Official Series Description


Lab Data Summary

Aggregate lab data for the MORRIS soil series. This aggregation is based on all pedons with a current taxon name of MORRIS, 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 MORRIS 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
14058PA1150031958PA115003Morris5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6988889,-75.8277778
14058PA1150171958PA115017Morris5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6597222,-75.9244444
14066PA0690011966PA069001Morris4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4919444,-75.6913889
14066PA0690031966PA069003Morris3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5405556,-75.6841667
14071PA0890811971PA089081Morris5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0141667,-75.2852778
14085PA0690221985PA069022Morris4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5991667,-75.7102778
14085PA0690231985PA069023Morris3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5991667,-75.7102778
14085PA1030411985PA103041Morris4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.315,-75.0227778
14085PA1150351985PA115035Morris2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6552778,-75.8494444
14085PA1270031985PA127003Morris3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9069444,-75.4061111
14088PA0810751988PA081075Morris4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5716667,-76.8152778
14088PA1130061988PA113006Morris5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3586111,-76.3619444
14087P021886NY025006Morris4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3869438,-75.0924988
14093P081593PA103105Morris7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3461113,-75.1594467
14092P0035S1991NY077001Morris7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4208336,-75.1116638
14093P0629S1993NY025004Morris7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3266678,-74.775444

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MORRIS 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 MORRIS 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 MORRIS 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 MORRIS 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 terrace figure.

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Competing Series

Soil series competing with MORRIS 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 MORRIS 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 MORRIS 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.

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

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 MORRIS, 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. NY-2010-09-28-10 | Delaware County - 2006

    Typical pattern of soils and geologic materials in the Lackawanna-Wellsboro, Tunkhannock-Maplecrest-Barbour, and Oquaga-Lordstown-Arnot general soil map units (Soil Survey of Delaware County, New York; 2006).

  2. NY-2010-09-28-19 | Otsego County - 2006

    Typical pattern of soils and underlying material in the Wellsboro-Oquaga-Lackawanna general soil map unit (Soil Survey of Otsego County, New York; 2006).

  3. NY-2012-02-15-01 | Albany County - June 1992

    Typical pattern of soils and parent material in the Wellsboro-Lackawanna-Morris unit (Soil Survey of Albany County, New York; June 1992).

  4. NY-2012-02-15-23 | Greene County - February 1993

    Typical pattern of soils and underlying material in the Wellsboro-Oquaga-Morris association (Soil Survey of Greene County, New York; February 1993).

  5. NY-2012-02-15-46 | Sullivan County - July 1989

    Typical landscape pattern of the soils and the underlying material in the Wellsboro-Oquaga-Lackawanna general soil map unit (Soil Survey of Sullivan County, New York; July 1989).

  6. PA-2012-03-12-23 | Bradford and Sullivan Counties - August 1986

    Typical pattern of soils and parent material in the Morris-Oquaga-Wellsboro map unit (Soil Survey of Bradford and Sullivan Counties, PA; 1986).

  7. PA-2012-03-12-24 | Bradford and Sullivan Counties - August 1986

    Typical pattern of soils and parent material in the Wellsboro-Oquaga-Morris map unit (Soil Survey of Bradford and Sullivan Counties, PA; 1986).

  8. PA-2012-03-13-43 | Lackawanna and Wyoming Counties - March 1982

    Typical pattern of soils and underlying material in the Wellsboro-Morris-Oquaga association (Soil Survey of Lackawanna and Wyoming Counties, PA; 1982).

  9. PA-2012-03-13-54 | Luzerne County - October 1981

    Typical pattern of soils and underlying material in association 1 (Soil Survey of Luzerne County, PA; 1981).

  10. PA-2012-03-13-65 | Monroe County - August 1981

    Typical pattern of soils and underlying material in the Lackawanna-Wellsboro-Oquaga map unit (Soil Survey of Monroe County, PA; 1981).

  11. PA-2012-03-13-67 | Monroe County - August 1981

    Typical pattern of soils and underlying material in the Lordstown-Oquaga map unit (Soil Survey of Monroe County, PA; 1981).

  12. PA-2012-03-14-19 | Tioga County - June 1981

    Typical pattern of soils in the Morris-Oquaga-Wellsboro association (Soil Survey of Tioga County, PA; 1981).

  13. PA-2012-03-14-20 | Tioga County - June 1981

    Typical pattern of soils in the Oquaga-Lordstown association (Soil Survey of Tioga County, PA; 1981).

  14. PA-2012-03-14-32 | Wayne County - September 1985

    Typical pattern of soils and underlying material in the Oquaga-Wellsboro-Arnot association (Soil Survey of Wayne County, PA; 1985).

Map Units

Map units containing MORRIS 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
Morris channery silt loam, 3 to 8 percent slopesMoB23902887602vcltny00119851:15840
Morris channery silt loam, 8 to 15 percent slopesMoC6292887612vclvny00119851:15840
Morris channery silt loam, 3 to 8 percent slopes, extremely stonyMrB4092887622vxcwny00119851:15840
Morris silt loam, 8 to 15 percent slopes216C8083181582vcm4ny00320131:24000
Morris silt loam, 3 to 8 percent slopes216B543181592vcm3ny00320131:24000
Morris channery silt loam, 8 to 15 percent slopesMtC55862892022vclvny00719661:15840
Morris channery silt loam, 2 to 8 percent slopesMtB23302892012vclsny00719661:15840
Morris and Tuller soils, 3 to 25 percent slopes, very stonyMuD9622892032vxcsny00719661:15840
Volusia and Morris channery silt loams, 3 to 10 percent slopes, very stonyVpB242202900542srfpny01719821:15840
Morris channery silt loam, 3 to 8 percent slopesMoB64202900202vcltny01719821:15840
Morris channery silt loam, 8 to 15 percent slopesMoC22402900212vclvny01719821:15840
Morris channery silt loam, 0 to 3 percent slopesMoA5132900192vclpny01719821:15840
Morris and Volusia soils, 2 to 10 percent slopes, very stonyMsB52222905252srfqny02519991:24000
Morris flaggy silt loam, 3 to 8 percent slopesMrB45192905232vcm6ny02519991:24000
Morris flaggy silt loam, 8 to 15 percent slopesMrC41742905242vcm7ny02519991:24000
Lackawanna-Morris complex, 15 to 35 percent slopes, very stonyLcD18922904942vxcrny02519991:24000
Morris flaggy silt loam, 0 to 3 percent slopesMrA5612905222vcm5ny02519991:24000
Morris channery silt loam, 3 to 8 percent slopesMoB10032916812vcltny03919851:24000
Morris channery silt loam, 3 to 15 percent slopes, very stonyMpC4682916832vcmcny03919851:24000
Morris channery silt loam, 8 to 15 percent slopesMoC2272916822vclvny03919851:24000
Morris channery silt loam, 0 to 3 percent slopesMoA2172916802vclpny03919851:24000
Morris channery silt loam, 2 to 8 percent slopesMoB34002942572vclsny07719931:24000
Morris and Volusia soils, 3 to 15 percent slopes, extremely stonyMpC29892942592srfvny07719931:24000
Morris channery silt loam, 8 to 15 percent slopesMoC16252942582vclvny07719931:24000
Volusia, Morris, and Erie soils, 0 to 15 percent slopes, very stonyVmC146822945662srfsny09519651:15840
Morris stony silt loam, 2 to 8 percent slopesMoB25632945182vcm9ny09519651:15840
Morris stony silt loam, 8 to 15 percent slopesMoC9802945192vcmbny09519651:15840
Morris channery silt loam, gently sloping, extremely stonyMSB45552948422vxd1ny10119721:15840
Morris channery silt loam, 2 to 8 percent slopesMrB44012948402vclsny10119721:15840
Morris channery silt loam, 8 to 15 percent slopesMrC23432948412vclvny10119721:15840
Scriba and Morris loams, gently sloping, rubblySeB97192951252vxdtny10519841:15840
Morris loam, 3 to 8 percent slopesMrB70982950932vxdjny10519841:15840
Morris loam, 0 to 3 percent slopesMrA30602950922vxdhny10519841:15840
Morris loam, 8 to 15 percent slopesMrC12742950942vxdkny10519841:15840
Scriba and Morris soils, gently sloping, very boulderySEB94072955402vxd3ny11119741:15840
Morris-Tuller complex, gently sloping, very boulderyMTB38622955062vxd2ny11119741:15840
Scriba and Morris soils, gently sloping, extremely boulderySGB28652955412vxd4ny11119741:15840
Scriba and Morris soils, 0 to 8 percent slopesSdB4942955392vcm8ny11119741:15840
Morris channery silt loam, 0 to 8 percent slopes, extremely stonyMrB14995393922vxctpa02519601:20000
Morris channery silt loam, 3 to 8 percent slopesMrB234539538l3fgpa03719651:20000
Morris very stony silt loam, 0 to 8 percent slopesMsB226539539l3fhpa03719651:20000
Morris channery loam, 3 to 8 percent slopesMrB115922993142vxdfpa06919761:20000
Morris channery loam, 0 to 8 percent slopes, rubblyMxB93752993182vxdqpa06919761:20000
Morris channery loam, 8 to 15 percent slopesMrC48892993152vxdgpa06919761:20000
Morris flaggy loam, 3 to 8 percent slopesMsB32082993162vxdlpa06919761:20000
Morris channery loam, 8 to 25 percent slopes, rubblyMxD22282993192vxdspa06919761:20000
Morris flaggy loam, 8 to 15 percent slopesMsC15522993172vxdmpa06919761:20000
Morris channery loam, 0 to 3 percent slopesMrA14252993132vxddpa06919761:20000
Morris channery silt loam, 0 to 8 percent slopes, extremely stonyMsB164272964642vxctpa07919741:20000
Morris channery silt loam, 0 to 8 percent slopesMoB73322964622vclqpa07919741:20000
Morris channery silt loam, 8 to 15 percent slopesMoC14102964632vclvpa07919741:20000
Morris channery silt loam, 8 to 15 percent slopes, extremely stonyMsC11982964652vxcxpa07919741:20000
Morris channery silt loam, 0 to 8 percent slopes, extremely stonyMrB53765391022vxctpa08119811:20000
Morris channery silt loam, 3 to 8 percent slopesMoB25705391002vcltpa08119811:20000
Morris channery silt loam, 8 to 15 percent slopesMoC6505391012vclvpa08119811:20000
Morris channery silt loam, 0 to 8 percent slopes, extremely stonyMoB140302963392vxctpa08919751:20000
Morris channery silt loam, 2 to 10 percent slopesMgB13592963382vclrpa08919751:20000
Morris channery silt loam, 8 to 25 percent slopes, extremely stonyMoC8642963402vxcypa08919751:20000
Morris very channery loam, 0 to 8 percent slopes, very stony19B77842971942vxdnpa10319951:24000
Morris very channery loam, 8 to 15 percent slopes, very stony19C7332971952vxdppa10319951:24000
Morris and Volusia soils, 8 to 25 percent slopes, very stonyMrsD111629442392wbnvpa10519531:24000
Morris silt loam, 8 to 15 percent slopesMrC101424331682vcm4pa10519531:24000
Morris silt loam, 3 to 8 percent slopesMrB62224331672vcm3pa10519531:24000
Morris silt loam, 15 to 25 percent slopesMrD26218835732vxd0pa10519531:24000
Morris and Volusia soils, 0 to 8 percent slopes, very stonyMrsB15029442382wbntpa10519531:24000
Morris channery silt loam, 3 to 8 percent slopes, erodedMoB2215342970652vxd5pa11519681:20000
Morris flaggy silt loam, 3 to 8 percent slopes, erodedMrB2134522970672vxd7pa11519681:20000
Morris channery silt loam, 8 to 15 percent slopes, erodedMoC2129442970662vxd6pa11519681:20000
Morris channery silt loam, 0 to 8 percent slopes, extremely stonyMsB83252970702vxctpa11519681:20000
Morris flaggy silt loam, 8 to 15 percent slopes, erodedMrC279432970682vxdbpa11519681:20000
Morris channery silt loam, 8 to 25 percent slopes, extremely stonyMsD50852970712vxcypa11519681:20000
Morris channery silt loam, 0 to 3 percent slopesMoA21122970642vclppa11519681:20000
Morris flaggy silt loam, 15 to 25 percent slopes, erodedMrD27672970692vxdcpa11519681:20000
Morris gravelly silt loam, 8 to 15 percent slopesMoC165272971382vclypa11719731:20000
Morris gravelly silt loam, 3 to 8 percent slopesMoB148422971372vclxpa11719731:20000
Morris gravelly silt loam, 8 to 25 percent slopes, extremely stonyMsD36612971412vcm1pa11719731:20000
Morris gravelly silt loam, 0 to 8 percent slopes, extremely stonyMsB34182971402vcm0pa11719731:20000
Morris gravelly silt loam, 15 to 25 percent slopesMoD25772971392vclzpa11719731:20000
Morris gravelly silt loam, 0 to 3 percent slopesMoA22352971362vclwpa11719731:20000
Morris channery loam, 0 to 8 percent slopes, rubblyMxB399922966102vxdqpa12719771:20000
Morris channery loam, 3 to 8 percent slopesMoB199762966082vxdfpa12719771:20000
Morris channery loam, 8 to 15 percent slopes, rubblyMxC111502966112vxdrpa12719771:20000
Morris channery loam, 8 to 15 percent slopesMoC58752966092vxdgpa12719771:20000
Morris channery loam, 0 to 3 percent slopesMoA10302966072vxddpa12719771:20000
Morris channery loam, 0 to 8 percent slopes, rubblyMxB73943019472vxdqpa13119761:20000
Morris channery loam, 3 to 8 percent slopesMrB52433019432vxdfpa13119761:20000
Morris channery loam, 8 to 15 percent slopesMrC46473019442vxdgpa13119761:20000
Morris flaggy loam, 3 to 8 percent slopesMsB27623019452vxdlpa13119761:20000
Morris channery loam, 8 to 25 percent slopes, rubblyMxD10633019482vxdspa13119761:20000
Morris flaggy loam, 8 to 15 percent slopesMsC10353019462vxdmpa13119761:20000
Morris channery loam, 0 to 3 percent slopesMrA4633019422vxddpa13119761:20000
Morris channery silt loam, 3 to 8 percent slopes, extremely stonyMsB417712967702vxcwpa61019781:20000
Morris channery silt loam, 3 to 8 percent slopesMoB417192967682vcltpa61019781:20000
Morris channery silt loam, 8 to 15 percent slopesMoC416792967692vclvpa61019781:20000
Morris channery silt loam, 8 to 25 percent slopes, extremely stonyMsD230262967712vxcypa61019781:20000

Map of Series Extent

Approximate geographic distribution of the MORRIS 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 .