Official Series Description


Lab Data Summary

Aggregate lab data for the CROGHAN soil series. This aggregation is based on all pedons with a current taxon name of CROGHAN, 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 CROGHAN 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
14240A0301S1957NY049001Croghan5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8477783,-75.4455566
14310N0308S09ME003004.CroghanCroghan6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6066667,-69.5866111

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CROGHAN 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 CROGHAN 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 CROGHAN 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 CROGHAN 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 CROGHAN 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 CROGHAN 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 CROGHAN 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.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

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Soil series sharing subgroup-level classification with CROGHAN, 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. ME-2010-09-03-05 | Franklin County Area and Part of Somerset County - 2003

    Typical pattern of the soils and underlying material in the Adams-Croghan-Naumburg general soil map unit (Soil Survey of Franklin County Area and Part of Somerset County, Maine; 2003).

  2. ME-2010-09-03-06 | Franklin County Area and Part of Somerset County - 2003

    Typical pattern of the soils and underlying material in the Colton-Sheepscot-Markey general soil map unit (Soil Survey of Franklin County Area and Part of Somerset County, Maine; 2003).

  3. ME-2012-02-03-10 | Oxford County Area - March 1995

    Typical pattern of the soils and underlying material in the Adams-Croghan-Colton general soil map unit (Soil Survey of Oxford County Area, Maine; March 1995).

  4. ME-2012-02-03-13 | York County - June 1982

    Typical pattern of soils and underlying material in the Adams-Colton association (Soil Survey of York County, Maine; June 1982).

  5. ME-2012-02-03-20 | York County - June 1982

    Typical pattern of soils and underlying material in the Naumburg-Croghan association (Soil Survey of York County, Maine; June 1982).

  6. NH-2012-02-14-03 | Cheshire County - June 1989

    Typical landscape pattern of soils and underlying material in the Colton-Adams general soil map unit (Soil Survey of Cheshire County, New Hampshire; June 1989).

  7. NH-2012-02-14-10 | Grafton County Area - 1999

    Typical pattern of soils and underlying material in the Adams-Colton unit (Soil Survey of Grafton County Area, New Hampshire; 1999).

  8. NH-2012-02-14-16 | Hillsborough County, Western Part - October 1985

    Typical landscape pattern of soils and parent material in the Colton-Adams-Naumburg association (Soil Survey of Hillsborough County, New Hampshire, Western Part; October 1985).

  9. NH-2012-02-14-27 | Sullivan County - December 1983

    Typical pattern of soils and underlying material in the Colton-Adams-Rumney unit (Soil Survey of Sullivan County, New Hampshire; December 1983).

  10. NY-2010-09-28-04 | Clinton County - 2006

    Typical pattern of deltaic sands and associated soils in the Champlain-Adams-Croghan general soil map unit (Soil Survey of Clinton County, New York; 2006).

  11. NY-2010-09-28-12 | Hamilton County - 2006

    Typical relationship of soils and underlying deposits in the Adams-Colton-Naumburg general soil map unit (Soil Survey of Hamilton County, New York; 2006).

  12. NY-2010-09-28-29 | St. Lawrence County - 2005

    Typical landscape of soils and underlying material in the Hogansburg-Muskellunge-Grenville association (Soil Survey of St. Lawrence County, New York; 2005).

  13. NY-2010-09-28-31 | Akwesasne Territory: St. Regis Mohawk Reservation - 2005

    One of three major rivers flows through Akwesasne. The Raquetter River sliced through glacial till ridges (consisting of Grenville, Hogansburg, and Malone soils) and deposited fine-grained sands at varying depths over silt, clay, or loamy till. The silt and clay sediments of Adjidaumo and Muskellunge soils are remnants of proglacial lake and marine environments (Soil Survey of Akwesasne Territory; St. Regis Mohawk Reservation; 2005).

Map Units

Map units containing CROGHAN 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
Croghan loamy fine sand, 3 to 8 percent slopes284B17512786229bxtma61419931:25000
Croghan loamy fine sand, 0 to 3 percent slopes284A5582786219bxsma61419931:25000
Adams-Croghan association, 0 to 15 percent slopesAGC44573157582w40gme00519691:24000
Naumburg-Croghan association, gently slopingNCB690315810blmfme00519691:24000
Croghan loamy fine sand, 3 to 8 percent slopesCrB4173157772x1f7me00519691:24000
Croghan loamy fine sand, 0 to 3 percent slopesCrA2883157762wqnzme00519691:24000
Croghan loamy fine sand, 0 to 8 percent slopes, woodedCrB307222846232wqp0me03119781:20000
Croghan-Urban land complex, 0 to 8 percent slopesCuB3632846242wqp2me03119781:20000
Adams-Croghan association, 0 to 15 percent slopesAFC88082849582w40gme61019921:20000
Croghan loamy fine sand, 0 to 8 percent slopes, woodedCuB27272849952wqp0me61019921:20000
Naumburg-Croghan complex, 0 to 8 percent slopesNAB541814830661ls7vme61220161:24000
Naumburg-Croghan complex, 0 to 8 percent slopesNcB59424819542p9p1me61220161:24000
Adams-Croghan association, 0 to 15 percent slopesAGC157422857282w40gme61319871:20000
Naumburg-Croghan association, gently slopingNCB125302858059ldjme61319871:20000
Croghan loamy fine sand, 3 to 8 percent slopesCrB52292857582x1f7me61319871:20000
Croghan loamy fine sand, 0 to 3 percent slopesCrA27552857572wqnzme61319871:20000
Nicholville-Croghan complex, 0 to 8 percent slopesNGB124022856092x1f0me61720041:24000
Sheepscot-Croghan-Kinsman complex, 0 to 8 percent slopesSJB100162856169l6fme61720041:24000
Adams-Croghan association, 0 to 8 percent slopesAGB46982855262x1cdme61720041:24000
Nicholville-Croghan complex, 8 to 15 percent slopesNGC10692856102x1f2me61720041:24000
Croghan loamy fine sand, 3 to 8 percent slopesCzB9142855572x1f7me61720041:24000
Adams-Croghan association, 0 to 8 percent slopesACB69032856482x1cdme61920051:24000
Roundabout-Croghan association, 0 to 8 percent slopesRUB47422856912x1f4me61920051:24000
Croghan-Adams association, 0 to 8 percent slopesCAB404025498892wqnhme62020111:24000
Naumburg-Croghan association, 0 to 8 percent slopesNCB328925498872qtl8me62020111:24000
Croghan-Adams association, 0 to 8 percent slopesCAB441325498382wqnhme62120111:24000
Naumburg-Croghan association, 0 to 8 percent slopesNCB69825498372qtjsme62120111:24000
Adams-Croghan association, 0 to 8 percent slopesASB762319084302x1cdme62220071:24000
Sheepscot-Croghan-Kinsman complex, 0 to 8 percent slopesSPB771909077222k4me62220071:24000
Croghan loamy fine sand, 0 to 8 percent slopes613B17392797032wqp1nh00519851:20000
Croghan loamy fine sand, 0 to 3 percent slopes61349262811402wqnznh00919861:24000
Croghan loamy fine sand, 0 to 8 percent slopesCyA6812797552wqp1nh01919811:20000
Croghan loamy fine sand, 0 to 3 percent slopes613A16612792012wqnznh60219831:20000
Croghan loamy fine sand, 3 to 8 percent slopes613B7282792022x1f7nh60219831:20000
Croghan loamy fine sand, 0 to 3 percent slopes613A336015977642wqnznh6031:24000
Croghan loamy fine sand, 3 to 8 percent slopes613B317815977662x1f7nh6031:24000
Croghan loamy fine sand, 0 to 8 percent slopes613B48932805362wqp1nh60720001:24000
Croghan loamy fine sand, 0 to 8 percent slopes, wooded613A158982802442wqp0nh60920071:24000
Croghan loamy fine sand, 0 to 3 percent slopesCxA23232901459qxjny01919951:24000
Croghan loamy fine sand, 3 to 8 percent slopesCxB23032901469qxkny01919951:24000
Croghan fine sand, 3 to 8 percent slopesCwB933316473bm9tny03120071:24000
Croghan fine sand, 0 to 3 percent slopesCwA709316474bm9vny03120071:24000
Naumburg-Croghan complex, 0 to 3 percent slopes365A502319785bqrnny03120071:24000
Au Gres-Scarboro-Croghan associationAda128992677430bmbrny03320181:24000
Naumburg-Croghan complex, 0 to 3 percent slopes365A68811913202226v6ny03320181:24000
Croghan-Naumburg complex, 0 to 3 percent slopes364A57891913203226v7ny03320181:24000
Croghan loamy sand, 0 to 3 percent slopesCna49462677466bmchny03320181:24000
Croghan loamy sand, 3 to 15 percent slopesCnb14282677506bmcjny03320181:24000
Croghan sandy loam over till, 0 to 6 percent slopesCqb12102677534bmccny03320181:24000
Croghan fine sand, 0 to 3 percent slopes395A7431913228226w1ny03320181:24000
Croghan fine sandy loam over clay, 0 to 6 percent slopesCpa6372677493bmclny03320181:24000
Croghan fine sand, 0 to 3 percent slopesCxA48627536372spk6ny03320181:24000
Croghan fine sand, 3 to 8 percent slopesCxB28727536382spk7ny03320181:24000
Croghan loamy sand over clay, 0 to 3 percent slopesCoa2322677550bmckny03320181:24000
Croghan fine sandy loam, 0 to 5 percent slopes1022A53316773981t9gmny03520071:24000
Naumburg-Croghan complex, 0 to 3 percent slopes365A2502915319sc7ny03520071:24000
Naumburg-Croghan complex365A47032919489sspny04119941:62500
Croghan-Naumburg complex, 0 to 3 percent slopes364A41552518237226v7ny04320181:24000
Naumburg-Croghan complex, 0 to 3 percent slopes365A39692514987226v6ny04320181:24000
Croghan fine sand, 0 to 3 percent slopes395A8792518271226w1ny04320181:24000
Croghan loamy fine sand, 0 to 3 percent slopes57A4826776019vcdny04320181:24000
Croghan-Naumburg complex, 0 to 3 percent slopes364A81592516797226v7ny04920181:24000
Croghan loamy fine sand, 0 to 5 percent slopesCoB68192677655bmjhny04920181:24000
Croghan fine sand, 0 to 3 percent slopes395A12082516846226w1ny04920181:24000
Naumburg-Croghan complex, 0 to 3 percent slopes365A7422516796226v6ny04920181:24000
Croghan fine sand, 0 to 8 percent slopesCxB35927537092spm1ny04920181:24000
Croghan loamy fine sand, 0 to 3 percent slopes57A1527536919vcdny04920181:24000
Croghan loamy fine sand, 0 to 3 percent slopes57A30562934589vcdny06519931:24000
Croghan loamy fine sand, 3 to 8 percent slopes57B19282934599vcfny06519931:24000
Naumburg-Croghan complex, 0 to 3 percent slopes365A373118089226v6ny06519931:24000
Croghan loamy fine sand, 0 to 6 percent slopesCrB13512935549vghny06719731:20000
Croghan loamy fine sand, 3 to 8 percent slopesCvB141772949269wwrny08919901:24000
Naumburg-Croghan complex365125862948729wv0ny08919901:24000
Croghan loamy fine sand, 0 to 3 percent slopesCvA101002949259wwqny08919901:24000
Croghan sand, 0 to 8 percent slopesCuB58672949249wwpny08919901:24000
Croghan loamy fine sand, 0 to 3 percent slopes20A722960539y23ny68919991:24000
Croghan loamy fine sand, 3 to 8 percent slopes38B10202829022x1f7vt00520061:20000
Croghan loamy fine sand, 0 to 3 percent slopes38A3012829012wqnzvt00520061:20000
Croghan loamy fine sand, 0 to 3 percent slopes38A206514010692wqnzvt00920121:
Croghan loamy fine sand, 3 to 8 percent slopes38B119414010702x1f7vt00920121:
Croghan loamy fine sand, 0 to 8 percent slopesCrB18182819032wqp1vt01519791:20000
Croghan loamy fine sand, 0 to 3 percent slopes27A6522834422wqnzvt01920051:20000
Croghan loamy fine sand, 3 to 8 percent slopes27B6082834432x1f7vt01920051:20000
Croghan and Sheepscot soils, 0 to 8 percent slopes71B30872832822wqnxvt02720001:20000
Urban land-Colton-Croghan complex, 0 to 8 percent slopes75B13872833089hszvt02720001:20000
Croghan and Sheepscot soils, 8 to 15 percent slopes71C3682832832wqnyvt02720001:20000

Map of Series Extent

Approximate geographic distribution of the CROGHAN 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 .