Soil Data Explorer - EAGLEVIEW

Official Series Description

Lab Data Summary

Aggregate lab data for the EAGLEVIEW soil series. This aggregation is based on all pedons with a current taxon name of EAGLEVIEW, 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 EAGLEVIEW were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
88	UMN1000	S1969MN0611000	Eagleview	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.5628281,-94.1146164

Water Balance

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

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the EAGLEVIEW series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the EAGLEVIEW series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the EAGLEVIEW 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 (updated 2024-10-23).

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

Competing Series

Soil series competing with EAGLEVIEW share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the EAGLEVIEW series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the EAGLEVIEW 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 (updated 2024-10-23).

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

Soil series sharing subgroup-level classification with EAGLEVIEW, 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 (updated 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing EAGLEVIEW 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
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	7729	397573	2x14c	mn005	1994	1:20000
Eagleview and Menahga soils, 3 to 15 percent slopes	A1C	7585	397574	2x14d	mn005	1994	1:20000
Eagleview-Menahga complex, 15 to 30 percent slopes	867E	4825	397575	2t4t9	mn005	1994	1:20000
Bootlake-Eagleview complex, 1 to 8 percent slopes	1252B	4729	397467	fblj	mn005	1994	1:20000
Eagleview-Balmlake complex, 1 to 8 percent slopes	1132B	2799	397419	fbjz	mn005	1994	1:20000
Eagleview-Snellman complex, 1 to 8 percent slopes	1140B	2613	397429	fbk9	mn005	1994	1:20000
Eagleview-Bootlake complex, 8 to 15 percent slopes	1263C	2272	397468	fblk	mn005	1994	1:20000
Eagleview-Balmlake complex, 8 to 15 percent slopes	1132C	1683	397420	fbk0	mn005	1994	1:20000
Eagleview-Snellman complex, 8 to 15 percent slopes	1140C	1375	397430	fbkb	mn005	1994	1:20000
Eagleview-Balmlake complex, 15 to 30 percent slopes	1132E	705	397421	fbk1	mn005	1994	1:20000
Sybil-Eagleview complex, 8 to 15 percent slopes	1195C	268	397433	fbkf	mn005	1994	1:20000
Sybil-Eagleview complex, 2 to 8 percent slopes	1195B	226	397432	fbkd	mn005	1994	1:20000
Sybil-Eagleview complex, 15 to 30 percent slopes	1195E	89	397434	fbkg	mn005	1994	1:20000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	61057	3026512	2x14c	mn007	1991	1:24000
Eagleview and Menahga soils, 3 to 15 percent slopes	A1C	10492	3026513	2x14d	mn007	1991	1:24000
Eagleview-Two Inlets complex, 1 to 8 percent slopes, pitted	2018B	2700	2520474	2qkjj	mn007	1991	1:24000
Eagleview-Two Inlets complex, 15 to 30 percent slopes	2018E	946	2520476	2qkjn	mn007	1991	1:24000
Eagleview-Two Inlets complex, 8 to 15 percent slopes, pitted	2018C	120	2520475	2qkjk	mn007	1991	1:24000
Eagleview-Menahga complex, 1 to 8 percent slopes	D36B	268	753006	2t4t7	mn009	2007	1:12000
Eagleview-Menahga complex, 8 to 15 percent slopes	D36C	23	753005	2t4t8	mn009	2007	1:12000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	6571	3026519	2x14c	mn021	1993	1:20000
Eagleview and Menahga soils, 3 to 15 percent slopes	A1C	369	3026520	2x14d	mn021	1993	1:20000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	3111	430602	2x14c	mn029	1993	1:20000
Eagleview and Menahga soils, 3 to 15 percent slopes	A1C	1875	430603	2x14d	mn029	1993	1:20000
Eagleview-Menahga complex, 15 to 30 percent slopes	867E	736	430605	2t4t9	mn029	1993	1:20000
Eagleview-Two Inlets complex, 1 to 8 percent slopes, pitted	2018B	281	2603645	2qkjj	mn029	1993	1:20000
Eagleview-Two Inlets complex, 15 to 30 percent slopes	2018E	27	2603646	2qkjn	mn029	1993	1:20000
Nymore-Eagleview complex, Mississippi River Valley, pitted, 8 to 15 percent slopes	D96C	955	2732682	2sln5	mn035	2009	1:24000
Nymore-Eagleview complex, Mississippi River Valley, pitted, 1 to 8 percent slopes	D96B	530	2732681	2sln4	mn035	2009	1:24000
Eagleview-Nymore-Corliss complex, Mississippi River Valley, 15 to 60 percent slopes	D99G	455	2732686	2slnb	mn035	2009	1:24000
Nymore-Eagleview complex, Mississippi River Valley, pitted, 15 to 30 percent slopes	D96E	201	2732683	2sln7	mn035	2009	1:24000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	26445	436739	2x14c	mn057	1998	1:24000
Two Inlets-Eagleview-Steamboat complex, pitted, 3 to 15 percent slopes	675C	23233	436694	gndx	mn057	1998	1:24000
Two Inlets-Eagleview-Steamboat complex, pitted, 15 to 35 percent slopes	675E	15750	436695	gndy	mn057	1998	1:24000
Eagleview-Menahga complex, 15 to 30 percent slopes	867E	5670	436741	2t4t9	mn057	1998	1:24000
Eagleview and Menahga soils, 3 to 15 percent slopes	A1C	4969	436740	2x14d	mn057	1998	1:24000
Two Inlets-Eagleview-Steamboat complex, pitted, 35 to 65 percent slopes	675G	2827	436696	gndz	mn057	1998	1:24000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	124186	3026530	2x14c	mn061	1982	1:24000
Eagleview and Menahga soils, 3 to 15 percent slopes	A1C	3254	3026531	2x14d	mn061	1982	1:24000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	1715	399259	2x14c	mn087	1992	1:20000
Sybil-Eagleview complex, 2 to 8 percent slopes	1195B	11451	435547	gm6x	mn111	1996	1:20000
Sybil-Eagleview complex, 8 to 15 percent slopes	1195C	4092	435548	gm6y	mn111	1996	1:20000
Leaflake-Eagleview complex, 1 to 6 percent slopes	716B	3613	435909	gmll	mn111	1996	1:20000
Sybil-Eagleview complex, 15 to 30 percent slopes	1195E	1628	435549	gm6z	mn111	1996	1:20000
Sybil-Eagleview complex, 0 to 2 percent slopes	1195A	1544	435546	gm6w	mn111	1996	1:20000
Leaflake-Eagleview complex, 6 to 12 percent slopes	716C	579	435910	gmlm	mn111	1996	1:20000
Leaflake-Eagleview complex, 12 to 20 percent slopes	716D	99	435911	gmln	mn111	1996	1:20000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	27026	3026534	2x14c	mn159	1987	1:20000
Eagleview and Menahga soils, 3 to 15 percent slopes	A1C	1537	3026535	2x14d	mn159	1987	1:20000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	167	2406876	2x14c	mn613	2016	1:24000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	65	3026541	2x14c	mn619	2009	1:24000
Eagleview and Menahga soils, 1 to 8 percent slopes	A1B	5758	822890	2x14c	mn621	2006	1:24000

Map of Series Extent

Approximate geographic distribution of the EAGLEVIEW 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 (updated 2024-10-30).