Official Series Description


Lab Data Summary

Aggregate lab data for the EAGLESNEST soil series. This aggregation is based on all pedons with a current taxon name of EAGLESNEST, 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 EAGLESNEST 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
88UMN4225S1989MN0074225Eaglesnest3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.2519913,-95.049263
93AUMN2060S1975MN137006 (2060)Eaglesnest3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.649189,-91.8871002
93A97P0209S1995MN137016Eaglesnest6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.7127762,-92.515831

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the EAGLESNEST 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 EAGLESNEST 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 EAGLESNEST 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 EAGLESNEST 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 EAGLESNEST 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 EAGLESNEST 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 EAGLESNEST 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 EAGLESNEST, 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 EAGLESNEST 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-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyI2a31D2498427745792wcmsmn03120131:24000
Eaglesnest-Wahlsten complex, 2 to 8 percent slopes, bouldery, very rockyF2B446131148432ls2zmn03120131:24000
Conic, bouldery-Rock outcrop-Eaglesnest, bouldery complex, 2 to 18 percent slopesI2c22D196727746292t20smn03120131:24000
Eaglesnest-Babbitt complex, 1 to 8 percent slopes, boulderyI3-30B182927745632t211mn03120131:24000
Babbitt-Lithic Endoaquepts-Eaglesnest complex, 0 to 8 percent slopes, boulderyI2c20B140527746872t20qmn03120131:24000
Eaglesnest, bouldery-Wahlsten, bouldery complex, 2 to 8 percent slopes, very rockyI2a30B27827744852t209mn03120131:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyI2a31D2067431149232wcmsmn07520131:24000
Conic, bouldery-Rock outcrop-Eaglesnest, bouldery complex, 2 to 18 percent slopesI2c22D1402031149322t20smn07520131:24000
Eaglesnest-Babbitt complex, 1 to 8 percent slopes, boulderyI3-30B279631149392t211mn07520131:24000
Eaglesnest-Wahlsten complex, 2 to 8 percent slopes, bouldery, very rockyF2B96831149652ls2zmn07520131:24000
Longsiding-Eaglesnest, bouldery, complex, 1 to 8 percent slopesF38B831149772lt5nmn07520131:24000
Conic, bouldery-Rock outcrop-Eaglesnest, bouldery, complex, 0 to 18 percent slopesF209D8820824079722ltpjmn61320161:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyF3D4626624064372wcmsmn61320161:24000
Babbitt-Lithic Endoaquepts-Eaglesnest complex, 0 to 8 percent slopes, boulderyF210B1108924079742ltplmn61320161:24000
Eaglesnest-Wahlsten complex, 2 to 8 percent slopes, bouldery, very rockyF2B1050624064362ls2zmn61320161:24000
Longsiding-Eaglesnest, bouldery, complex, 1 to 8 percent slopesF38B639024074802lt5nmn61320161:24000
Soudan-Eaglesnest-Babbitt complex, 1 to 8 percent slopes, boulderyF6B15722494000wmd6mn61320161:24000
Eaglesnest stony loam, 2 to 8 percent slopes, boulderyF11B36124068962lsktmn61320161:24000
Eaglesnest-Babbitt complex, 1 to 8 percent slopes, boulderyF12B29924068972lskvmn61320161:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyF3D2711818614452wcmsmn61720071:24000
Eaglesnest-Wahlsten complex, 2 to 8 percent slopes, boulderyF2B13355186144420gzlmn61720071:24000
Eaglesnest-Babbitt complex, 1 to 8 percent slopes, boulderyF12B12366186146220h05mn61720071:24000
Soudan-Eaglesnest-Babbitt complex, 1 to 8 percent slopes, boulderyF6B5838186145220gzvmn61720071:24000
Eaglesnest stony loam, 4 to 12 percent slopes, very boulderyF1C4397186143720gzcmn61720071:24000
Eveleth-Eaglesnest complex, 2 to 20 percent slopes, very boulderyF177C27051913133226rzmn61720071:24000
Eaglesnest stony loam, 2 to 8 percent slopes, boulderyF11B2281186146120h04mn61720071:24000
Longsiding-Eaglesnest, bouldery, complex, 0 to 8 percent slopesF38B781186143020gz4mn61720071:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyF3D178138229972wcmsmn62120061:24000
Eaglesnest-Babbitt complex, 1 to 8 percent slopes, boulderyF12B6366823023wmf4mn62120061:24000
Eaglesnest-Wahlsten complex, 2 to 8 percent slopes, boulderyF2B4666822998wmdbmn62120061:24000
Eaglesnest stony loam, 4 to 12 percent slopes, very boulderyF1C4143822999wmdcmn62120061:24000
Soudan-Eaglesnest-Babbitt complex, 1 to 8 percent slopes, boulderyF6B2783822994wmd6mn62120061:24000
Eaglesnest stony loam, 2 to 8 percent slopes, boulderyF11B1278823024wmf5mn62120061:24000
Longsiding-Eaglesnest, bouldery, complex, 0 to 8 percent slopesF38B126715364291nks7mn62120061:24000
Eaglesnest-Wahlsten complex, 2 to 8 percent slopes, boulderyF2B76029438392pfxzmn62520151:24000
Eveleth-Eagelsnest-Conic complex, bouldery, 6 to 18 percent slopes, very rockyF3D26129438402wcmsmn62520151:24000

Map of Series Extent

Approximate geographic distribution of the EAGLESNEST 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 .