65 percent slopes, extremely stonyKfF1921553374lktswv04320051:24000
Kaymine and Fiveblock soils, 0 to 8 percent slopes, extremely stonyKfB606553375lkttwv04320051:24000
Cedarcreek and Fiveblock soils, 25 to 75 percent slopes, very stony, unreclaimed, highwallChF50930548982xpgwwv07919811:20000
Cedarcreek and Fiveblock soils, 8 to 25 percent slopes, very stony, unreclaimedCcD18630548932xpgtwv07919811:20000
Cedarcreek and Fiveblock soils, 8 to 25 percent slopes, very stony, unreclaimed, highwallChD11330548972xpgywv07919811:20000
Cedarcreek and Fiveblock soils, 25 to 75 percent slopes, very stony, unreclaimedCcF9330548942xb0lwv07919811:20000
Cedarcreek and Fiveblock soils, 8 to 25 percent slopes, very stony, reclaimedCfD4730549002xph2wv07919811:20000
Cedarcreek and Fiveblock soils, 0 to 8 percent slopes, very stony, reclaimedCfB830548992xph1wv07919811:20000
Cedarcreek and Fiveblock soils, 0 to 8 percent slopes, very stony, unreclaimedCcB530548922xpgvwv07919811:20000
Fiveblock channery sandy loam, very steep, very stonyFvF1520515012k8x9wv09919931:24000
Fiveblock channery sandy loam, steepFvE605513494k7bbwv10919841:24000
Fiveblock and Kaymine soils, 35 to 80 percent slopes, extremely stonyFkF17385115554017sfhwv62020051:24000
Fiveblock and Kaymine soils, 0 to 15 percent slopes, extremely stonyFkC4235115553917sfgwv62020051:24000
Kaymine and Fiveblock soils, 35 to 65 percent slopes, extremely stonyKfF75115554917sfswv62020051:24000
Kaymine and Fiveblock soils, 0 to 8 percent slopes, extremely stonyKfB20115554817sfrwv62020051:24000
Fiveblock very channery sandy loam, very steep, extremely stonyFvF121724622232nn4kwv70520091:24000
Fiveblock channery sandy loam, very steep, extremely stonyFvF14552512853k7lcwv76720111:20000
Fiveblock channery sandy loam, 3 to 8 percent slopes, extremely stonyFvB8992512852k7lbwv76720111:20000

Map of Series Extent

Approximate geographic distribution of the FIVEBLOCK 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 .