Official Series Description


Lab Data Summary

Aggregate lab data for the CODORUS soil series. This aggregation is based on all pedons with a current taxon name of CODORUS, 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 CODORUS 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
12895P008294VA167003Codorus6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9452782,-82.1483612
14804N024903PA029014Codorus7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.862278,-75.7835312
14800P1339S2000MD005005Codorus7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3028194,-76.7042222
14800P1090S2000VA047020Codorus3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.460358,-77.949786

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CODORUS 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 CODORUS 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 CODORUS 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 CODORUS 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 mountains figure.

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Competing Series

Soil series competing with CODORUS 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 CODORUS 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 CODORUS 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.

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

Soil series sharing subgroup-level classification with CODORUS, 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. DC-2011-05-31-03 | District of Columbia - 1976

    Typical pattern of soils and parent material in the Manor-Glenelg association (Soil Survey of District of Columbia; 1976).

  2. DC-2011-05-31-04 | District of Columbia - 1976

    Diagram of fall line between the Piedmont Plateau and the Coastal Plain. Diagram also shows the relationship of parent material and topography (Soil Survey of District of Columbia; 1976).

  3. MD-2010-09-07-03 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Mt. Airy-Glenelg-Blocktown general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  4. MD-2010-09-10-01 | Cecil County -

    Elsinboro-Delanco-Sassafras association (Soil Survey of Cecil County, Maryland).

  5. MD-2010-09-10-02 | Cecil County -

    Glenelg-Brinklow-Manor-Glenville association (Soil Survey of Cecil County, Maryland).

  6. MD-2010-09-10-06 | Howard County - 2008

    Relationship of soils, topography, and underlying material in the Occoquan-Brinklow-Glenelg general soil map unit (Soil Survey of Howard County, Maryland; 2008).

  7. MD-2012-02-03-18 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Mt. Airy-Glenelg-Blocktown general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  8. PA-2010-09-30-03 | Adams County - 2005

    Typical pattern of soils and parent material in the Edgemont-Highfield-Catoctin general soil map unit (Soil Survey of Adams County, Pennsylvania; 2005).

  9. PA-2010-09-30-16 | York County - 2002

    Typical pattern of soils and parent material in the Chester-Glenelg general soil map unit (Soil Survey of York County, Pennsylvania; 2002).

  10. PA-2010-09-30-17 | York County - 2002

    Typical pattern of soils and parent material in the Mt. Airy-Manor general soil map unit (Soil Survey of York County, Pennsylvania; 2002).

  11. PA-2012-03-13-71 | Montgomery County - April 1967

    Typical landscape in the southern part of Montgomery County, showing the pattern of soils formed on schist and the relationship of the soils in the pattern (Soil Survey of Montgomery County, PA; 1967).

  12. VA-2010-11-05-09 | Culpeper County -

    Relationship of soils and landscape in the Piedmont Granite Gneiss (Soil Survey of Culpeper County, Virginia).

  13. VA-2010-11-05-12 | Culpeper County -

    Relationship of soils and landscape in the Southern Piedmont Schist and Metamonzonite (Soil Survey of Culpeper County, Virginia).

  14. VA-2010-11-05-13 | Culpeper County -

    Relationship of soils and landscape in the Piedmont Metabasalt (Soil Survey of Culpeper County, Virginia).

Map Units

Map units containing CODORUS 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
Codorus silt loamCk19112858849t0dc00119751:12000
Codorus-Urban land complexCn10812858949t1dc00119751:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHw355324798542p7h9de00320091:24000
Delanco-Codorus-Hatboro complex, 0 to 8 percent slopes, floodedDcB250724798602p7hhde00320091:24000
Codorus silt loam, 0 to 3 percent slopes, occasionally floodedCh25224798552p7hbde00320091:24000
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently floodedCHA17321377334mb0md00320031:12000
Comus and Codorus soils, 0 to 2 percent slopes, occasionally floodedCTA396609572ng9mmd00320031:12000
Codorus silt loams, 0 to 3 percent slopesCfA1157924036562lp69md00520101:12000
Codorus silt loam, 0 to 3 percent slopesCdA503724957732ptj9md01320101:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, floodedHw333824406992mxr7md01520091:12000
Codorus silt loam, 0 to 3 percent slopes, occasionally floodedCh122424407002mxr8md01520091:12000
Delanco-Codorus-Hatboro complex, 0 to 8 percent slopes, floodedDcB36624407082mxrjmd01520091:12000
Codorus and Hatboro silt loams, 0 to 3 percent slopesCgA6347534793kyhdmd02120011:12000
Hatboro-Codorus silt loams, 0 to 3 percent slopesHdA4246534818kyj6md02120011:12000
Mt. Zion-Codorus complex, 0 to 8 percent slopesMoB1367535039kyrbmd02120011:12000
Glenville-Codorus complex, 3 to 8 percent slopesGvB1131559042lrqmmd02120011:12000
Glenville-Codorus complex, 0 to 3 percent slopesGvA293534973kyp6md02120011:12000
Codorus and Hatboro silt loams, 0 to 3 percent slopesCo5055792809vlzhmd02720041:12000
Hatboro-Codorus silt loams, 0 to 3 percent slopesHa4167793006vm5vmd02720041:12000
Glenville-Codorus silt loams, 0 to 8 percent slopesGoB1086793004vm5smd02720041:12000
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently floodedCp24514793971lnfhmd02720041:12000
Codorus silt loam, 0 to 3 percent slopes, occasionally flooded53A3640533646kx9dmd03119891:15840
Codorus and Hatboro soils, frequently floodedCF250124552972ndy4md03320091:12000
Codorus-Hatboro-Urban land complex, frequently floodedCh123024552982ndy5md03320091:12000
Codorus gravelly sandy loamCn148534210kxwlmd04319981:12000
Codorus silt loamCm133534205kxwfmd04319981:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently flooded50A7835338862w06dmd51019931:12000
Codorus silt loamCu6992533371kx0jmd60019721:15840
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcA33095333532w06dmd60019721:15840
Codorus loamCd5531295964bvjmd60119981:12000
Codorus loam, 0 to 2 percent slopes, frequently floodedCoA627923903442l7bwnc00319881:24000
Codorus loam, 0 to 2 percent slopes, frequently floodedCnA755926792092r925nc02720121:12000
Codorus loam, 0 to 2 percent slopes, frequently floodedCsA794729738882wx18nc03320161:24000
Codorus loam, 0 to 2 percent slopes, frequently floodedCsA587424312642mlxwnc03519691:15840
Codorus loam, 0 to 2 percent slopes, frequently floodedCwA56124328272mnk9nc05719851:24000
Codorus loam, 0 to 2 percent slopes, frequently floodedCoA1149024246202md0knc05919881:24000
Codorus loam, 0 to 2 percent slopes, frequently floodedCoA1595624335182mp8lnc06719701:15840
Codorus loam, 0 to 2 percent slopes, frequently floodedCnA477724330732mnt7nc08119751:20000
Codorus loam, 0 to 2 percent slopes, frequently floodedCsA1030724244772mcvync09720111:12000
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently floodedCoA354124392852mw8mnc14519871:24000
Codorus loam, 0 to 2 percent slopes, frequently floodedCsA1247023890432l5zxnc15719831:24000
Codorus loam, 0 to 2 percent slopes, occasionally floodedCsA272423884592l5d2nc16919921:24000
Codorus loam, 0 to 2 percent slopes, frequently floodedCoA1127023890612l60hnc19319931:24000
Codorus loam, 0 to 2 percent slopes, occasionally floodedCrA417923967492lg0hnc19719601:15840
Dan River and Codorus soils, 0 to 2 percent slopes, occasionally floodedDhA99623983522lhp6nc19719601:15840
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt273214239872w06gnj01919701:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt282514036802w06gnj02119691:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt23813954112w06gnj02319851:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt439914440352w06gnj02719741:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt206914049872w06gnj03519721:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt122614526612w06gnj03919891:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHcuAt3811474812w06gnj04120071:12000
Codorus silt loamCm2195545570l9q1pa00119911:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHbA12585436372w06gpa01719971:24000
Codorus silt loamCo7359641418pjfxpa02920081:24000
Codorus silt loam, 0 to 3 percent slopes, occasionally floodedCmA230598446530cdtpa04519601:20000
Codorus silt loamCh1430541164l53xpa09120081:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHbA1805432762w06gpa09520071:12000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedHbA11314795062w06gpa10119711:15840
Codorus silt loamCh6423962002lffspa10119711:15840
Codorus silt loamCm16123542831l6vppa13319901:24000
Codorus silt loam, 0 to 2 percent slopes, occasionally flooded1652105163122v7hpva00319811:15840
Dan River-Codorus complex, 0 to 2 percent slopes, occasionally flooded7733805164672v7k0va00319811:15840
Codorus silt loam, 0 to 3 percent slopes, frequently flooded7A19411366944l7hva00920041:24000
Urban land-Codorus complex, 0 to 3 percent slopes3A134123058441mva01320021:24000
Codorus-Hatboro complex, 0 to 3 percent slopes, frequently flooded2A15123049441bva01320021:24000
Codorus loam, 0 to 2 percent slopes, occasionally flooded8A34371359952xx5yva01919851:24000
Codorus-Hatboro complex, 0 to 3 percent slopes, frequently flooded12A2012924793792p6zzva02920101:24000
Codorus silt loamCo1757519200kf8dva03519651:15840
Codorus-Hatboro silt loamsCs840519201kf8fva03519651:15840
Codorus and Meadowville soils, 2 to 7 percent slopes, occasionally flooded11B977817263031vyc6va04720061:24000
Codorus silt loam, 0 to 2 percent slopes, occasionally flooded12A642317263051vyc8va04720061:24000
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently flooded10A136017263021vyc5va04720061:24000
Codorus loam, 0 to 2 percent slopes, frequently flooded12A99615874031q8tkva04920051:24000
Codorus and Hatboro soils, 0 to 2 percent slopes, occasionally flooded30A1216522503192fjmyva05920071:12000
Codorus silt loam, 0 to 2 percent slopes, occasionally flooded29A310022503152fjmtva05920071:12000
Wheaton-Codorus complex, 0 to 2 percent slopes103A234622505482fjwbva05920071:12000
Codorus loam, 0 to 2 percent slopes, frequently flooded2A8867189524421m4xva06120061:12000
Codorus loam, 0 to 3 percent slopes, frequently flooded6A25871914762228gjva06320071:24000
Codorus loam, 0 to 3 percent slopes, frequently flooded12A470916705031t296va07720061:24000
Suches-Codorus complexSc2110516906kbwdva07919831:15840
Codorus silt loamCn588516883kbvnva07919831:15840
Codorus and Hatboro soils, 0 to 2 percent slopes, frequently flooded14A2283114728051lfkvva08320041:24000
Codorus loam, 0 to 2 percent slopes, occasionally flooded13A463714728041lfktva08320041:24000
Codorus loam, 0 to 2 percent slopes, frequently flooded5A279212239243c4va08919951:24000
Codorus silt loam, 0 to 2 percent slopes, occasionally flooded2A6043642008pk1yva10720061:12000
Codorus loam, cobbly subsoil variantCn1752516957kby1va11319671:15840
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedAc4455169152w06dva11319671:15840
Codorus silt loam, 0 to 2 percent slopes, occasionally flooded8A26261371864lrcva12519921:24000
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedMx48961198822w06dva13719661:15840
Codorus silt loam, 0 to 2 percent slopes, frequently floodedCw39591198092z1whva13719661:15840
Codorus-Comus complex, 0 to 2 percent slopes, frequently flooded8A219051201632yzrnva14319891:24000
Codorus loam, 0 to 2 percent slopes, occasionally flooded7A36421201622yzrmva14319891:24000
Hatboro-Codorus complex, 0 to 2 percent slopes27A3742521170kh9yva15319851:15840
Codorus loam, 0 to 2 percent slopes14A385521148kh97va15319851:15840
Hatboro-Codorus complex, 0 to 3 percent slopes, frequently floodedAd16545173922w06dva15719581:20000
Codorus loam, cobbly subsoil variantCn173098281kby1va15719581:20000
Codorus and Hatboro soils, 0 to 2 percent slopes, occasionally flooded30A2291912968226lnva51020071:12000
Wheaton-Codorus complex, 0 to 2 percent slopes103A111912990226mcva51020071:12000
Codorus loam, 0 to 2 percent slopes, frequently flooded52A7523738072kp4fva51520081:24000
Dan River-Codorus complex, 0 to 2 percent slopes, occasionally flooded7715724964552v7k0va54020111:24000
Codorus silt loam, 0 to 2 percent slopes, occasionally flooded165824964262v7hpva54020111:24000
Codorus silt loam, 0 to 2 percent slopes, occasionally flooded29A10319078832219mva60020071:12000
Codorus and Hatboro soils, 0 to 2 percent slopes, occasionally flooded30A7619078822219lva60020071:12000
Wheaton - Codorus complex, 0 to 2 percent slopes103A5819078942219zva60020071:12000
Codorus and Hatboro soils, 0 to 2 percent slopes, occasionally flooded30A11190783722184va61020071:12000

Map of Series Extent

Approximate geographic distribution of the CODORUS 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 .