Soil Data Explorer - ELLIOTTSVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the ELLIOTTSVILLE soil series. This aggregation is based on all pedons with a current taxon name of ELLIOTTSVILLE, 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 ELLIOTTSVILLE were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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
143	10N0305	2009ME003001	Elliottsville	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.9811944,-69.1819167
143	08N0116	S07ME003006.Elliottsville	Elliottsville	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.9500639,-69.3167694
143	10N0317	S09ME021001.Elliottsville	Elliottsville	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.5350278,-68.9985
144B	02N0650	ME-02-11-019-43	Elliottsville	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.9383333,-69.1716667

Water Balance

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

Competing Series

Soil series competing with ELLIOTTSVILLE 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 ELLIOTTSVILLE 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 ELLIOTTSVILLE 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).

Soil series sharing subgroup-level classification with ELLIOTTSVILLE, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. ME-2010-09-03-02 | Franklin County Area and Part of Somerset County - 2003

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

Map Units

Map units containing ELLIOTTSVILLE 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
Chesuncook-Elliottsville-Telos association, 3 to 15 percent slopes, very stony	ECC	7878	285003	2t0jv	me610	1992	1:20000
Monson-Elliottsville-Telos complex, 3 to 15 percent slopes, very stony	MVC	6827	285028	2w3z2	me610	1992	1:20000
Elliottsville-Monson complex, 15 to 30 percent slopes, very stony	EME	5341	285005	2w3y0	me610	1992	1:20000
Elliottsville-Monson complex, 3 to 15 percent slopes, very stony	EMC	4315	285004	2w3xz	me610	1992	1:20000
Thorndike-Elliottsvillle complex, 3 to 15 percent slopes, very rocky	TOC	2834	285063	2wqmg	me610	1992	1:20000
Elliottsville-Thorndike complex, 8 to 15 percent slopes	EtC	1717	285007	2wqn2	me610	1992	1:20000
Elliottsville-Thorndike complex, 3 to 8 percent slopes	EtB	763	285006	2wqn1	me610	1992	1:20000
Thorndike-Elliottsville complex, 15 to 45 percent slopes, very rocky	TOE	589	285064	2wqmr	me610	1992	1:20000
Elliottsville-Thorndike complex, 15 to 25 percent slopes, very rocky	EtD	324	285008	2wqn3	me610	1992	1:20000
Chesuncook-Elliottsville-Telos association, 3 to 15 percent slopes, very stony	CEC	38498	1483065	1ls7t	me612	2016	1:24000
Elliottsville-Monson complex, 3 to 15 percent slopes, rocky	EXC	18622	744558	szs0	me612	2016	1:24000
Elliottsville-Chesuncook association, 3 to 8 percent slopes	EcB	10406	741290	swcl	me612	2016	1:24000
Monson-Elliottsville-Abram complex, 8 to 30 percent slopes, very rocky	MVD	9540	746067	t1bp	me612	2016	1:24000
Elliottsville-Chesuncook association, 3 to 8 percent slopes, very stony	ElB	8276	2481992	2p9q8	me612	2016	1:24000
Chesuncook-Elliottsville association, 15 to 30 percent slopes, very stony	CED	4399	744549	szrq	me612	2016	1:24000
Elliottsville-Monson complex, 3 to 8 percent slopes	EmB	3864	1483060	1ls7n	me612	2016	1:24000
Elliottsville-Chesuncook association, 8 to 15 percent slopes, very stony	ElC	3208	2481991	2p9q7	me612	2016	1:24000
Elliottsville-Monson complex, 3 to 8 percent slopes, rocky	EvB	2381	2482005	2p9qp	me612	2016	1:24000
Chesuncook-Elliottsville association, 8 to 15 percent slopes	EcC	2292	1483000	1ls5q	me612	2016	1:24000
Monson-Elliottsville-Abram complex, 3 to 8 percent slopes, rocky	EaB	1685	1482287	1lrfq	me612	2016	1:24000
Elliottsville-Urban land-Chesuncook association, 0 to 15 percent slopes	EuC	1549	2396088	2lfb5	me612	2016	1:24000
Monson-Elliottsville complex, 8 to 15 percent slopes, rocky	MeC	1370	2482004	2p9qn	me612	2016	1:24000
Elliottsville-Monson complex, 8 to 15 percent slopes	EmC	1283	1483059	1ls7m	me612	2016	1:24000
Elliottsville-Chesuncook association, 15 to 30 percent slopes, very stony	ElD	788	2752433	2synp	me612	2016	1:24000
Monson-Elliottsville-Abram complex, 15 to 30 percent slopes, rocky	MeD	669	2752436	2syns	me612	2016	1:24000
Monson-Elliottsville-Abram complex, 8 to 15 percent slopes, rocky	EaC	593	1483062	1ls7q	me612	2016	1:24000
Elliottsville-Monson-Abram complex, 30 to 60 percent slopes, rocky	MVE	494	746068	t1bq	me612	2016	1:24000
Telos-Chesuncook-Elliottsville association, 3 to 15 percent slopes, very stony	TLC	27652	285367	2t0jq	me615	1994	1:24000
Monson-Elliottsville-Knob Lock complex, 8 to 30 percent slopes, very rocky	MYD	25733	285345	2w3y4	me615	1994	1:24000
Chesuncook-Elliottsville-Telos association, 15 to 35 percent slopes, very stony	CFD	7903	285309	2t0jt	me615	1994	1:24000
Monson-Elliottsville-Knob Lock complex, 30 to 60 percent slopes, very rocky	MYE	6613	285346	2w3y5	me615	1994	1:24000
Elliottsville-Monson complex, 15 to 30 percent slopes, very stony	EMD	4850	285327	2w3y0	me615	1994	1:24000
Elliottsville-Monson complex, 3 to 15 percent slopes, very stony	EMC	4691	285326	2w3xz	me615	1994	1:24000
Elliottsville-Chesuncook complex, 3 to 8 percent slopes	EcB	258	285330	2w10n	me615	1994	1:24000
Chesuncook-Elliottsville-Telos association, 3 to 15 percent slopes, very stony	CKC	2432	285539	2t0jv	me617	2004	1:24000
Telos-Elliottsville-Monarda complex, 0 to 8 percent slopes, very stony	TEB	1762	285625	2w3zb	me617	2004	1:24000
Danforth-Elliottsville association, 3 to 15 percent slopes, extremely stony	DAC	1344	285558	2x1dm	me617	2004	1:24000
Elliottsville-Monson complex, 3 to 15 percent slopes, very stony	EMC	990	285567	2w3xz	me617	2004	1:24000
Elliottsville-Chesuncook complex, 3 to 8 percent slopes	EcB	250	285568	2w10n	me617	2004	1:24000
Telos-Chesuncook-Elliottsville association, 3 to 15 percent slopes, very stony	TEC	155631	285695	2t0jq	me619	2005	1:24000
Elliottsville-Monson complex, 3 to 15 percent slopes, very stony	EMC	66586	285707	2w3xz	me619	2005	1:24000
Chesuncook-Elliottsville-Telos association, 15 to 35 percent slopes, very stony	CHD	53525	285696	2t0jt	me619	2005	1:24000
Monson-Elliottsville-Knob Lock complex, 30 to 60 percent slopes, very rocky	MVE	51926	285715	2w3y5	me619	2005	1:24000
Elliottsville-Monson complex, 15 to 30 percent slopes, very stony	EMD	48324	285708	2w3y0	me619	2005	1:24000
Danforth-Elliottsville association, 3 to 15 percent slopes, extremely stony	DEC	45455	285663	2x1dm	me619	2005	1:24000
Monson-Elliottsville-Knob Lock complex, 8 to 30 percent slopes, very rocky	MVC	38523	285714	2w3y4	me619	2005	1:24000
Danforth-Elliottsville association, 15 to 30 percent slopes, extremely stony	DED	10098	285664	2x1dn	me619	2005	1:24000
Elliottsville-Monson complex, 25 to 60 percent slopes, rocky	EME	5954	285709	2w3yx	me619	2005	1:24000
Chesuncook-Elliottsville-Telos association, 3 to 15 percent slopes, very stony	CHC	5588	285652	2t0jv	me619	2005	1:24000
Chesuncook-Elliottsville association, 15 to 35 percent slopes, very stony	CEE	53172	2549957	2t0k0	me620	2011	1:24000
Monson-Knob Lock-Elliottsville complex, 15 to 60 percent slopes, very rocky	MKE	40189	2549927	2t0k2	me620	2011	1:24000
Monson-Elliottsville complex, 15 to 35 percent slopes, rocky	MEE	24052	2549925	2w3y1	me620	2011	1:24000
Chesuncook-Elliottsville association, 15 to 35 percent slopes, very stony	CEE	79780	2549860	2t0k0	me621	2011	1:24000
Monson-Elliottsville complex, 15 to 35 percent slopes, rocky	MEE	45732	2549865	2w3y1	me621	2011	1:24000
Monson-Knob Lock-Elliottsville complex, 15 to 60 percent slopes, very rocky	MKE	9438	2549867	2t0k2	me621	2011	1:24000
Danforth-Elliottsville association, 3 to 15 percent slopes, extremely stony	DEC	25745	1909086	2x1dm	me622	2007	1:24000
Telos-Chesuncook-Elliottsville association, 3 to 15 percent slopes, very stony	TEC	25594	1909295	2t0jq	me622	2007	1:24000
Elliottsville-Knob Lock-Monson complex, 3 to 25 percent slopes, very rocky	EKC	6994	1909304	2w3yw	me622	2007	1:24000
Chesuncook-Elliottsville-Telos association, 15 to 35 percent slopes, very stony	CED	5659	1909296	2t0jt	me622	2007	1:24000
Chesuncook-Elliottsville-Telos association, 3 to 15 percent slopes, very stony	CEC	5316	1908952	2t0jv	me622	2007	1:24000
Elliottsville-Monson complex, 3 to 15 percent slopes, very stony	EMC	3702	1909301	2w3xz	me622	2007	1:24000
Monson-Elliottsville-Knob Lock complex, 30 to 60 percent slopes, very rocky	MXF	3553	1909305	2w3y5	me622	2007	1:24000
Chesuncook-Elliottsville-Telos association, moderately steep, very stony	882D	198	280757	9f4p	nh607	2000	1:24000
Telos-Chesuncook-Elliottsvlle association, gently sloping, very stony	782B	191	280746	9f4b	nh607	2000	1:24000

Map of Series Extent

Approximate geographic distribution of the ELLIOTTSVILLE 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).