Soil Data Explorer - MARKLAND

Official Series Description

Lab Data Summary

Aggregate lab data for the MARKLAND soil series. This aggregation is based on all pedons with a current taxon name of MARKLAND, 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 MARKLAND 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
114A	91P0433	90IN119013	Markland	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1805573,-86.9111099
114B	JN7923	1979IN071023	Markland	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7687111,-86.1530306
114B	WS8104	1981IN175004	Markland	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.76775,-86.0927194
115A	GN7925	1979IN055025	Markland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.963725,-87.1281361
120B	LW8008	1980IN093008	Markland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8402417,-86.5513611
120B	MT8103	1981IN101003	Markland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.74355,-86.7494056
120B	91P0434	90IN119014	Markland	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1722221,-86.7236099
120B	92P0613	S1992IN123003	Markland	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.0688896,-86.5097198
121	SW8108	1981IN155008	Markland	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7633167,-85.0932917
n/a	RO-034	1957-OH141-034	Markland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CL-009	1966-OH025-009	Markland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WS-003	1966-OH167-003	Markland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	JF7802	1978IN077002	Markland	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	HA-006	1978-OH061-006	Markland	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	80IL157082	1980IL157082	Markland	3	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 MARKLAND 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 MARKLAND series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the MARKLAND 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 MARKLAND 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).

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

Competing Series

Soil series competing with MARKLAND share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the MARKLAND 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 MARKLAND 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).

Soil series sharing subgroup-level classification with MARKLAND, 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. IN-2010-09-24-20 | Perry County -

   Typical pattern of soils and parent materials of alluvial, stream terrace lacustrine and aeolian landforms adjacent to hills underlain with interbedded shale and limestone in Ohio River Valley (Soil Survey of Perry County, Indiana).

2. IN-2012-01-19-30 | Jefferson County - May 1985

   Pattern of soils and parent material in the Huntington-Dearborn-Elkinsville map unit (Soil Survey of Jefferson County, Indiana; 1985).

3. IN-2012-01-19-40 | Perry County - September 1969

   Relationship of relief and geologic strata to certain of the soil series represented in Perry County. The vertical scale is greatly exaggerated (Soil Survey of Perry County, Indiana; 1969).

Map Units

Map units containing MARKLAND 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
Markland silt loam, 5 to 10 percent slopes, eroded	467C2	635	211676	2zczd	il059	1966	1:20000
Markland silt loam, 2 to 5 percent slopes	467B	522	211674	2zczb	il059	1966	1:20000
Markland silt loam, 7 to 12 percent slopes, eroded	467D2	467	211678	738b	il059	1966	1:20000
Markland silt loam, 2 to 5 percent slopes, eroded	467B2	358	211675	2zczc	il059	1966	1:20000
Markland silt loam, 12 to 18 percent slopes	467E	283	211679	738c	il059	1966	1:20000
Markland soils, 4 to 7 percent slopes, severely eroded	467C3	143	211677	7389	il059	1966	1:20000
Markland silt loam, 2 to 5 percent slopes, eroded	467B2	325	175141	2zczc	il065	1982	1:15840
Markland silty clay loam, 10 to 18 percent slopes, eroded	467D2	1843	200482	6qm5	il157	2001	1:12000
Markland silt loam, 5 to 10 percent slopes, eroded	467C2	1113	178888	2zczd	il165	1974	1:15840
Markland soils, 7 to 15 percent slopes, severely eroded	467D3	1028	178889	604m	il165	1974	1:15840
Markland silty clay loam, 12 to 18 percent slopes, severely eroded	467E3	146	179699	60zr	il185	1962	1:20000
Markland silty clay loam, 7 to 12 percent slopes, severely eroded	467D3	136	179698	60zq	il185	1962	1:20000
Markland silty clay loam, 4 to 7 percent slopes, severely eroded	467C3	72	179697	60zp	il185	1962	1:20000
Markland silt loam, 5 to 10 percent slopes, eroded, rarely flooded	7467C2	817	1543972	1ntmk	il193	2006	1:12000
Markland silt loam, 2 to 5 percent slopes, eroded, rarely flooded	7467B2	732	1543971	1ntmj	il193	2006	1:12000
Markland silt loam, 2 to 5 percent slopes, eroded	467B2	339	1543912	2zczc	il193	2006	1:12000
Markland silt loam, 5 to 10 percent slopes, eroded	467C2	224	1543913	2zczd	il193	2006	1:12000
Markland silty clay loam, 5 to 10 percent slopes, severely eroded	467C3	177	1543914	1ntkp	il193	2006	1:12000
Markland silt loam, 12 to 25 percent slopes, eroded, rarely flooded	MdqDQ	325	196659	6lmv	in019	2001	1:12000
Markland silt loam, 18 to 50 percent slopes, rarely flooded	McnGQ	268	201230	6rd9	in019	2001	1:12000
Markland silt loam, 6 to 12 percent slopes, eroded	McgC2	145	210705	727y	in019	2001	1:12000
Markland silty clay loam, 12 to 25 percent slopes, severely eroded, rarely flooded	McuDQ	49	201144	6r9j	in019	2001	1:12000
Markland silty clay loam, 6 to 12 percent slopes, severely eroded	McpC3	41	201136	6r98	in019	2001	1:12000
Markland silt loam, 25 to 70 percent slopes	MdeG	381	1652584	1sgn5	in025	1970	1:20000
Markland silty clay loam, 6 to 12 percent slopes, severely eroded	McpC3	278	1652553	1sgm5	in025	1970	1:20000
Markland silty clay loam, 12 to 18 percent slopes, severely eroded	McpD3	207	1652587	1sgn8	in025	1970	1:20000
Markland silt loam, 12 to 18 percent slopes, eroded	McgD2	136	1652583	1sgn4	in025	1970	1:20000
Markland silt loam, 2 to 6 percent slopes, eroded	MaB2	181	162959	5gkr	in027	1969	1:20000
Markland silt loam, 6 to 18 percent slopes, eroded	MaD2	80	162960	5gks	in027	1969	1:20000
Markland silt loam, 2 to 12 percent slopes, eroded	MaB2	780	1600662	1qqm8	in029	1979	1:15840
Markland silt loam, 18 to 35 percent slopes, eroded	MaF2	699	1600663	1qqm9	in029	1979	1:15840
Markland silty clay loam, 6 to 18 percent slopes, severely eroded	MbD3	307	1600664	1qqmb	in029	1979	1:15840
Markland silty clay loam, 6 to 12 percent slopes, severely eroded	McpC3	185	185246	66rp	in043	2000	1:12000
Markland silt loam, 18 to 50 percent slopes, rarely flooded	McnGQ	120	185265	66s9	in043	2000	1:12000
Markland silty clay loam, 12 to 25 percent slopes, severely eroded, rarely flooded	McuDQ	82	185176	66pf	in043	2000	1:12000
Markland silty clay loam, 2 to 6 percent slopes, eroded	MbB2	498	161555	5f3g	in055	1984	1:15840
Markland silty clay loam, 6 to 18 percent slopes, severely eroded	MdwD3	285	792095	vl7g	in061	2007	1:12000
Markland silt loam, 18 to 50 percent slopes, rarely flooded	McnGQ	280	775597	v128	in061	2007	1:12000
Markland silt loam, 6 to 18 percent slopes, eroded	MdlD2	255	1678257	1tbcb	in061	2007	1:12000
Markland silty clay loam, 6 to 12 percent slopes, severely eroded	McpC3	450	1907074	220gj	in071	1985	1:15840
Markland silt loam, 1 to 6 percent slopes, eroded	MaB2	332	964665	11ct7	in077	1982	1:15840
Markland silt loam, 8 to 15 percent slopes, eroded	MaC2	181	964666	11ct8	in077	1982	1:15840
Markland silt loam, 2 to 6 percent slopes, eroded	MbB2	235	164493	5j57	in083	1979	1:15840
Markland silty clay loam, 6 to 15 percent slopes, severely eroded, rarely flooded	MdvC3Q	680	1708141	1vbgb	in101	1984	1:15840
Markland silt loam, 12 to 18 percent slopes, eroded	MbD2	549	163222	5gv7	in109	1979	1:15840
Markland silt loam, 18 to 25 percent slopes	MbE	424	163223	5gv8	in109	1979	1:15840
Markland silty clay loam, 6 to 18 percent slopes, severely eroded	MbD3	233	1600556	1qqhv	in115	1979	1:15840
Markland silt loam, 2 to 12 percent slopes, eroded	MaB2	170	1600554	1qqhs	in115	1979	1:15840
Markland silt loam, 18 to 50 percent slopes, rarely flooded	McnGQ	1573	535820	kzkj	in123	1997	1:12000
Markland silty clay loam, 12 to 25 percent slopes, severely eroded, rarely flooded	McuDQ	1567	535822	kzkl	in123	1997	1:12000
Markland silty clay loam, 6 to 12 percent slopes, severely eroded	McpC3	1020	535821	kzkk	in123	1997	1:12000
Markland silt loam, 6 to 12 percent slopes, eroded	McgC2	367	535819	kzkh	in123	1997	1:12000
Markland silty clay loam, 6 to 15 percent slopes, severely eroded	MbC3	127	161920	5fh7	in125	1983	1:15840
Markland silty clay loam, 6 to 12 percent slopes, severely eroded	MlC3	1253	160035	5cjf	in147	1966	1:15840
Markland silt loam, 2 to 6 percent slopes, eroded	MkB2	1059	160030	5cj8	in147	1966	1:15840
Markland silty clay loam, 12 to 18 percent slopes, severely eroded	MlD3	678	160036	5cjg	in147	1966	1:15840
Markland silty clay loam, 2 to 6 percent slopes, severely eroded	MlB3	483	160034	5cjd	in147	1966	1:15840
Markland silt loam, 18 to 25 percent slopes	MkE	381	160033	5cjc	in147	1966	1:15840
Markland silt loam, 6 to 12 percent slopes, eroded	MkC2	342	160031	5cj9	in147	1966	1:15840
Markland silt loam, 12 to 18 percent slopes, eroded	MkD2	197	160032	5cjb	in147	1966	1:15840
Markland silt loam, 2 to 6 percent slopes, eroded	MaB2	570	162691	5g93	in153	1966	1:15840
Markland silty clay loam, 6 to 18 percent slopes, severely eroded	McD3	394	162694	5g96	in153	1966	1:15840
Markland silt loam, 18 to 25 percent slopes, eroded	MaE2	44	162693	5g95	in153	1966	1:15840
Markland silt loam, 12 to 18 percent slopes, eroded	MaD2	40	162692	5g94	in153	1966	1:15840
Markland silt loam, 8 to 15 percent slopes, eroded	MaC2	635	535281	kz04	in155	1984	1:15840
Markland silt loam, 1 to 6 percent slopes, eroded	MaB2	195	535280	kz03	in155	1984	1:15840
Markland silt loam, 2 to 6 percent slopes, eroded	MkB2	748	162754	5gc4	in163	1972	1:15840
Markland silty clay loam, 6 to 18 percent slopes, severely eroded	MlC3	557	162756	5gc6	in163	1972	1:15840
Markland silt loam, 6 to 18 percent slopes, eroded	MkC2	355	162755	5gc5	in163	1972	1:15840
Markland silt loam, 2 to 6 percent slopes, eroded	MkB2	1360	159960	5cg0	in173	1976	1:15840
Markland silty clay loam, 6 to 18 percent slopes, severely eroded	MoC3	1144	159962	5cg2	in173	1976	1:15840
Markland silt loam, 6 to 18 percent slopes	MkC	326	159961	5cg1	in173	1976	1:15840
Markland silt loam, 2 to 8 percent slopes	MaB	425	535493	kz6z	in175	1984	1:15840
Markland silt loam, 2 to 6 percent slopes	MdB	193	549204	2wv60	ky101	1964	1:15840
Markland silt loam, 12 to 35 percent slopes, rarely flooded	MkE	180	549208	2zs54	ky101	1964	1:15840
Markland silty clay loam, 2 to 6 percent slopes, eroded	MhB2	154	549206	2wv5y	ky101	1964	1:15840
Markland silty clay, 6 to 12 percent slopes, severely eroded	MeC3	132	549205	2wv5x	ky101	1964	1:15840
Markland silty clay loam, 6 to 12 percent slopes, eroded	MhC2	110	549207	2wv5z	ky101	1964	1:15840
Markland silt loam, 12 to 35 percent slopes, rarely flooded	MkE	775	549280	2zs54	ky107	1974	1:12000
Markland silty clay, 6 to 12 percent slopes, severely eroded	MbC3	479	549281	2wv5x	ky107	1974	1:12000
Markland silty clay, 6 to 12 percent slopes, severely eroded	MlC3	455	549980	lg99	ky179	1967	1:15840
Markland silt loam, 2 to 12 percent slopes	MkC	225	549978	lg97	ky179	1967	1:15840
Markland silty clay, 12 to 20 percent slopes, severely eroded	MlD3	195	549981	lg9b	ky179	1967	1:15840
Markland silt loam, 12 to 20 percent slopes, eroded	MkD2	170	549979	lg98	ky179	1967	1:15840
Licking silty clay, 12 to 20 percent slopes, severely eroded (markland)	LmD3	1708	552052	ljg4	ky603	1968	1:15840
Markland silt loam, 2 to 6 percent slopes	MkB	1470	550406	lgr1	ky605	1975	1:20000
Markland soils, 12 to 30 percent slopes	MlD	876	550408	lgr3	ky605	1975	1:20000
Markland soils, 6 to 12 percent slopes	MlC	624	550407	lgr2	ky605	1975	1:20000
Markland silty clay loam, 12 to 35 percent slopes, severely eroded	MaD3	1046	549598	lfwz	ky607	1992	1:20000
Markland silty clay loam, 6 to 12 percent slopes, severely eroded	MaC3	620	549597	lfwy	ky607	1992	1:20000
Markland silty clay, occasionally flooded, 10 to 30 percent slopes, severely eroded	MbD3	7494	551000	lhc6	ky608	1983	1:20000
Markland silt loam, rarely flooded, 2 to 6 percent slopes	MaB	513	550999	lhc5	ky608	1983	1:20000
Markland soils, 12 to 35 percent slopes	MbD	3293	552000	ljdg	ky612	1972	1:15840
Markland silt loam, 2 to 6 percent slopes	MaB	965	551999	ljdf	ky612	1972	1:15840
Markland silty clay, 6 to 12 percent slopes, severely eroded	MfC3	406	549405	2wv5x	ky615	1971	1:20000
Markland silt loam, 12 to 30 percent slopes	MdE	383	549403	lfpp	ky615	1971	1:20000
Markland silty clay loam, 2 to 6 percent slopes, eroded	MeB2	266	549404	2wv5y	ky615	1971	1:20000
Markland silt loam, 0 to 2 percent slopes	MdA	193	549402	lfpn	ky615	1971	1:20000
Markland silty clay, 12 to 30 percent slopes, severely eroded	MfE3	172	549406	lfps	ky615	1971	1:20000
Markland silty clay, 6 to 12 percent slopes, severely eroded	MdC3	3205	551050	lhdt	ky621	1975	1:20000
Markland silt loam, 12 to 35 percent slopes, rarely flooded	MkE	680	551113	2zs54	ky631	1976	1:20000
Markland silty clay loam, 6 to 12 percent slopes	MaC	2019	549515	lft9	ky635	1978	1:20000
Markland silt loam, 12 to 35 percent slopes, rarely flooded	MkE	1070	549516	2zs54	ky635	1978	1:20000
Markland silty clay loam, 2 to 6 percent slopes	MaB	13	1721614	1vsgy	oh017	1977	1:15840
Markland-Urban land complex, 2 to 6 percent slopes	MaUB	7	3381104	30tqb	oh017	1977	1:15840
Markland silt loam, 2 to 6 percent slopes	MdB	67	168802	5nn7	oh025	1972	1:20000
Markland silt loam, 15 to 35 percent slopes, eroded	MaD2	599	536666	l0ft	oh031	1996	1:15840
Markland silt loam, 6 to 15 percent slopes	MaC	104	536665	l0fs	oh031	1996	1:15840
Markland silt loam, 2 to 6 percent slopes	MaB	55	536664	l0fr	oh031	1996	1:15840
Markland-Glenford complex, 15 to 35 percent slopes, eroded	McD2	30	2108962	28sk1	oh031	1996	1:15840
Markland silty clay loam, 2 to 6 percent slopes	MaB	539	169407	5p8r	oh061	1980	1:15840
Urban land-Alfic Udarents-Markland complex, 0 to 12 percent slopes	UAMXC	330	2652883	2pyyw	oh061	1980	1:15840
Markland silty clay loam, 18 to 25 percent slopes, eroded	MaE2	251	169410	5p8v	oh061	1980	1:15840
Markland silty clay loam, 6 to 12 percent slopes, eroded	MaC2	199	169408	5p8s	oh061	1980	1:15840
Markland silty clay loam, 12 to 18 percent slopes, eroded	MaD2	86	169409	5p8t	oh061	1980	1:15840
Markland silt loam, 6 to 12 percent slopes, moderately eroded	MdC2	306	1420461	1jp3b	oh071	1973	1:15840
Markland silt loam, 2 to 6 percent slopes	MdB	138	1420460	1jp39	oh071	1973	1:15840
Markland silt loam, 12 to 18 percent slopes, moderately eroded	MdD2	129	1420462	1jp3c	oh071	1973	1:15840
Markland silty clay loam, 12 to 25 percent slopes, eroded	MaD2	129	537447	l180	oh115	1992	1:15840
Markland-Glenford complex, 15 to 35 percent slopes, eroded	McD2	2383	537915	l1r3	oh119	1989	1:15840
Markland silty clay loam, 6 to 15 percent slopes, eroded	MbC2	1388	537914	l1r2	oh119	1989	1:15840
Markland silt loam, 2 to 6 percent slopes	MaB	1342	537913	l1r1	oh119	1989	1:15840
Markland silty clay loam, 15 to 25 percent slopes, eroded	MaD2	816	537660	l1gw	oh131	1984	1:15840
Markland silty clay loam, 3 to 8 percent slopes, eroded	MaB2	780	537658	l1gt	oh131	1984	1:15840
Markland silty clay loam, 8 to 15 percent slopes, eroded	MaC2	732	537659	l1gv	oh131	1984	1:15840
Markland silt loam, 6 to 12 percent slopes, moderately eroded	McC2	75	1689024	1tpkn	oh131	1984	1:15840
Markland silty clay loam, 12 to 20 percent slopes, eroded	MbD2	20	1689006	1tpk2	oh131	1984	1:15840
Markland silt loam, 2 to 6 percent slopes	McB	10	1689023	1tpkm	oh131	1984	1:15840
Markland silty clay loam, 6 to 12 percent slopes, eroded	MbC2	4	1689005	1tpk1	oh131	1984	1:15840
Markland silt loam, 12 to 18 percent slopes, moderately eroded	McD2	1	1689025	1tpkp	oh131	1984	1:15840
Markland silty clay loam, 6 to 12 percent slopes, eroded	MbC2	438	170902	5qtz	oh141	1997	1:15840
Markland silty clay loam, 12 to 20 percent slopes, eroded	MbD2	311	170903	5qv0	oh141	1997	1:15840
Markland silty clay loam, 20 to 35 percent slopes, eroded	MbE2	244	170904	5qv1	oh141	1997	1:15840
Markland silt loam, 2 to 6 percent slopes	MaB	168	170901	5qty	oh141	1997	1:15840
Markland silt loam, 2 to 6 percent slopes	MbB	1143	536525	l098	oh167	1973	1:15840
Markland silt loam, 18 to 50 percent slopes	MbG	476	536528	l09c	oh167	1973	1:15840
Markland silt loam, 6 to 12 percent slopes	MbC	372	536526	l099	oh167	1973	1:15840
Markland silt loam, 12 to 18 percent slopes, moderately eroded	MbD2	295	536527	l09b	oh167	1973	1:15840
Markland silt loam, 8 to 15 percent slopes	MaC	710	513672	k7j2	wv011	1984	1:20000
Markland silt loam, 3 to 8 percent slopes	MaB	200	513671	k7j1	wv011	1984	1:20000
Markland silt loam, 8 to 15 percent slopes	MaC	360	515029	k8xv	wv099	1993	1:24000
Markland silt loam, 3 to 8 percent slopes	MaB	180	515028	k8xt	wv099	1993	1:24000
Markland silt loam, 3 to 10 percent slopes	MdB	1668	514609	k8h9	wv601	1966	1:15840
Markland silt loam, 10 to 20 percent slopes	MdC	648	514610	k8hb	wv601	1966	1:15840
Markland silty clay loam, 10 to 20 percent slopes, severely eroded	MeC3	563	514612	k8hd	wv601	1966	1:15840
Markland silty clay loam, 20 to 30 percent slopes, severely eroded	MeD3	476	514613	k8hf	wv601	1966	1:15840
Markland silty clay loam, 30 to 40 percent slopes, severely eroded	MeE3	317	514614	k8hg	wv601	1966	1:15840
Markland silt loam, 30 to 40 percent slopes	MdE	251	514611	k8hc	wv601	1966	1:15840

Map of Series Extent

Approximate geographic distribution of the MARKLAND 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).