Official Series Description


Lab Data Summary

Aggregate lab data for the EVELETH soil series. This aggregation is based on all pedons with a current taxon name of EVELETH, 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 EVELETH 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
93AUMN4229S1989MN1374229Eveleth3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8687286,-92.0915222

Water Balance

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

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

Competing Series

Soil series competing with EVELETH 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 EVELETH 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 EVELETH series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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

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

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 EVELETH, 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

No block diagrams are available.

Map Units

Map units containing EVELETH 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
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly complex, 0 to 18 percent slopes, very rockyI2b21D17227527745722t20kmn03120131:24000
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly complex, 0 to 30 percent slopes, very rockyI2b21E6918327746662t20lmn03120131:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyI2a31D2498427745792wcmsmn03120131:24000
Eveleth, bouldery-Conic, bouldery-Rock outcrop complex, 18 to 30 percent slopesI2a32E1573127746092t20cmn03120131:24000
Eveleth stony loam, 8 to 18 percent slopes, boulderyI3-32D391327745162t212mn03120131:24000
Conic, bouldery-Rock outcrop-Eveleth, bouldery complex, 2 to 35 percent slopesI2c23E31827747272t20tmn03120131:24000
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly complex, 0 to 18 percent slopes, very rockyI2b21D20717431149272t20kmn07520131:24000
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly complex, 0 to 30 percent slopes, very rockyI2b21E2169631149282t20lmn07520131:24000
Eveleth, bouldery-Conic, bouldery-Rock outcrop complex, 18 to 30 percent slopesI2a32E2136731149242t20cmn07520131:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyI2a31D2067431149232wcmsmn07520131:24000
Conic, bouldery-Rock outcrop-Eveleth, bouldery complex, 2 to 35 percent slopesI2c23E86931149332t20tmn07520131:24000
Eveleth stony loam, 8 to 18 percent slopes, boulderyI3-32D16431149402t212mn07520131:24000
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly, complex, 0 to 18 percent slopesF35D9953924064392ls32mn61320161:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyF3D4626624064372wcmsmn61320161:24000
Eveleth, bouldery-Conic, bouldery-Rock outcrop complex, 18 to 30 percent slopesF4E2329824068912lsknmn61320161:24000
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly, complex, 0 to 30 percent slopesF35E2024324064402ls33mn61320161:24000
Conic, bouldery-Rock outcrop-Eveleth, bouldery, complex, 0 to 35 percent slopesF209E1369425186522qj01mn61320161:24000
Eveleth stony loam, 8 to 18 percent slopes, boulderyF14D1442494004wmf2mn61320161:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyF3D2711818614452wcmsmn61720071:24000
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly, complex, 0 to 18 percent slopesF35D26539186145020gzsmn61720071:24000
Eveleth-Conic, bouldery-Rock outcrop complex, 18 to 30 percent slopesF4E7350186144620gznmn61720071:24000
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly, complex, 0 to 30 percent slopesF35E57871912959226lcmn61720071:24000
Eveleth stony loam, 8 to 18 percent slopes, boulderyF14D4140186146420h07mn61720071:24000
Eveleth-Eaglesnest complex, 2 to 20 percent slopes, very boulderyF177C27051913133226rzmn61720071:24000
Eveleth-Conic complex, 20 to 50 percent slopes, very boulderyF22F2202186143820gzdmn61720071:24000
Soudan-Eveleth complex, 8 to 18 percent slopes, boulderyF44D4401912966226llmn61720071:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyF3D178138229972wcmsmn62120061:24000
Eveleth, bouldery-Conic, bouldery-Aquepts, rubbly, complex, 0 to 18 percent slopesF35D3352823034wmfhmn62120061:24000
Eveleth-Conic, bouldery-Rock outcrop complex, 18 to 30 percent slopesF4E1496822996wmd8mn62120061:24000
Eveleth stony loam, 8 to 18 percent slopes, boulderyF14D1294823021wmf2mn62120061:24000
Eveleth-Conic complex, 20 to 50 percent slopes, very boulderyF22F822823032wmffmn62120061:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyF3D26129438402wcmsmn62520151:24000

Map of Series Extent

Approximate geographic distribution of the EVELETH 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 .