Official Series Description


Lab Data Summary

Aggregate lab data for the COLONEL soil series. This aggregation is based on all pedons with a current taxon name of COLONEL, 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 COLONEL 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
1432013NH6050012013NH605001Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0403242,-71.7923676
1432013NH6050162013NH605016Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0672618,-71.8358139
1432013NH6050372013NH605037Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0875361,-71.7883722
1432013NH6050412013NH605041Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0795417,-71.7864972
1432013NH6050422013NH605042Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0809889,-71.7854278
1432013NH6050452013NH605045Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1359944,-71.8228667
1432013NH6050592013NH605059Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0549389,-71.8488611
1432013NH6050622013NH605062Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0572278,-71.8412167
1432013NH6050692013NH605069Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0895806,-71.7709417
1432013NH6050712013NH605071Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0926694,-71.7731222
1432013NH6050752013NH605075Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0546528,-71.7774639
1432013NH6050762013NH605076Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0984639,-71.78365
1432013NH6050822013NH605082Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0673472,-71.8202639
14309N0154S08ME021002.ColonelCOLONEL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4093819,-69.1407318
14309N0163S08ME021011.ColonelCOLONEL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9188614,-69.1592789
14310N0330S09ME021014.ColonelColonel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4241111,-69.0587778
14340A4198S1977ME021003Colonel7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1066132,-69.2032547
14300P1237S2000VT003001Colonel7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.089118,-73.019329
14300P1236S2000VT007001Colonel7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5352783,-72.8354721
144B2013NH6050332013NH605033Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0711417,-71.8406722
144B2013NH6050542013NH605054Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0695222,-71.8174944
144B2013NH6050552013NH605055Colonel1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0722194,-71.8220667
144B87P059387ME001001Colonel7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2708321,-70.2402802
144B93P0832S1993VT005002Colonel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2572212,-72.2744446
144B93P0833S1993VT005003Colonel7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2858315,-72.2944412
n/a91P004890ME019002Colonel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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Soil series sharing subgroup-level classification with COLONEL, 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-2010-09-03-01 | Franklin County Area and Part of Somerset County - 2003

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

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

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

  3. ME-2012-02-03-07 | Oxford County Area - March 1995

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

  4. ME-2012-02-03-09 | Oxford County Area - March 1995

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

  5. ME-2012-02-03-11 | Oxford County Area - March 1995

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

Map Units

Map units containing COLONEL 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
Skerry-Colonel association, 0 to 15 percent slopes, very stonySTC135813158242x9p8me00519691:24000
Colonel-Brayton assocation, 0 to 8 percent slopes, very stonyCFB9685315664blgqme00519691:24000
Colonel fine sandy loam, 0 to 8 percent slopes, very stonyCdB50343000982ty6qme00519691:24000
Colonel fine sandy loam, 3 to 8 percent slopesCcB24043001052ty6nme00519691:24000
Colonel fine sandy loam, 8 to 15 percent slopes, very stonyCdC5873001062ty6rme00519691:24000
Skerry-Colonel association, 3 to 15 percent slopesSSC3343158232x9p6me00519691:24000
Skerry-Colonel association, 15 to 35 percent slopes, very stonySTD3033158252x9p9me00519691:24000
Peru-Colonel association, 3 to 15 percent slopes, very stonyDUC1563157822w9nvme00519691:24000
Colonel fine sandy loam, 8 to 15 percent slopesCcC953000912ty6pme00519691:24000
Colonel-Peru association, 3 to 15 percent slopes, very stonyCPC1261582849792ty7tme61019921:20000
Brayton-Colonel association, 0 to 8 percent slopes, very stonyBSB364032849652ty7sme61019921:20000
Colonel fine sandy loam, 3 to 8 percent slopesCnB17862849882ty6nme61019921:20000
Colonel fine sandy loam, 0 to 8 percent slopes, very stonyCoB16312849902ty6qme61019921:20000
Colonel fine sandy loam, 8 to 15 percent slopes, very stonyCoC4192849912ty6rme61019921:20000
Colonel fine sandy loam, 8 to 15 percent slopesCnC3782849892ty6pme61019921:20000
Peru-Colonel association, 15 to 35 percent slopes, very stonyDUD163198182w9nxme61019921:20000
Peru-Colonel association, 3 to 15 percent slopesDTC33000542w9nwme61019921:20000
Brayton-Colonel association, 0 to 8 percent slopes, very stonyBSB340932850772ty7rme61119881:20000
Peru-Colonel complex, 3 to 8 percent slopes, very stonyDtB220092850962trs2me61119881:20000
Peru-Colonel complex, 3 to 8 percent slopesDsB82892850952xk0sme61119881:20000
Peru-Colonel-Tunbridge complex, 3 to 8 percent slopes, very stonyDWB79322850912tsw1me61119881:20000
Brayton-Colonel association, gently sloping, rubblyBTB58542850789kn2me61119881:20000
Peru-Colonel-Tunbridge association, 3 to 15 percent slopes, very stonyPCC28572744557szrzme61220161:24000
Brayton-Colonel complex, 0 to 8 percent slopes, very stonyBRB21956746267t1k4me61220161:24000
Colonel-Peru-Brayton complex, 0 to 8 percent slopes, very stonyCDB19535744551szrsme61220161:24000
Scantic-Lamoine-Colonel association, 0 to 8 percent slopes, very stonySLB15936742170sx8zme61220161:24000
Brayton-Colonel-Lyman complex, 0 to 8 percent slopes, rockyBYB8357744552szrtme61220161:24000
Colonel-Peru complex, 3 to 8 percent slopes, very stonyCpB292314829791ls51me61220161:24000
Skerry-Becket-Colonel complex, 0 to 8 percent slopes, very boulderySKB168526436372rk0hme61220161:24000
Brayton-Colonel complex, 0 to 8 percent slopes, very stonyBcB157224819842p9q0me61220161:24000
Colonel gravelly fine sandy loam, 3 to 8 percent slopesCoB1177741212sw92me61220161:24000
Skerry-Colonel association, 0 to 15 percent slopes, very stonySTC1076572858282x9p8me61319871:20000
Skerry-Colonel association, 15 to 35 percent slopes, very stonySTD251092858292x9p9me61319871:20000
Colonel fine sandy loam, 0 to 8 percent slopes, very stonyCfB164212857502ty6qme61319871:20000
Peru-Colonel association, 3 to 15 percent slopes, very stonyDUC120982857602w9nvme61319871:20000
Peru-Colonel association, 15 to 35 percent slopes, very stonyDUD61412857612w9nxme61319871:20000
Skerry-Colonel association, 3 to 15 percent slopesSSC52402858272x9p6me61319871:20000
Colonel fine sandy loam, 3 to 8 percent slopesCeB31272857482ty6nme61319871:20000
Colonel fine sandy loam, 8 to 15 percent slopes, very stonyCfC15522857512ty6rme61319871:20000
Peru-Colonel association, 3 to 15 percent slopesDTC7432857592w9nwme61319871:20000
Colonel fine sandy loam, 8 to 15 percent slopesCeC4752857492ty6pme61319871:20000
Colonel-Brayton-Peru association, 0 to 8 percent slopes, very stonyCPB650892853112ty7qme61519941:24000
Peru-Colonel-Lyman association, 3 to 15 percent slopes, very stonyDYC287292853232w9p0me61519941:24000
Peru-Colonel association, 3 to 15 percent slopes, very stonyDXC209672853222w9nvme61519941:24000
Colonel-Brayton-Lyman complex, undulating, very stonyCQB87712853129kwmme61519941:24000
Colonel-Hermon association, 0 to 15 percent slopes, extremely boulderyCRC38992853132x9qbme61519941:24000
Colonel fine sandy loam, 3 to 8 percent slopesCoB2232853162ty6nme61519941:24000
Brayton-Colonel association, 0 to 8 percent slopes, very stonyBRB503672855322ty7rme61720041:24000
Peru-Colonel complex, 0 to 8 percent slopes, very stonyDHB343122855592trrwme61720041:24000
Peru-Tunbridge-Colonel complex, 3 to 15 percent slopes, very stonyDWC260572855622w9ndme61720041:24000
Lamoine-Scantic-Colonel complex, 0 to 8 percent slopes, very stonyLSB240162855852x1brme61720041:24000
Skerry-Colonel association, 0 to 8 percent slopes, very stonySOB172342856182x9p7me61720041:24000
Skerry-Colonel-Tunbridge complex, 0 to 15 percent slopes, very stonySTC166292856192xk0dme61720041:24000
Brayton-Colonel association, 0 to 8 percent slopes, extremely stonyBTB64642855339l3rme61720041:24000
Skerry-Colonel-Rawsonville complex, 0 to 15 percent slopes, very stonySRC476714012891j14wme61720041:24000
Peru-Colonel complex, 3 to 8 percent slopesDgB35502855652xk0sme61720041:24000
Peru-Colonel complex, 3 to 8 percent slopes, very stonyDkB28162855662trs2me61720041:24000
Peru-Rawsonville-Colonel complex, 3 to 15 percent slopes, very stonyDUC77814012641j142me61720041:24000
Colonel-Peru-Pillsbury association, 3 to 15 percent slopes, very stonyCNC910762856802trrgme61920051:24000
Colonel-Pillsbury-Peru association, 0 to 8 percent slopes, very stonyCPB844392856792trrjme61920051:24000
Peru-Colonel-Rawsonville association, 3 to 15 percent slopesDTC818342856749l89me61920051:24000
Peru-Colonel-Marlow association, 3 to 15 percent slopes, very stonyDMC494542856772trrhme61920051:24000
Colonel-Skerry-Pillsbury association, 0 to 15 percent slopes, very stonyCSC251792856662x9qfme61920051:24000
Colonel-Pillsbury-Skerry association, 0 to 8 percent slopes, very stonyCRB228752856652x9qcme61920051:24000
Mahoosuc-Colonel-Pillsbury association, 1 to 16 percent slopesMCC8672857209l9sme61920051:24000
Brayton-Colonel-Peru association, 0 to 8 percent slopes, extremely stonyBCB4440325499142trrlme62020111:24000
Peru-Colonel-Rawsonville association, 3 to 15 percent slopes, very stonyDOC3277425499102qtlzme62020111:24000
Colonel-Peru-Brayton association, 3 to 15 percent slopes, very boulderyCDB2971325499152trrrme62020111:24000
Peru-Colonel-Marlow association, 3 to 15 percent slopes, very boulderyDCC2550825499122trs1me62020111:24000
Brayton-Colonel-Skerry association, 0 to 8 percent slopes, extremely boulderyBSB1587925499002x9q9me62020111:24000
Brayton-Colonel-Ragmuff association, 0 to 8 percent slopes, extremely stonyBRB1152825499092qtlyme62020111:24000
Skerry-Colonel association, 0 to 15 percent slopes, extremely boulderySCC881725499012x9pbme62020111:24000
Peru-Colonel-Rawsonville association, 3 to 15 percent slopes, very stonyDOC2182325498542qtk7me62120111:24000
Colonel-Peru-Brayton association, 3 to 15 percent slopes, very boulderyCDB1132625498562trrrme62120111:24000
Brayton-Colonel-Peru association, 0 to 8 percent slopes, extremely stonyBCB958425498552trrlme62120111:24000
Peru-Colonel-Marlow association, 3 to 15 percent slopes, very boulderyDCC123025498522trs1me62120111:24000
Colonel-Brayton-Peru association, 0 to 8 percent slopes, very stonyCLB8978819092882ty7qme62220071:24000
Peru-Tunbridge-Colonel complex, 3 to 15 percent slopes, very stonyDXC6384719092782w9ndme62220071:24000
Colonel-Peru-Brayton association, 0 to 15 percent slopes, very stonyCNC5449519092892trrkme62220071:24000
Peru-Colonel-Marlow association, 3 to 15 percent slopes, very stonyDOC3876719092862trrhme62220071:24000
Colonel-Skerry-Brayton association, 0 to 15 percent slopes, very stonyCOC2901619091792x9qdme62220071:24000
Brayton-Colonel association, 0 to 8 percent slopes, very stonyBLB1265019090922ty7rme62220071:24000
Brayton-Colonel association, 0 to 8 percent slopes, extremely stonyBNB63781909093222knme62220071:24000
Brayton-Colonel association, 0 to 8 percent slopes, rubblyBOB45861909275222rjme62220071:24000
Peru-Colonel complex, 0 to 8 percent slopes, very stonyDNB441819090902trrwme62220071:24000
Lamoine-Scantic-Colonel complex, 0 to 8 percent slopes, very stonyLLB194419090832x1brme62220071:24000
Skerry-Colonel association, 0 to 8 percent slopes, very stonySRB89919090892x9p7me62220071:24000
Peru-Colonel-Tunbridge complex, 3 to 8 percent slopes, very stonyDTB8021909274222rhme62220071:24000
Skerry-Colonel association, 0 to 8 percent slopes, very stony759B1482807432x9p7nh60720001:24000
Skerry-Colonel association, 15 to 35 percent slopes, very stony759D272807392x9p9nh60720001:24000
Colonel-Cabot complex, 3 to 15 percent slopes, extremely bouldery87C80422829962w9nrvt00520061:20000
Colonel-Cabot complex, 8 to 15 percent slopes, very stony73C35412829732w9nnvt00520061:20000
Colonel-Cabot complex, 3 to 8 percent slopes, very stony73B14202829722w9nlvt00520061:20000
Colonel-Cabot complex, 3 to 8 percent slopes72B4082829692w9nkvt00520061:20000
Colonel-Cabot complex, 8 to 15 percent slopes72C2512829702w9nmvt00520061:20000
Colonel-Cabot complex, 15 to 35 percent slopes, very stony73D2132829742w9nqvt00520061:20000
Colonel-Cabot complex, 15 to 25 percent slopes72D82829712w9npvt00520061:20000
Cabot-Colonel complex, 8 to 15 percent slopes, very stonySIE127277424099642w9nfvt00920121:
Peru-Colonel complex, 15 to 35 percent slopes, very stonySIE334216924099692trrpvt00920121:
Tunbridge-Peru-Colonel complex, 15 to 35 percent slopes, very stonySIE434192224099772trrqvt00920121:
Tunbridge-Colonel-Cabot complex, 8 to 15 percent slopes, very stonySIE423751024099762w9ntvt00920121:
Wilmington-Colonel complex, 0 to 8 percent slopes, very stonySIE212023024099662xk1fvt00920121:
Monadnock-Sunapee-Colonel complex, 8 to 15 percent slopes, very stonySIE621062125038932q31hvt00920121:
Cabot-Colonel complex, 8 to 15 percent slopesSIE12N103525050022w9njvt00920121:
Colonel-Peru complex, 8 to 15 percent slopes, very stonySIE3297424204152m7mxvt00920121:
Wilmington-Colonel complex, 3 to 8 percent slopesSIE21N51925050032q47lvt00920121:
Tunbridge-Colonel-Cabot complex, 8 to 15 percent slopes, rockySIE42N49925050072w9nsvt00920121:
Monadnock-Sunapee-Colonel complex, 8 to 15 percent slopesSIE62N12625050112q47vvt00920121:
Peru-Colonel complex, 15 to 25 percent slopesSIE33N7925050052xk0rvt00920121:
Tunbridge-Peru-Colonel complex, 15 to 25 percent slopes, rockySIE43N5925050082q47rvt00920121:
Colonel-Peru complex, 8 to 15 percent slopesSIE32N825050042q47mvt00920121:
Colonel-Cabot complex, 8 to 15 percent slopes, very stony259C128052834352w9nnvt01920051:20000
Colonel-Cabot complex, 3 to 8 percent slopes, very stony259B64682834342w9nlvt01920051:20000
Colonel-Cabot complex, 3 to 8 percent slopes247B44572834302w9nkvt01920051:20000
Colonel-Cabot complex, 8 to 15 percent slopes247C18652834312w9nmvt01920051:20000
Colonel-Cabot complex, 15 to 35 percent slopes, very stony259D12092834362w9nqvt01920051:20000
Colonel-Cabot complex, 15 to 25 percent slopes247D522834322w9npvt01920051:20000
Colonel fine sandy loam, 8 to 15 percent slopes, very stony19C123382825782ty6rvt02319961:20000
Colonel fine sandy loam, 8 to 15 percent slopes14C72432825432ty6pvt02319961:20000
Colonel fine sandy loam, 3 to 15 percent slopes, extremely bouldery99C40662828022trr9vt02319961:20000
Colonel fine sandy loam, 15 to 35 percent slopes, very stony19D33302825792trr8vt02319961:20000
Colonel fine sandy loam, 0 to 8 percent slopes, very stony19B30882825772ty6qvt02319961:20000
Colonel fine sandy loam, 3 to 8 percent slopes14B28432825422ty6nvt02319961:20000
Colonel fine sandy loam, 15 to 35 percent slopes, extremely bouldery99D10422828032trrbvt02319961:20000
Colonel fine sandy loam, 15 to 25 percent slopes14D7472825442trr7vt02319961:20000
Peru, Skerry, and Colonel soils, 8 to 15 percent slopes, very stony18C213172831412w9r1vt02720001:20000
Peru, Skerry, and Colonel soils, 8 to 15 percent slopes17C69692831382w9qyvt02720001:20000
Peru-Colonel-Marlow association, 3 to 35 percent slopes, very stony203D68132833389htyvt02720001:20000
Peru, Skerry, and Colonel soils, 15 to 25 percent slopes17D25082831392w9qzvt02720001:20000
Peru, Skerry, and Colonel soils, 3 to 8 percent slopes17B24892831372w9qxvt02720001:20000
Peru, Skerry, and Colonel soils, 0 to 8 percent slopes, very stony18B22682831402w9r0vt02720001:20000

Map of Series Extent

Approximate geographic distribution of the COLONEL 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 .