Soil Data Explorer - COSHOCTON

Official Series Description

Lab Data Summary

Aggregate lab data for the COSHOCTON soil series. This aggregation is based on all pedons with a current taxon name of COSHOCTON, 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 COSHOCTON 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
124	CS-005	1965-OH031-005	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.36778,-81.789444
n/a	MS-s05	1961-OH119-S05	Coshocton	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	TU-w08	1961-OH157-W08	Coshocton	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CS-006	1965-OH031-006	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	HL-002	1970-OH075-002	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	HL-004	1970-OH075-004	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AS-021	1972-OH005-021	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CS-030	1976-OH031-030	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CS-032	1976-OH031-032	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CA-030	1978-OH019-030	Coshocton	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	TU-019	1979-OH157-019	Coshocton	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	HL-006	1985-OH075-006	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MS-029	1986-OH119-029	Coshocton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COSHOCTON 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 COSHOCTON series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the COSHOCTON 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 2023-10-09).

Geomorphic description summaries for the COSHOCTON 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 2023-10-04).

Competing Series

Soil series competing with COSHOCTON share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the COSHOCTON 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 2023-10-09).

Geomorphic description summaries for the COSHOCTON 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 2023-10-04).

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 COSHOCTON, 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 2023-10-02).

Block Diagrams

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

1. OH-2010-09-29-12 | Coshocton County - 2001

   Typical pattern of soils and parent material in the Bethesda-Coshocton-Westmoreland association (Soil Survey of Coshocton County, Ohio; 2001).

2. OH-2010-09-29-13 | Coshocton County - 2001

   Typical pattern of soils and parent material in the Coshocton-Westmoreland-Rigley association (Soil Survey of Coshocton County, Ohio; 2001).

3. OH-2010-09-29-14 | Coshocton County - 2001

   Typical pattern of soils and parent material in the Coshocton-Brownsville-Westmoreland association (Soil Survey of Coshocton County, Ohio; 2001).

Map Units

Map units containing COSHOCTON 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
Coshocton loam, 6 to 15 percent slopes	CvC	355	288155	2xqvy	oh005	1976	1:15840
Coshocton loam, 2 to 6 percent slopes	CvB	172	288154	9nv9	oh005	1976	1:15840
Coshocton silt loam, 2 to 6 percent slopes	CxB	13	1592636	2xqw0	oh005	1976	1:15840
Coshocton silt loam, 6 to 15 percent slopes, eroded	CxC2	3	1592637	2xqw3	oh005	1976	1:15840
Westmoreland-Coshocton silt loams, 15 to 25 percent slopes	WmD	47735	538016	l1vc	oh019	1981	1:15840
Westmoreland-Coshocton silt loams, 8 to 15 percent slopes	WmC	38191	538015	l1vb	oh019	1981	1:15840
Coshocton-Keene silt loams, 3 to 8 percent slopes	CoB	9294	537975	l1t1	oh019	1981	1:15840
Coshocton silt loam, 3 to 8 percent slopes	CnB	4666	537974	2xqw4	oh019	1981	1:15840
Coshocton silt loam, 15 to 25 percent slopes	CpD	785	1670018	2xqw6	oh019	1981	1:15840
Coshocton silt loam, 6 to 15 percent slopes	CpC	318	1670017	2xqw2	oh019	1981	1:15840
Gilpin-Coshocton complex, 15 to 25 percent slopes	GkD	142	1670024	1t1sr	oh019	1981	1:15840
Gilpin-Coshocton complex, 6 to 15 percent slopes	GkC	127	1670023	1t1sq	oh019	1981	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes	CsD	103	1589698	2z52p	oh019	1981	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes, very stony	CtD	63	1589699	2z52t	oh019	1981	1:15840
Coshocton silt loam, 2 to 6 percent slopes	CpB	41	1670678	2xqw0	oh019	1981	1:15840
Coshocton-Guernsey silt loams, 8 to 15 percent slopes	CsC	29	1589697	2z52r	oh019	1981	1:15840
Coshocton silt loam, 6 to 15 percent slopes	CoC	9256	298755	b0w8	oh029	2005	1:12000
Gilpin-Coshocton silt loams, 6 to 15 percent slopes	GoC	6847	298780	b0x2	oh029	2005	1:12000
Westmoreland-Coshocton silt loams, 8 to 15 percent slopes	WmC	1293	298849	b0z9	oh029	2005	1:12000
Gilpin-Coshocton silt loams, 15 to 25 percent slopes	GoD	1235	298781	b0x3	oh029	2005	1:12000
Coshocton silt loam, 2 to 6 percent slopes	CoB	935	298754	2xqw0	oh029	2005	1:12000
Gilpin-Coshocton-Urban land complex, 6 to 15 percent slopes	GpC	376	300247	b2fd	oh029	2005	1:12000
Coshocton silt loam, 15 to 25 percent slopes	CoD	324	298756	2xqw6	oh029	2005	1:12000
Westmoreland-Coshocton silt loams, 15 to 25 percent slopes	WmD	86	298850	b0zb	oh029	2005	1:12000
Coshocton silt loam, 15 to 25 percent slopes	CoD	55138	536618	2xqw6	oh031	1996	1:15840
Coshocton silt loam, 6 to 15 percent slopes, eroded	CoC2	25377	536617	2xqw3	oh031	1996	1:15840
Coshocton-Westmoreland complex, 25 to 35 percent slopes	CsE	13374	536625	l0dh	oh031	1996	1:15840
Coshocton-Westmoreland complex, 15 to 25 percent slopes	CsD	6547	536624	l0dg	oh031	1996	1:15840
Coshocton silt loam, 15 to 25 percent slopes, very stony	CpD	5981	536621	2xqw8	oh031	1996	1:15840
Coshocton silt loam, 25 to 35 percent slopes	CoE	4951	536619	2rfbd	oh031	1996	1:15840
Coshocton silt loam, 2 to 6 percent slopes	CoB	2626	536616	2xqw0	oh031	1996	1:15840
Coshocton-Rigley complex, 25 to 35 percent slopes	CrE	1510	536623	l0df	oh031	1996	1:15840
Coshocton silt loam, 6 to 15 percent slopes, very stony	CpC	894	536620	l0db	oh031	1996	1:15840
Coshocton-Westmoreland silt loams, 25 to 40 percent slopes	CtE	559	2108958	28sjx	oh031	1996	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes	CuD	436	2108981	2z52p	oh031	1996	1:15840
Coshocton silt loam, 15 to 25 percent slopes, eroded	CoD2	223	2108998	2xqw7	oh031	1996	1:15840
Coshocton-Rigley complex, 15 to 25 percent slopes	CrD	158	536622	l0dd	oh031	1996	1:15840
Rigley-Coshocton complex, 25 to 40 percent slopes	RkE	77	2108965	28sk4	oh031	1996	1:15840
Coshocton silt loam, 8 to 15 percent slopes, eroded	CnC2	36	2108972	2xqw5	oh031	1996	1:15840
Westmoreland-Coshocton complex, 8 to 15 percent slopes, eroded	WlC2	16	2108999	28sl7	oh031	1996	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes, very stony	CvD	2	2108982	2z52t	oh031	1996	1:15840
Coshocton loam, 15 to 25 percent slopes	CoD	457	536884	2xqvz	oh059	1998	1:15840
Coshocton silt loam, 8 to 15 percent slopes, eroded	CsC2	220	536885	2xqw5	oh059	1998	1:15840
Coshocton silt loam, 15 to 25 percent slopes	CsD	190	1592935	2xqw6	oh059	1998	1:15840
Coshocton silt loam, 3 to 8 percent slopes	CsB	3	1592956	2xqw4	oh059	1998	1:15840
Coshocton silt loam, 15 to 25 percent slopes	CnD	13772	536727	2xqw6	oh067	1993	1:15840
Westmoreland-Coshocton complex, 25 to 40 percent slopes	WmE	4993	536782	l0kk	oh067	1993	1:15840
Coshocton silt loam, 6 to 15 percent slopes	CnC	4708	536726	2xqw2	oh067	1993	1:15840
Gilpin-Coshocton complex, 6 to 15 percent slopes	GoC	1186	536740	l0j6	oh067	1993	1:15840
Coshocton silt loam, 2 to 6 percent slopes	CnB	606	536725	2xqw0	oh067	1993	1:15840
Gilpin-Coshocton complex, 15 to 25 percent slopes	GoD	477	536741	l0j7	oh067	1993	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes	CrD	107	1695499	2z52p	oh067	1993	1:15840
Coshocton-Guernsey silt loams, 25 to 40 percent slopes	CrE	23	1695500	2z52q	oh067	1993	1:15840
Westmoreland-Coshocton silt loams, 15 to 25 percent slopes	WtD	8	1695504	1tx9p	oh067	1993	1:15840
Coshocton silt loam, 6 to 15 percent slopes, eroded	CtC2	26922	286893	2xqw3	oh075	1989	1:15840
Coshocton silt loam, 15 to 25 percent slopes, eroded	CtD2	24440	286894	2xqw7	oh075	1989	1:15840
Coshocton silt loam, 2 to 6 percent slopes	CtB	7120	286892	2xqw0	oh075	1989	1:15840
Coshocton silt loam, 12 to 25 percent slopes, very stony	CvD	4345	286896	9mjq	oh075	1989	1:15840
Coshocton silt loam, 25 to 35 percent slopes	CtE	2830	286895	2rfbd	oh075	1989	1:15840
Westmoreland-Coshocton complex, 15 to 25 percent slopes, eroded	WgD2	2045	286943	9ml7	oh075	1989	1:15840
Westmoreland-Coshocton complex, 8 to 15 percent slopes, eroded	WgC2	1800	286942	9ml6	oh075	1989	1:15840
Coshocton silt loam, 15 to 25 percent slopes	CtD	493	1677002	2xqw6	oh075	1989	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes	CwD	187	1677013	2z52p	oh075	1989	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes, very stony	CxD	151	1677015	2z52t	oh075	1989	1:15840
Coshocton-Westmoreland complex, 15 to 25 percent slopes	CzD	36	1677004	1t91x	oh075	1989	1:15840
Coshocton-Guernsey silt loams, 25 to 40 percent slopes	CwE	14	1677014	2z52q	oh075	1989	1:15840
Coshocton silt loam, 15 to 25 percent slopes, very stony	CuD	3	1677003	2xqw8	oh075	1989	1:15840
Gilpin-Coshocton silt loams, 8 to 15 percent slopes	GoC	9714	536079	kztw	oh081	1987	1:15840
Gilpin-Coshocton silt loams, 15 to 25 percent slopes	GoD	7088	536080	kztx	oh081	1987	1:15840
Coshocton silt loam, 1 to 7 percent slopes	CnB	1052	536066	kztg	oh081	1987	1:15840
Gilpin-Coshocton complex, 6 to 15 percent slopes	GmC	495	1652939	1sh0m	oh081	1987	1:15840
Westmoreland-Coshocton silt loams, 8 to 15 percent slopes	WmC	8	1652984	1sh22	oh081	1987	1:15840
Coshocton silt loam, 6 to 15 percent slopes	CoC	4	1652977	2xqw2	oh081	1987	1:15840
Coshocton silt loam, 2 to 6 percent slopes	CoB	1	1652976	2xqw0	oh081	1987	1:15840
Coshocton silt loam, 2 to 6 percent slopes	CvB	1655	613574	2xqw0	oh083	1983	1:15840
Coshocton silt loam, 6 to 12 percent slopes	CvC	1523	613575	nlgr	oh083	1983	1:15840
Coshocton silt loam, 12 to 18 percent slopes	CvD	1009	613576	nlgs	oh083	1983	1:15840
Rigley-Coshocton complex, 18 to 25 percent slopes	RhE	413	614622	nmkj	oh083	1983	1:15840
Coshocton silt loam, 15 to 25 percent slopes	CtD	106	2216003	2xqw6	oh083	1983	1:15840
Coshocton-Rigley complex, 15 to 25 percent slopes	CxD	33	2216005	2dcy1	oh083	1983	1:15840
Coshocton silt loam, 15 to 25 percent slopes, eroded	CtD2	24	1593064	2xqw7	oh083	1983	1:15840
Coshocton silt loam, 6 to 15 percent slopes, eroded	CtC2	20	1593063	2xqw3	oh083	1983	1:15840
Coshocton loam, 6 to 15 percent slopes	CsC	1	1593056	2xqvy	oh083	1983	1:15840
Coshocton silt loam, 12 to 18 percent slopes, eroded	CoD2	13755	171021	5qyt	oh089	1986	1:15840
Coshocton silt loam, 6 to 12 percent slopes, eroded	CoC2	10630	171020	2xqw1	oh089	1986	1:15840
Coshocton silt loam, 18 to 25 percent slopes, eroded	CoE2	2455	171022	5qyv	oh089	1986	1:15840
Rigley-Coshocton complex, 18 to 25 percent slopes	RhE	1765	171076	5r0l	oh089	1986	1:15840
Coshocton silt loam, 2 to 6 percent slopes	CoB	880	171019	2xqw0	oh089	1986	1:15840
Coshocton silt loam, 15 to 25 percent slopes	CsD	188	1540766	2xqw6	oh089	1986	1:15840
Rigley-Coshocton complex, 25 to 40 percent slopes	RhF	40	1540775	1nq9f	oh089	1986	1:15840
Coshocton silt loam, 8 to 15 percent slopes, eroded	CsC2	24	1540765	2xqw5	oh089	1986	1:15840
Coshocton silt loam, 6 to 15 percent slopes, eroded	CtC2	11	2216048	2xqw3	oh089	1986	1:15840
Coshocton-Westmoreland silt loams, 25 to 40 percent slopes	CtE	19686	537879	l1py	oh119	1989	1:15840
Coshocton silt loam, 15 to 25 percent slopes	CsD	19655	537878	2xqw6	oh119	1989	1:15840
Coshocton silt loam, 8 to 15 percent slopes, eroded	CsC2	10428	537877	2xqw5	oh119	1989	1:15840
Rigley-Coshocton complex, 25 to 40 percent slopes	RhE	8642	537933	l1rp	oh119	1989	1:15840
Coshocton loam, 6 to 15 percent slopes	CvC	3	1406551	2xqvy	oh139	1971	1:15840
Westmoreland-Coshocton silt loams, 15 to 25 percent slopes	WpD	83	1595503	1qk7v	oh151	1967	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes	CsD	78	1595461	2z52p	oh151	1967	1:15840
Westmoreland-Coshocton silt loams, 8 to 15 percent slopes	WpC	74	1595502	1qk7t	oh151	1967	1:15840
Coshocton-Guernsey silt loams, 8 to 15 percent slopes	CsC	37	1595460	2z52r	oh151	1967	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes, very stony	CxD	12	1595464	2z52t	oh151	1967	1:15840
Coshocton silt loam, 15 to 25 percent slopes, eroded	CtD2	10	1595454	2xqw7	oh151	1967	1:15840
Coshocton-Guernsey silt loams, 25 to 40 percent slopes	CsE	6	1595462	2z52q	oh151	1967	1:15840
Coshocton silt loam, 6 to 12 percent slopes	CtC	4	1595475	1qk6y	oh151	1967	1:15840
Coshocton-Guernsey silt loams, 8 to 15 percent slopes, very stony	CxC	4	1595463	2z52s	oh151	1967	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes	CsD	42775	536299	2z52p	oh157	1981	1:15840
Coshocton-Guernsey silt loams, 8 to 15 percent slopes	CsC	17422	536298	2z52r	oh157	1981	1:15840
Coshocton-Guernsey silt loams, 25 to 40 percent slopes	CsE	5200	536300	2z52q	oh157	1981	1:15840
Coshocton-Guernsey silt loams, 15 to 25 percent slopes, very stony	CtD	4500	536302	2z52t	oh157	1981	1:15840
Coshocton silt loam, 3 to 8 percent slopes	CpB	3030	536297	2xqw4	oh157	1981	1:15840
Coshocton-Guernsey silt loams, 8 to 15 percent slopes, very stony	CtC	460	536301	2z52s	oh157	1981	1:15840
Coshocton silt loam, 6 to 15 percent slopes, eroded	ChC2	331	1589447	2xqw3	oh157	1981	1:15840
Westmoreland-Coshocton silt loams, 15 to 25 percent slopes	WkD	297	1589445	1qbyf	oh157	1981	1:15840
Coshocton loam, 15 to 25 percent slopes	CrD	250	1589372	2xqvz	oh157	1981	1:15840
Westmoreland-Coshocton silt loams, 8 to 15 percent slopes	WkC	60	1589444	1qbyd	oh157	1981	1:15840
Coshocton silt loam, 6 to 15 percent slopes	ChC	27	1589386	2xqw2	oh157	1981	1:15840
Coshocton silt loam, 8 to 15 percent slopes, eroded	CpC2	7	1589373	2xqw5	oh157	1981	1:15840
Westmoreland-Coshocton complex, 8 to 15 percent slopes, eroded	WlC2	7	1589419	1qbxl	oh157	1981	1:15840
Coshocton-Keene silt loams, 3 to 8 percent slopes	CyB	4	1589442	1qbyb	oh157	1981	1:15840
Coshocton silt loam, 15 to 25 percent slopes	CpD	3	1589396	2xqw6	oh157	1981	1:15840
Coshocton silt loam, 2 to 6 percent slopes	ChB	1	1589407	2xqw0	oh157	1981	1:15840
Coshocton silt loam, 6 to 12 percent slopes	CtC	265	287186	9mv2	oh169	1981	1:15840

Map of Series Extent

Approximate geographic distribution of the COSHOCTON 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 2023-10-04).