Official Series Description


Lab Data Summary

Aggregate lab data for the HOLLIS soil series. This aggregation is based on all pedons with a current taxon name of HOLLIS, 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 HOLLIS 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
144A98P0355S1998NY061001Hollis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8708878,-73.923111
144A99P0553S1999CT005001Hollis6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9174843,-72.9431381
144A00P0011S1999NY061003Hollis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7983894,-73.9577484
144A00P0201S2000CT007004Hollis5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4749985,-72.3383331
144A01N0093S2000NY119001Hollis6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9944333,-73.7976139
144A02N1100S2002CT005005Hollis5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7521667,-73.4791389
144A02N1101S2002CT005006Hollis5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7556111,-73.4770833
144B02N1096S2002CT005001Hollis5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0031389,-73.0646667
144B02N1098S2002CT005003Hollis5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9426667,-73.2759444
144B02N1099S2002CT005004Hollis5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9434722,-73.2703056
144B02N1104S2002CT005009Hollis4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9863889,-73.3231944

Water Balance

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

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

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Competing Series

Soil series competing with HOLLIS 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 HOLLIS 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 HOLLIS 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 .

Click the image to view it full size.

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 HOLLIS, 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. CT-2011-05-31-01 | Fairfield County - 1981

    Typical pattern of soils and parent material in the Charlton-Hollis map unit (Soil Survey of Fairfield County, Conneticut; 1981).

  2. CT-2011-05-31-02 | Fairfield County - 1981

    Typical pattern soils and parent material in the Hollis-Charlton-Rock outcrop map unit (Soil Survey of Fairfield County, Conneticut; 1981).

  3. CT-2011-05-31-06 | New London County - 1983

    Typical pattern soils in the Charlton-Canton-Hollis general soil map unit (Soil Survey of New London County, Conneticut; 1983).

  4. CT-2011-05-31-07 | New London County - 1983

    Typical pattern of soils in the Woodbridge-Paxton-Montauk general soil map unit (Soil Survey of New London County, Conneticut; 1983).

  5. CT-2011-05-31-08 | New London County - 1983

    Typical pattern of soils in the Hinckley-Merrimac-Agawam general soil map unit (Soil Survey of New London County, Conneticut; 1983).

  6. CT-2011-05-31-09 | Windham County - 1981

    Typical pattern of soils and underlying material in the Charlton-Canton-Leicester association (Soil Survey of Windham County, Conneticut; 1981).

  7. MA-2010-09-07-03 | Hampden and Hampshire Counties, Western Part - 1995

    Pattern of soils and parent material in the Chatfield-Hollis-Montauk general soil map unit (Soil Survey of Hampden and Hampshire Counties, Western Part, Massachusetts; 1995).

  8. MA-2010-09-07-08 | Worcester County, Southern Part - 1998

    Typical pattern of soils and underlying material in the Paxton-Woodbridge-Ridgebury association (Soil Survey of Worcester County, Massachusetts, Southern Part; 1998).

  9. MA-2010-09-10-01 | Middlesex County - 2009

    A typical pattern of soils and underlying material in the Bernardston-Pittstown general soil map unit (Soil Survey of Middlesex County, Massachusetts; 2009).

  10. MA-2010-09-10-02 | Middlesex County - 2009

    A typical pattern of soils and underlying material in the Canton-Charlton-Hollis association (Soil Survey of Middlesex County, Massachusetts; 2009).

  11. MA-2010-09-10-05 | Middlesex County - 2009

    A typical pattern of soils and underlying material in the Narragansett-Haven association (Soil Survey of Middlesex County, Massachusetts; 2009).

  12. MA-2012-02-02-16 | Hampden and Hampshire Counties, Western Part - December 1995

    Pattern of soils and parent material in the Chatfield-Hollis-Montauk general soil map unit (Soil Survey of Hampden and Hampshire Counties, Western Part, Massachusetts; December 1995).

  13. MA-2012-02-02-19 | Hampshire County, Central Part - December 1981

    Soils, topography, and underlying material in the Charlton-Paxton-Woodbridge association (Soil Survey of Hampshire County, Massachusetts, Central Part; December 1981).

  14. MA-2012-02-02-23 | Norfolk and Suffolk Counties - September 1989

    Typical pattern of soils and underlying material in the Canton-Charlton-Hollis general soil map unit (Soil Survey of Norfolk and Suffolk Counties, Massachusetts; September 1989).

  15. MA-2012-02-02-25 | Plymouth County - 1969

    Relationship of soils to topography and underlying material in association 2 (Soil Survey of Plymouth County, Massachusetts; 1969).

  16. MA-2012-02-03-04 | Worcester County, Northeastern Part - December 1985

    Typical pattern of soils and parent material in the Chatfield-Hollis-Rock outcrop map unit (Soil Survey of Worcester County, Massachusetts, Northeastern Part; December 1985).

  17. MA-2012-02-03-05 | Worcester County, Southern Part - 1998

    Typical pattern of soils and underlying material in the Paxton-Woodbridge-Ridgebury association (Soil Survey of Worcester County, Massachusetts, Southern Part; 1998).

  18. MA-2012-02-03-06 | Worcester County, Southern Part - 1998

    Typical pattern of soils and underlying material in the Chatfield-Hollis association (Soil Survey of Worcester County, Massachusetts, Southern Part; 1998).

  19. NH-2012-02-14-22 | Rockingham County - October 1994

    Typical pattern of soils and parent material in the Canton-Chatfield-Hollis general soil map unit (Soil Survey of Rockingham County, New Hampshire; October 1994).

  20. NH-2012-02-14-23 | Strafford County - March 1973

    Typical pattern of soils and underlying material in the Gloucester-Hollis-Leicester association (Soil Survey of Strafford County, New Hampshire; March 1973).

  21. NH-2012-02-14-25 | Strafford County - March 1973

    Typical pattern of soils and underlying material in the Hollis-Charlton-Buxton-Scantic association (Soil Survey of Strafford County, New Hampshire; March 1973).

  22. NY-2012-02-15-40 | Rockland County - October 1990

    Relationship between soils, landscape position, and parent materials in Rockland County (Soil Survey of Rockland County, New York; October 1990).

Map Units

Map units containing HOLLIS 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
Hollis-Chatfield-Rock outcrop complex, 15 to 45 percent slopes75E7624833958159lqpct60120031:12000
Hollis-Chatfield-Rock outcrop complex, 3 to 15 percent slopes75C4617333958149lqnct60120031:12000
Rock outcrop-Hollis complex, 3 to 45 percent slopes76E852733958169lqqct60120031:12000
Rock outcrop-Hollis complex, 45 to 60 percent slopes76F676933958179lqrct60120031:12000
Hollis-Chatfield-Rock outcrop complex, 15 to 45 percent slopes75E2705934001889lqpct60220031:12000
Hollis-Chatfield-Rock outcrop complex, 3 to 15 percent slopes75C2309934001879lqnct60220031:12000
Narragansett-Hollis complex, 3 to 15 percent slopes, very rocky74C267934001869lqmct60220031:12000
Rock outcrop-Hollis complex, 3 to 45 percent slopes76E154134001899lqqct60220031:12000
Rock outcrop-Hollis complex, 45 to 60 percent slopes76F14834001909lqrct60220031:12000
Chatfield-Hollis complex, 25 to 60 percent slopes, rocky109F222302788419c4wma01120121:12000
Chatfield-Hollis complex, 15 to 25 percent slopes, rocky109D1520613956941hvbdma01120121:12000
Chatfield-Hollis complex, 8 to 15 percent slopes, rocky109C1340313956952w69lma01120121:12000
Chatfield-Hollis complex, 3 to 8 percent slopes, rocky109B545113956131hv7sma01120121:12000
Hollis-Chatfield complex, 8 to 15 percent slopes, very rocky114C41812788529c57ma01120121:12000
Canton-Chatfield-Hollis complex, 8 to 15 percent slopes, rocky112C35802789822w82cma01120121:12000
Canton-Chatfield-Hollis complex, 15 to 35 percent slopes, rocky112D30432789812w829ma01120121:12000
Canton-Chatfield-Hollis complex, 0 to 8 percent slopes, rocky112B19962789832w82bma01120121:12000
Charlton-Chatfield-Hollis complex, 8 to 15 percent slopes, rocky125C141413869591hk7mma01120121:12000
Charlton-Chatfield-Hollis complex, 15 to 25 percent slopes, rocky125D134313869601hk7nma01120121:12000
Charlton-Chatfield-Hollis complex, 3 to 8 percent slopes, rocky125B90025201232qk7xma01120121:12000
Charlton-Hollis-Rock outcrop complex, 3 to 8 percent slopes103B1380127671798ycma01719911:24000
Charlton-Hollis-Rock outcrop complex, 8 to 15 percent slopes103C129882767182wzp1ma01719911:24000
Charlton-Urban land-Hollis complex, 3 to 15 percent slopes, rocky631C12961796714vr1gma01719911:24000
Hollis-Rock outcrop-Charlton complex, 0 to 15 percent slopes104C111107963612w69pma01719911:24000
Hollis-Rock outcrop-Charlton complex, 15 to 25 percent slopes104D683927672198yhma01719911:24000
Rock outcrop-Hollis complex, 3 to 35 percent slopes105E620027672298yjma01719911:24000
Narragansett-Hollis-Rock outcrop complex, 3 to 15 percent slopes106C604827672398ykma01719911:24000
Charlton-Hollis-Rock outcrop complex, 15 to 25 percent slopes103D463727671998yfma01719911:24000
Narragansett-Hollis-Rock outcrop complex, 15 to 25 percent slopes106D235327672498ylma01719911:24000
Rock outcrop-Charlton-Hollis complex, 15 to 35 percent slopes717E4193790665vjrbma60519771:15840
Charlton-Rock outcrop-Hollis complex, 8 to 15 percent slopes711C4101790160vj71ma60519771:15840
Rock outcrop-Charlton-Hollis complex, 3 to 15 percent slopes717C2741790661vjr6ma60519771:15840
Charlton-Rock outcrop-Hollis complex, 3 to 8 percent slopes711B1647790157vj6yma60519771:15840
Charlton-Rock outcrop-Hollis complex, 15 to 25 percent slopes711D1311790166vj77ma60519771:15840
Rock outcrop-Hollis complex, 3 to 25 percent slopes105D166790667vjrdma60519771:15840
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopes102E179087910442w69hma60619811:15840
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopes102C107437910402w69gma60619811:15840
Hollis-Urban land-Rock outcrop complex, sloping724C2982791090vk61ma60619811:15840
Rock outcrop-Hollis complex, 3 to 25 percent slopes105D1850791266vkcqma60619811:15840
Charlton-Rock outcrop-Hollis complex, 15 to 25 percent slopes711D158827741299nsma60719751:15840
Charlton-Rock outcrop-Hollis complex, 3 to 15 percent slopes711C153327741199nrma60719751:15840
Hollis-Chatfield association, 15 to 45 percent slopes, very rocky912E35119030832wzp2ma60719751:15840
Charlton-Hollis-Rock outcrop complex, 8 to 15 percent slopes103C3102774102wzp1ma60719751:15840
Charlton-Hollis-Rock outcrop complex, 3 to 8 percent slopes103B22027740999npma60719751:15840
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopes102E2019030652w69hma60719751:15840
Hollis - Chatfield complex, 25 to 45 percent slopes114E19190306621w97ma60719751:15840
Chatfield - Hollis - association, 8 to 15 percent slopes, extremely stony903C8190308221w9rma60719751:15840
Charlton-Chatfield-Hollis association, 25 to 35 percent slopes, very rocky925E6190308521w9vma60719751:15840
Hollis-Chatfield association, 15 to 45 percent slopes, very rocky912E268882776642wzp2ma60819891:25000
Chatfield-Hollis-Association, rolling, extremely stony903C852227765899xqma60819891:25000
Charlton-Rock outcrop-Hollis complex, steep711E886427771899znma60919801:15840
Charlton-Rock outcrop-Hollis complex, sloping711C279827771799zmma60919801:15840
Charlton-Hollis-Rock outcrop complex, 8 to 15 percent slopes103C19112777152wzp1ma60919801:15840
Charlton-Hollis- Rock outcrop complex, 15 to 25 percent slopes103D39927771699zlma60919801:15840
Chatfield-Hollis association, 8 to 15 percent slopes903C121190384921x3hma60919801:15840
Hollis-Chatfield association, 15 to 45 percent slopes, very rocky912E1019038732wzp2ma60919801:15840
Charlton-Hollis-Rock outcrop complex, steep103E11528789735vhsbma61019851:25000
Charlton-Hollis-Rock outcrop complex, 8 to 15 percent slopes103C43157897262wzp1ma61019851:25000
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopes102C238618073882w69gma61319821:20000
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopes102D102878074092w69hma61319821:20000
Charlton-Chatfield-Hollis association, 15 to 45 percent slopes, very rocky925E113622787169c0vma61419931:25000
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopes102C332772779872w69gma61519921:25000
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopes102E112772779882w69hma61519921:25000
Hollis-Rock outcrop-Charlton complex, 0 to 15 percent slopes104C133357917222w69pma61619851:25000
Charlton-Hollis-Rock outcrop complex, 8 to 15 percent slopes103C101607916922wzp1ma61619851:25000
Charlton-Hollis-Rock outcrop complex, 3 to 8 percent slopes103B6470791690vktdma61619851:25000
Hollis-Rock outcrop-Charlton complex, 15 to 35 percent slopes104D5325791724vkvhma61619851:25000
Charlton-Hollis-Urban land complex, 3 to 15 percent slopes630C4751791697vktmma61619851:25000
Rock outcrop-Hollis complex, 3 to 25 percent slopes105D3755791794vkxrma61619851:25000
Charlton-Hollis-Rock outcrop complex, 15 to 25 percent slopes103D2600791695vktkma61619851:25000
Chatfield-Hollis-Canton complex, 8 to 15 percent slopes, rocky140C700702792952w82snh01519861:24000
Chatfield-Hollis-Canton complex, 0 to 8 percent slopes, rocky140B315062792942w82mnh01519861:24000
Chatfield-Hollis-Canton complex, 15 to 35 percent slopes, rocky140D227862792962w82pnh01519861:24000
Hollis-Rock outcrop-Chatfield complex, 15 to 60 percent slopes141E32682792979cmlnh01519861:24000
Hollis-Charlton very rocky fine sandy loams, 8 to 15 percent slopesHdC109212798889d7nnh01719681:20000
Hollis-Gloucester extremely rocky fine sandy loams, 8 to 25 percent slopesHlD68102798979d7ynh01719681:20000
Hollis-Charlton very rocky fine sandy loams, 3 to 8 percent slopesHdB51872798879d7mnh01719681:20000
Hollis-Gloucester extremely rocky fine sandy loams, 25 to 60 percent slopesHlE47262798989d7znh01719681:20000
Hollis-Charlton extremely rocky fine sandy loams, 8 to 25 percent slopesHeD47102798909d7qnh01719681:20000
Hollis-Charlton fine sandy loams, 3 to 8 percent slopesHcB42742798849d7jnh01719681:20000
Hollis-Gloucester very rocky fine sandy loams, 8 to 15 percent slopesHgC40972798959d7wnh01719681:20000
Hollis-Charlton fine sandy loams, 8 to 15 percent slopesHcC19982798859d7knh01719681:20000
Hollis-Charlton very rocky fine sandy loams, 15 to 25 percent slopesHdD19842798899d7pnh01719681:20000
Hollis-Gloucester very rocky fine sandy loams, 15 to 25 percent slopesHgD15882798969d7xnh01719681:20000
Hollis-Gloucester very rocky fine sandy loams, 3 to 8 percent slopesHgB15132798949d7vnh01719681:20000
Hollis-Charlton extremely rocky fine sandy loams, 25 to 60 percent slopesHeE11532798919d7rnh01719681:20000
Hollis-Gloucester fine sandy loams, 8 to 15 percent slopesHfC4752798939d7tnh01719681:20000
Hollis-Gloucester fine sandy loams, 3 to 8 percent slopesHfB4542798929d7snh01719681:20000
Hollis-Charlton fine sandy loams, 15 to 25 percent slopesHcD2462798869d7lnh01719681:20000
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopesCtD111412809662w69hnh60119801:20000
Chatfield-Hollis complex, 8 to 15 percent slopes, rockyCsC100372809652w69lnh60119801:20000
Chatfield-Hollis-Canton complex, 8 to 15 percent slopesCpC84262809622w82rnh60119801:20000
Chatfield-Hollis-Canton complex, 3 to 8 percent slopesCpB22682809612w82qnh60119801:20000
Chatfield-Hollis-Canton complex, 15 to 25 percent slopes, very rockyCpD21752809632w82nnh60119801:20000
Chatfield-Hollis complex, 3 to 8 percent slopesCsB8942809649fccnh60119801:20000
Chatfield-Montauk-Hollis complex, 8 to 15 percent slopes, very rocky250C232662801632w69vnh60920071:24000
Chatfield-Montauk-Hollis complex, 15 to 35 percent slopes, very rocky250D141062801642xfdwnh60920071:24000
Chatfield-Montauk-Hollis complex, 0 to 8 percent slopes, very rocky250B77142801622xfdxnh60920071:24000
Chatfield-Montauk-Hollis complex, 35 to 60 percent slopes, very rocky250E24382801652xfdvnh60920071:24000
Windsor-Hollis complex, 8 to 15 percent slopes, very rocky180C18572801472w2x5nh60920071:24000
Windsor-Hollis complex, 0 to 8 percent slopes, very rocky180B7022801462w2wxnh60920071:24000
Windsor-Hollis complex, 15 to 35 percent slopes, very rocky180D5962801482w2x4nh60920071:24000
Hollis-Rock outcrop-Chatfield complex, 35 to 60 percent slopes141E5052801249dh8nh60920071:24000
Hollis-Rock outcrop-Chatfield complex, 8 to 15 percent slopes141C492822833wm70nh60920071:24000
Hollis-Rock outcrop-Chatfield complex, 15 to 35 percent slopes, very stony141D3932801232xff0nh60920071:24000
Hollis-Rock outcrop-Chatfield complex, 3 to 8 percent slopes141B2422801229dh6nh60920071:24000
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopesChkC73103320513p46nj02719741:24000
Hollis-Rock outcrop-Chatfield complex, New Jersey Highlands, 15 to 35 percent slopesHncD4814690392w69snj02719741:24000
Chatfield-Hollis-Rock outcrop complex, New Jersey Highlands, 35 to 60 percent slopesChkE4114690372w69tnj02719741:24000
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopesChkC23314690161l9mmnj03119721:24000
Hollis-Rock outcrop-Chatfield complex, New Jersey Highlands, 15 to 35 percent slopesHncD3114690182w69snj03119721:24000
Chatfield-Hollis-Rock outcrop complex, New Jersey Highlands, 35 to 60 percent slopesChkE614690172w69tnj03119721:24000
Hollis-Rock outcrop-Chatfield complex, New Jersey Highlands, 15 to 35 percent slopesHncD164246248122w69snj03720021:24000
Chatfield-Hollis-Rock outcrop complex, New Jersey Highlands, 35 to 60 percent slopesChkE139486230782w69tnj03720021:24000
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopesChkC9342623075nxc6nj03720021:24000
Chatfield-Hollis-Rock outcrop complex, New Jersey Highlands, 35 to 60 percent slopesChkE466811474732w69tnj04120071:12000
Hollis-Rock outcrop-Chatfield complex, New Jersey Highlands, 15 to 35 percent slopesHncD344211474892w69snj04120071:12000
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopesChkC635114747217j17nj04120071:12000
Chatfield-Hollis-Greenbelt complex, 0 to 15 percent slopes, rockyCHGC48124824932pb7fny00520141:12000
Charlton-Chatfield-Hollis complex, 0 to 15 percent slopes, very rockyCCHC30824215802m8vhny00520141:12000
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopesCHRD18124870842ph0jny00520141:12000
Chatfield-Charlton-Hollis-Rock outcrop complex, 0 to 15 percent slopesCCHRC11624870812ph0fny00520141:12000
Chatfield-Greenbelt-Hollis-Rock outcrop complex, 0 to 15 percent slopesCGHRC9024824952pb7hny00520141:12000
Chatfield-Hollis-Rock outcrop complex, 35 to 60 percent slopesCHRE7024870852ph0kny00520141:12000
Chatfield-Greenbelt-Hollis-Rock outcrop complex, 15 to 35 percent slopesCGHRD1025891532qf9xny00520141:12000
Hollis-Chatfield-Rock outcrop complex, very steepHoF164682906719rghny02719921:24000
Hollis-Chatfield-Rock outcrop complex, hillyHoD105622906699rgfny02719921:24000
Hollis-Chatfield-Rock outcrop complex, steepHoE87222906709rggny02719921:24000
Chatfield-Hollis complex, rolling, very rockyCtC84292906329rf7ny02719921:24000
Chatfield-Hollis complex, 15 to 35 percent slopes, very rockyCtD82252906332w69wny02719921:24000
Hollis-Chatfield-Rock outcrop complex, rollingHoC37672906689rgdny02719921:24000
Chatfield-Hollis complex, undulating, very rockyCtB8882906319rf6ny02719921:24000
Chatfield-Hollis complex, 15 to 35 percent slopes, very rockyCoD36893164512w69wny03120071:24000
Hollis-Rock outcrop complex, 35 to 60 percent slopes, very stonyHsF245910299202xfdzny03120071:24000
Chatfield-Hollis complex, 8 to 15 percent slopes, very rocky, very stonyCoC2238316452bm94ny03120071:24000
Chatfield-Hollis complex, 35 to 60 percent slopes, very rocky, very stonyCoF8251020318137qhny03120071:24000
Hollis-Rock outcrop complex, 15 to 35 percent slopes, very stonyHsD6993192352xfdyny03120071:24000
Chatfield-Hollis complex, 3 to 8 percent slopes, very rocky, very stonyCoB368316453bm95ny03120071:24000
Hollis-Rock outcrop complex, 3 to 25 percent slopes17D168813818301hcx5ny03520071:24000
Chatfield-Hollis complex, 15 to 35 percent slopes, very rocky18D2067672862w69wny03520071:24000
Chatfield-Hollis complex, 8 to 15 percent slopes, very rocky18C103635432pb6tny03520071:24000
Hollis-Rock outcrop complex, 0 to 8 percent slopesHrB67112918469spdny04519811:15840
Hollis-Galoo, acid, complex, rocky, 0 to 8 percent slopesHpB11622918459spcny04519811:15840
Hollis fine sandy loam, 5 to 25 percent slopes, very stonyGnD9852677688bmkkny04920181:24000
Hollis-Rock outcrop association, slopingHGC5442928199tpsny05719731:24000
Rock outcrop-Hollis-Chatfield complex, 60 to 80 percent slopesRHCF17325188532m8vdny06120141:12000
Chatfield-Hollis-Rock outcrop complex, 35 to 60 percent slopesCHRE16825187912ph0kny06120141:12000
Chatfield-Greenbelt-Hollis-Rock outcrop complex, 15 to 35 percent slopesCGHRD16225188892qf9xny06120141:12000
Chatfield-Hollis-Greenbelt complex, 0 to 15 percent slopes, rockyCHGC12325187892pb7fny06120141:12000
Charlton-Chatfield-Hollis complex, 0 to 15 percent slopes, very rockyCCHC6625187862m8vhny06120141:12000
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopesCHRD5925187902ph0jny06120141:12000
Chatfield-Greenbelt-Hollis-Rock outcrop complex, 0 to 15 percent slopesCGHRC3825187882pb7hny06120141:12000
Chatfield-Charlton-Hollis-Rock outcrop complex, 0 to 15 percent slopesCCHRC525187872ph0fny06120141:12000
Rock outcrop-Hollis complex, 15 to 35 percent slopesROD265282939672w69nny07119761:15840
Rock outcrop-Hollis complex, slopingROC208172939669vwsny07119761:15840
Hollis soils, slopingHLC106812939269vvhny07119761:15840
Rock outcrop-Hollis complex, very steepROF88812939689vwvny07119761:15840
Hollis soils, moderately steepHLD47132939279vvjny07119761:15840
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopesCuD138422930722w69hny07919871:12000
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopesCtC102422930712w69gny07919871:12000
Hollis-Rock outcrop complex, 35 to 60 percent slopesHrF90252930782w69qny07919871:12000
Hollis-Rock outcrop complex, 35 to 60 percent slopesHlF36592932492w69qny08719861:24000
Chatfield-Hollis complex, 8 to 15 percent slopes, rockyCeC63072943622w69lny09119931:24000
Chatfield-Hollis complex, 15 to 35 percent slopes, very rockyCfD16202943632w69wny09119931:24000
Chatfield-Hollis complex, undulating, rockyCeB10972943619w9jny09119931:24000
Hollis-Charlton association, moderately steep and steepHLE594672959649xz7ny11519721:20000
Hollis-Rock outcrop association, gently sloping and slopingHNC128802959659xz8ny11519721:20000
Rock outcrop-Hollis association, moderately steep through very steepROF81732960039y0hny11519721:20000
Chatfield-Hollis-Rock outcrop complex, 15 to 35 percent slopesCuD109013097062w69hny11919871:12000
Chatfield-Hollis-Rock outcrop complex, 0 to 15 percent slopesCtC91863097052w69gny11919871:12000
Hollis-Rock outcrop complex, 35 to 60 percent slopesHrF61603097122w69qny11919871:12000

Map of Series Extent

Approximate geographic distribution of the HOLLIS 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 .