Official Series Description


Lab Data Summary

Aggregate lab data for the VILAS soil series. This aggregation is based on all pedons with a current taxon name of VILAS, 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 VILAS 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
90A18N0925S2016WI037004Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.737255,-88.283042
90A18N0919S2016WI085003Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.691467,-89.928025
90A18N0929S2016WI113002Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.097475,-91.413882
90A18N0932S2016WI129001Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.011282,-91.55342
90B40A1564S1957WI073002Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8452797,-89.7133331
9389P04501989WI037001Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7777786,-88.3244476
9385P091085WI003012Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9761124,-90.809166
9385P092185WI007001Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1811104,-91.0975037
9385P092085WI007005Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1822205,-91.0358353
94A40A203049WI007001Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6688881,-91.2177811
94A79P0388S1979WI085004Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.771946,-89.8072205
94A84P0798S1982WI069004VILASn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.518055,-89.5711136
94A83P0052S1982WI125009Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0094452,-89.2747192
94B18N0923S2016WI037002Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.79342,-88.3119
94B18N0928S2016WI075001Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.66287,-87.93416
94D18N0927S2016WI051002Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.093796,-89.93277
94D18N0920S2016WI085004Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.804877,-89.38599
94D18N0921S2016WI085005Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8861,-89.31456
94D18N0922S2016WI085006Vilasn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8616,-89.54611

Water Balance

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

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

Soil series sharing subgroup-level classification with VILAS, 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. MI-2012-02-06-27 | Iron County - October 1997

    Typical pattern of soils and parent material in the Karlin-Sarona-Vilas association (Soil Survey of Iron County, Michigan; October 1997).

  2. WI-2010-11-08-04 | Forest County -

    Typical pattern of soils and underlying parent material in the Pence-Vilas-Lupton association (Soil Survey of Forest County, Wisconsin).

  3. WI-2012-03-22-01 | Bayfield County - April 1961

    General soil areas: (1) Red clays and pink sands (Ontonagon, Superior, Orienta, Bibon); (2) Rolling and hilly pink stony sandy loams (Gogebic, Cloquet); (3) Rolling and hilly pink sands (Vilas, Omega, Hiawatha); (4) Nearly level pink sands (Omega, Vilas); (5) Undulating and rolling pink stony silt loams, loams, and sandy loams (Freeon, Gogebic, Cloquet); (6) Undulating pink fine sandy loams (Pence); and (7) Wet soils (Peat) (Soil Survey of Bayfield County, WI; 1961).

Map Units

Map units containing VILAS 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
Vilas-Rubicon complex , 1 to 6 percent slopes8121B136724419162mz0hmi01319841:20000
Vilas loamy sand, 6 to 15 percent slopes8119C68024419092xtn2mi01319841:20000
Vilas-Rubicon complex, 6 to 18 percent slopes8121C46524419172mz0jmi01319841:20000
Vilas loamy sand, 0 to 6 percent slopes8119B22724419082xtn1mi01319841:20000
Vilas, very deep water table-Croswell complex, 1 to 6 percent slopes8113B14124419072mz06mi01319841:20000
Vilas loamy sand, 15 to 30 percent slopes8119D9224419102xtn3mi01319841:20000
Vilas-Karlin complex, 1 to 6 percent slopes8112B9224419052mz04mi01319841:20000
Vilas, very deep water table-Croswell-Pence, very deep water table, complex, 1 to 6 percent slopes8058B6624751392p2l6mi01319841:20000
Vilas-Karlin complex, 6 to 18 percent slopes8112C2024419062mz05mi01319841:20000
Vilas-Rubicon complex, pitted, 01 to 18 percent slopes8066C824839972pcsymi01319841:20000
Vilas-Rubicon complex, pitted, 18 to 35 percent slopes8066D224839982pcszmi01319841:20000
Vilas loamy sand, 0 to 6 percent slopes57B49434152282xtn1mi04319851:20000
Vilas loamy sand, 6 to 15 percent slopes57D15874152292xtn2mi04319851:20000
Vilas loamy sand, 15 to 30 percent slopes57F11124152302xtn3mi04319851:20000
Pence-Vilas complex, 1 to 6 percent slopes52B605714562291kwb4mi05320071:24000
Vilas, very deep water table-Croswell-Pence, very deep water table, complex, 1 to 6 percent slopes58B137614562391kwbgmi05320071:24000
Pence-Vilas complex, 6 to 18 percent slopes52C90114562301kwb5mi05320071:24000
Vilas loamy sand, 0 to 6 percent slopes8119B1111124839522xtn1mi06119891:20000
Vilas-Rubicon complex , 1 to 6 percent slopes8121B516924839552pcrlmi06119891:20000
Vilas-Rubicon complex, pitted, 1 to 18 percent slopes8066C453524839902pcsqmi06119891:20000
Vilas-Rubicon complex, pitted, 18 to 35 percent slopes8066D273024839912pcsrmi06119891:20000
Vilas-Rubicon complex, 6 to 18 percent slopes8121C236824839562pcrmmi06119891:20000
Vilas, very deep water table-Croswell complex, 1 to 6 percent slopes8113B216524839192pcqfmi06119891:20000
Vilas loamy sand, 15 to 30 percent slopes8119D189724839542xtn3mi06119891:20000
Vilas loamy sand, 6 to 15 percent slopes8119C186224839532xtn2mi06119891:20000
Vilas-Karlin complex, 1 to 6 percent slopes8112B157624839162pcqbmi06119891:20000
Kellogg-Vilas-Tawas complex, 0 to 12 percent slopes8210B149524849362pds7mi06119891:20000
Sayner-Vilas complex, dissected, 1 to 18 percent slopes8262C79224856222pfhcmi06119891:20000
Kellogg-Vilas, very deep water table, complex, 0 to 6 percent slopes8206B74424849302pds1mi06119891:20000
Vilas-Rubicon complex, pitted, 35 to 75 percent slopes8066F71224839922pcssmi06119891:20000
Kalkaska-Vilas-Karlin complex, very deep water table, 1 to 6 percent slopes8260B57224856182pfh7mi06119891:20000
Pelissier-Sayner-Vilas complex, 1 to 6 percent slopes8261B37824856192pfh8mi06119891:20000
Vilas, very deep water table-Croswell-Pence, very deep water table, complex, 1 to 6 percent slopes8058B31524860602pfyhmi06119891:20000
Vilas-Karlin complex, 6 to 18 percent slopes8112C26824839172pcqcmi06119891:20000
Pelissier-Sayner-Vilas complex, 6 to 18 percent slopes8261C24024856202pfh9mi06119891:20000
Kellogg-Vilas, very deep water table, complex, 6 to 18 percent slopes8206C21424849292pds0mi06119891:20000
Vilas loamy sand, 35 to 55 percent slopes8267F4724839852pcskmi06119891:20000
Vilas-Karlin complex, 1 to 6 percent slopes78B11177416020fyx0mi07119921:20000
Vilas-Karlin complex, 6 to 18 percent slopes78D10035416021fyx1mi07119921:20000
Vilas loamy sand, 0 to 6 percent slopes77B64184160182xtn1mi07119921:20000
Karlin-Vilas-Rock outcrop complex, 1 to 18 percent slopes, stony71D4357416010fywpmi07119921:20000
Vilas loamy sand, 6 to 15 percent slopes77D25624160192xtn2mi07119921:20000
Vilas-Rubicon complex , 1 to 6 percent slopes8121B246524751432p2lbmi07119921:20000
Vilas-Rubicon complex, 6 to 18 percent slopes8121C177024751442p2lcmi07119921:20000
Vilas, very deep water table-Croswell-Pence, very deep water table, complex, 1 to 6 percent slopes8058B129524751382p2l5mi07119921:20000
Vilas-Karlin complex, 18 to 35 percent slopes78F895416022fyx2mi07119921:20000
Pence-Vilas complex, 1 to 6 percent slopes8052B57224749572p2dbmi07119921:20000
Vilas-Rubicon complex, pitted, 18 to 35 percent slopes8066D36624840012pct2mi07119921:20000
Pence-Vilas complex, 6 to 18 percent slopes8052C4024749582p2dcmi07119921:20000
Vilas loamy sand, 0 to 6 percent slopes198B60526313682xtn1mi09520041:24000
Vilas loamy sand, 6 to 15 percent slopes198D5696313692xtn2mi09520041:24000
Pence-Vilas complex, 1 to 6 percent slopes8052B170516747911t6rjmi13120071:24000
Vilas loamy sand, 0 to 6 percent slopes8119B133116748312xtn1mi13120071:24000
Vilas, very deep water table-Croswell-Pence, very deep water table, complex, 1 to 6 percent slopes8058B75316747951t6rnmi13120071:24000
Vilas-Karlin complex, 1 to 6 percent slopes8112B69516748271t6spmi13120071:24000
Vilas-Rubicon complex, 1 to 6 percent slopes8121B44216748331t6swmi13120071:24000
Vilas, very deep water table-Croswell complex, 1 to 6 percent slopes8113B43016748291t6srmi13120071:24000
Pence-Vilas complex, 6 to 18 percent slopes8052C34616747921t6rkmi13120071:24000
Sayner-Vilas complex, dissected, 1 to 18 percent slopes8262C17616748771t6v9mi13120071:24000
Vilas-Rubicon complex, 6 to 18 percent slopes8121C15916748341t6sxmi13120071:24000
Kellogg-Vilas-Tawas complex, 0 to 12 percent slopes8210B14016748621t6ttmi13120071:24000
Kellogg-Vilas, very deep water table, complex, 0 to 6 percent slopes8206B13016748611t6tsmi13120071:24000
Vilas loamy sand, 15 to 30 percent slopes8267D8616748792xtn3mi13120071:24000
Vilas-Karlin complex, 6 to 18 percent slopes8112C8016748281t6sqmi13120071:24000
Pelissier-Sayner-Vilas complex, 6 to 18 percent slopes8261C5816748761t6v8mi13120071:24000
Vilas loamy sand, 6 to 15 percent slopes8119C5016748322xtn2mi13120071:24000
Vilas-Kalkaska complex, pitted outwash, 1 to 18 percent slopes8066C3716747971t6rqmi13120071:24000
Pelissier-Sayner-Vilas complex, 1 to 6 percent slopes8261B3516748751t6v7mi13120071:24000
Vilas loamy sand, 35 to 55 percent slopes8267F2816748801t6vdmi13120071:24000
Vilas loamy sand, 0 to 6 percent slopes515B147914570122xtn1mi15320071:24000
Sayner-Pence-Vilas complex, 6 to 15 percent slopes3974C285514445181kh4cwi00320061:12000
Keweenaw-Sayner-Vilas complex, 0 to 6 percent slopes, stony3369B27916110772xjsqwi00320061:12000
Vilas-Lindquist complex, 6 to 15 percent slopes3594C26914444551kh2bwi00320061:12000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C26116110782xjsswi00320061:12000
Sayner-Pence-Vilas complex, 15 to 30 percent slopes3974E24014445191kh4dwi00320061:12000
Vilas-Lindquist complex, 0 to 6 percent slopes3594B23914444541kh29wi00320061:12000
Vilas loamy sand, 0 to 6 percent slopes3374B21214443632xtn1wi00320061:12000
Sayner-Pence-Vilas complex, 0 to 6 percent slopes3974B19214445171kh4bwi00320061:12000
Vilas loamy sand, 6 to 15 percent slopes3374C16814443642xtn2wi00320061:12000
Vilas-Lindquist complex, 15 to 30 percent slopes3594E1514444561kh2cwi00320061:12000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E816110792xjstwi00320061:12000
Vilas loamy sand, 6 to 15 percent slopes3374C415724337572xtn2wi00720051:12000
Vilas loamy sand, 0 to 6 percent slopes3374B327454337562xtn1wi00720051:12000
Vilas loamy sand, 15 to 30 percent slopes3374E194754337582xtn3wi00720051:12000
Keweenaw, stony-Vilas-Cathro complex, 0 to 15 percent slopes6884C6543114743617j02wi00720051:12000
Sayner-Pence-Vilas complex, 6 to 15 percent slopes3974C5659782505v883wi00720051:12000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C172811474032xjsswi00720051:12000
Sayner-Pence-Vilas complex, 15 to 30 percent slopes3974E1713782506v884wi00720051:12000
Keweenaw, stony-Vilas-Cathro complex, 0 to 55 percent slopes6884F1558114743717j03wi00720051:12000
Sayner-Pence-Vilas complex, 0 to 6 percent slopes3974B143813801091hb3nwi00720051:12000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E131011474022xjstwi00720051:12000
Vilas loamy sand, 20 to 45 percent slopes3374F104213835391hfp9wi00720051:12000
Vilas-Lindquist complex, 6 to 15 percent slopes3594C872114741217hz9wi00720051:12000
Keweenaw-Sayner-Vilas complex, 0 to 6 percent slopes, stony3369B56411474012xjsqwi00720051:12000
Vilas-Lindquist complex, 15 to 30 percent slopes3594E158114741117hz8wi00720051:12000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E6856560982xjstwi01320041:12000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C5216560972xjsswi01320041:12000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C87027810732xjsswi03120051:12000
Vilas loamy sand, 0 to 6 percent slopes3374B66547810762xtn1wi03120051:12000
Keweenaw, stony-Vilas-Cathro complex, 0 to 15 percent slopes6884C605714051171j54cwi03120051:12000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E28257810742xjstwi03120051:12000
Vilas loamy sand, 6 to 15 percent slopes3374C23007810772xtn2wi03120051:12000
Keweenaw-Sayner-Vilas complex, 0 to 6 percent slopes, stony3369B18847810722xjsqwi03120051:12000
Vilas loamy sand, 15 to 30 percent slopes3374E4317810782xtn3wi03120051:12000
Keweenaw, stony-Vilas-Cathro complex, 0 to 55 percent slopes6884F17714051191j54fwi03120051:12000
Vilas loamy sand, 0 to 6 percent slopes3374B59334300602xtn1wi03719951:12000
Vilas loamy sand, 6 to 15 percent slopes3374C52894300612xtn2wi03719951:12000
Sarona-Vilas complex, 6 to 15 percent slopes, very stony3663C5225430047gfhhwi03719951:12000
Pence-Vilas complex, 6 to 15 percent slopes3219C4628430029gfgxwi03719951:12000
Sarona-Vilas complex, 0 to 6 percent slopes, very stony3663B4488430046gfhgwi03719951:12000
Pence-Vilas complex, 0 to 6 percent slopes3219B3642430028gfgwwi03719951:12000
Pence-Vilas complex, 15 to 35 percent slopes3219E3438430030gfgywi03719951:12000
Vilas loamy sand, 15 to 30 percent slopes3374E32944300622xtn3wi03719951:12000
Ellwood-Iosco-Vilas complex, 0 to 15 percent slopes3685C2865430001gfg0wi03719951:12000
Sarona-Vilas complex, 15 to 30 percent slopes, very stony3663E2204430048gfhjwi03719951:12000
Rock outcrop-Ishpeming-Vilas complex, 1 to 15 percent slopes3925C1545430034gfh2wi03719951:12000
Ellwood-Vilas-Padus complex, 10 to 30 percent slopes3684E1514430002gfg1wi03719951:12000
Rock outcrop-Ishpeming-Vilas complex, 15 to 35 percent slopes3925E469430035gfh3wi03719951:12000
Pence-Vilas complex, 6 to 15 percent slopes3219C9721429864gf9lwi04119951:12000
Pence-Vilas complex, 0 to 6 percent slopes3219B4611429863gf9kwi04119951:12000
Pence-Vilas complex, 15 to 35 percent slopes3219E4495429865gf9mwi04119951:12000
Vilas loamy sand, 6 to 15 percent slopes3374C9444298772xtn2wi04119951:12000
Vilas loamy sand, 0 to 6 percent slopes3374B7344298762xtn1wi04119951:12000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C400116977052xjsswi05120061:12000
Sayner-Pence-Vilas complex, 6 to 15 percent slopes3974C2197782412v853wi05120061:12000
Vilas loamy sand, 0 to 6 percent slopes3374B20657819442xtn1wi05120061:12000
Vilas-Lindquist complex, 0 to 6 percent slopes3594B165217012431v38twi05120061:12000
Sayner-Pence-Vilas complex, 0 to 6 percent slopes3974B83016976991tzlhwi05120061:12000
Vilas loamy sand, 6 to 15 percent slopes3374C8137819452xtn2wi05120061:12000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E75217012472xjstwi05120061:12000
Sayner-Pence-Vilas complex, 15 to 30 percent slopes3974E540782413v854wi05120061:12000
Vilas-Lindquist complex, 6 to 15 percent slopes3594C51717012441v38vwi05120061:12000
Keweenaw, stony-Vilas-Cathro complex, 0 to 15 percent slopes6884C21017012581v399wi05120061:12000
Keweenaw-Sayner-Vilas complex, 0 to 6 percent slopes, stony3369B20716977042xjsqwi05120061:12000
Vilas loamy sand, 15 to 30 percent slopes3374E1727819462xtn3wi05120061:12000
Vilas-Lindquist complex, 15 to 30 percent slopes3594E8317012451v38wwi05120061:12000
Vilas loamy sand, 0 to 6 percent slopes3374B35924210732xtn1wi06719831:20000
Vilas loamy sand, 6 to 15 percent slopes3374C13134210742xtn2wi06719831:20000
Vilas-Sayner loamy sands, 1 to 6 percent slopes3774B13231431652gh58wi06919931:20000
Vilas-Sayner loamy sands, 6 to 15 percent slopes3774C11529431653gh59wi06919931:20000
Vilas-Sayner loamy sands, 15 to 35 percent slopes3774E5695431654gh5bwi06919931:20000
Vilas loamy sand, 0 to 6 percent slopes3374B34393958732xtn1wi07819981:12000
Vilas loamy sand, 6 to 15 percent slopes3374C29943958752xtn2wi07819981:12000
Vilas loamy sand, 15 to 30 percent slopes3374E10813958742xtn3wi07819981:12000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C295674210952xjsswi08519881:20000
Vilas loamy sand, 0 to 6 percent slopes3374B242774211192xtn1wi08519881:20000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E233394210962xjstwi08519881:20000
Vilas loamy sand, 6 to 15 percent slopes3374C172594211202xtn2wi08519881:20000
Siskiwit-Vilas complex, 0 to 6 percent slopes, stony3794B151434210942tp04wi08519881:20000
Vilas loamy sand, 15 to 30 percent slopes3374E118814211212xtn3wi08519881:20000
Sayner-Pence-Vilas complex, 6 to 15 percent slopes3974C601813957291hvcjwi09920061:12000
Vilas-Lindquist complex, 6 to 15 percent slopes3594C377415988101qnpjwi09920061:12000
Sayner-Pence-Vilas complex, 15 to 30 percent slopes3974E297313957281hvchwi09920061:12000
Vilas-Lindquist complex, 0 to 6 percent slopes3594B295512922711dcq5wi09920061:12000
Vilas-Lindquist complex, 15 to 30 percent slopes3594E83815988111qnpkwi09920061:12000
Sayner-Pence-Vilas complex, 0 to 6 percent slopes3974B14313957301hvckwi09920061:12000
Vilas-Lindquist complex, 0 to 6 percent slopes3594B193114515817fmlwi10720061:12000
Vilas-Lindquist complex, 6 to 15 percent slopes3594C88114516017fmnwi10720061:12000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E85556253562xjstwi11320061:12000
Vilas-Lindquist complex, 0 to 6 percent slopes3594B707910178161353swi11320061:12000
Vilas-Lindquist complex, 6 to 15 percent slopes3594C701410178201353xwi11320061:12000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C38226253552xjsswi11320061:12000
Vilas-Lindquist complex, 15 to 30 percent slopes3594E225710178191353wwi11320061:12000
Sayner-Pence-Vilas complex, 6 to 15 percent slopes3974C143613861011hjbywi11320061:12000
Keweenaw-Sayner-Vilas complex, 0 to 6 percent slopes, stony3369B7199914032xjsqwi11320061:12000
Sayner-Pence-Vilas complex, 15 to 30 percent slopes3974E38613861001hjbxwi11320061:12000
Siskiwit-Vilas complex, 0 to 6 percent slopes, stony3794B105954212472tp04wi12519851:20000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C72704212482xjsswi12519851:20000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E49014212492xjstwi12519851:20000
Keweenaw-Sayner-Vilas complex, 5 to 35 percent slopes, stony3369E151624354712xjstwi12920021:12000
Keweenaw-Sayner-Vilas complex, 1 to 15 percent slopes, stony3369C113394354702xjsswi12920021:12000
Keweenaw-Sayner-Vilas complex, 0 to 6 percent slopes, stony3369B16696359892xjsqwi12920021:12000
Vilas loamy sand, 0 to 6 percent slopes3374B4304354722xtn1wi12920021:12000
Vilas loamy sand, 6 to 15 percent slopes3374C2184354732xtn2wi12920021:12000
Vilas loamy sand, 15 to 30 percent slopes3374E74354742xtn3wi12920021:12000

Map of Series Extent

Approximate geographic distribution of the VILAS 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 .