Soil Data Explorer - GRAYLING

Official Series Description

Lab Data Summary

Aggregate lab data for the GRAYLING soil series. This aggregation is based on all pedons with a current taxon name of GRAYLING, 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 GRAYLING 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
93A	UMN2961	S1979MN137062 (2961)	Grayling	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.7748604,-92.5544815
94A	94P0184	S1993MI069006	Grayling	n/a	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.3233299,-83.3837585
94B	40A1922	S1966MI041001	Grayling	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.8994408,-86.9227676
94C	40A1921	S1966MI031001	Grayling	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.3899972,-84.5358222

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GRAYLING 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 GRAYLING 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 GRAYLING 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 GRAYLING 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 GRAYLING 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 GRAYLING 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 GRAYLING 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 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 GRAYLING, 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. MI-2010-09-07-23 | Montmorency County - 2003

   Typical pattern of soils and underlying material in the Rubicon-Grayling-Tawas and Millersburg-Klacking-Horsehead associations (Soil Survey of Montmorency County, Michigan; 2003).

2. MI-2012-02-06-03 | Alcona County - 1998

   Typical pattern of soils and parent material in the McGinn-Hoist-Klacking, Grayling-Graycalm-Typic Udipsamments, and Glennie-Bamfield-Lupton associations (Soil Survey of Alcona County, Michigan; 1998).

3. MI-2012-02-06-07 | Cheboygan County - September 1991

   Typical pattern of soils and parent material in the Grayling-Rubicon and Cheboygan-Blue Lake associations (Soil Survey of Cheboygan County, Michigan; September 1991).

4. MI-2012-02-06-40 | Menominee County - September 1989

   Typical pattern of soils and parent material in the Pemene-Grayling-Lupton map unit (Soil Survey of Menominee County, Michigan; September 1989).

5. MI-2012-03-22-01 | Cheboygan County - September 1991

   Typical pattern of soils and parent material in the Grayling-Rubicon and Cheboygan-Blue Lake associations (Soil Survey of Cheboygan County, MI; 1991).

Map Units

Map units containing GRAYLING 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
Grayling sand, calcareous substratum, nearly level and undulating	209B	10892	190251	6cz4	mi001	1993	1:20000
Grayling sand, banded substratum, nearly level and undulating	211B	5586	190255	6cz8	mi001	1993	1:20000
Grayling sand, nearly level and undulating	210B	4955	190252	6cz5	mi001	1993	1:20000
Graycalm-Grayling sands, rolling	223C	4453	190270	6czr	mi001	1993	1:20000
Graycalm-Grayling sands, nearly level and undulating	223B	3469	190269	6czq	mi001	1993	1:20000
Grayling sand, 0 to 6 percent slopes	81B	2653	190367	6d2w	mi001	1993	1:20000
Grayling sand, rolling	210C	1694	190253	6cz6	mi001	1993	1:20000
Grayling sand, banded substratum, rolling	211C	953	190256	6cz9	mi001	1993	1:20000
Grayling sand, very deep water table, nearly level and undulating	212B	743	190257	6czb	mi001	1993	1:20000
Grayling sand, 18 to 35 percent slopes	81E	583	190369	6d2y	mi001	1993	1:20000
Grayling sand, hilly	210D	474	190254	6cz7	mi001	1993	1:20000
Grayling sand, 6 to 12 percent slopes	81C	368	190368	6d2x	mi001	1993	1:20000
Graycalm-Grayling sands, hilly	223D	187	190271	6czs	mi001	1993	1:20000
Grayling sand, very deep water table, 0 to 6 percent slopes	373B	1153	191277	6f17	mi007	1998	1:12000
Grayling association	Gr	11018	189167	6bv5	mi011	1964	1:20000
Grayling sand, 1 to 6 percent slopes	8250B	8402	2450716	2n85c	mi013	1984	1:20000
Grayling sand, 6 to 18 percent slopes	8250C	2943	2450717	2n85d	mi013	1984	1:20000
Grayling-Kinross complex, 0 to 15 percent slopes	29D	1218	414965	fxsz	mi013	1984	1:20000
Grayling sand, 0 to 8 percent slopes	12B	8717	190524	6d7y	mi031	1988	1:15840
Grayling sand, 0 to 6 percent slopes	GyB	29475	189617	2v14v	mi035	1977	1:15840
Grayling sand, 6 to 18 percent slopes	GyC	3171	189618	6c9q	mi035	1977	1:15840
Grayling sand, 18 to 35 percent slopes	GyD	551	189619	6c9r	mi035	1977	1:15840
Grayling sand, 0 to 6 percent slopes	81B	73813	189733	2v14v	mi039	1993	1:15840
Grayling sand, 6 to 18 percent slopes	81D	12499	189734	6cfg	mi039	1993	1:15840
Grayling sand, nearly level and undulating	210B	4683	189667	6cc9	mi039	1993	1:15840
Grayling sand, 18 to 45 percent slopes	81F	4035	189735	6cfh	mi039	1993	1:15840
Grayling sand, very deep water table, nearly level and undulating	212B	3117	189675	6cck	mi039	1993	1:15840
Graycalm-Grayling sands, hilly	223D	2770	189691	6cd2	mi039	1993	1:15840
Graycalm-Grayling sands, rolling	223C	1837	189690	6cd1	mi039	1993	1:15840
Grayling sand, rolling	210C	1668	189668	6ccb	mi039	1993	1:15840
Graycalm-Grayling sands, nearly level and undulating	223B	1365	189689	6cd0	mi039	1993	1:15840
Grayling sand, banded substratum, nearly level and undulating	211B	1229	189671	6ccf	mi039	1993	1:15840
Grayling sand, hilly	210D	1060	189669	6ccc	mi039	1993	1:15840
Grayling sand, steep	210E	811	189670	6ccd	mi039	1993	1:15840
Grayling sand, banded substratum, steep	211E	530	189674	6ccj	mi039	1993	1:15840
Grayling sand, banded substratum, rolling	211C	259	189672	6ccg	mi039	1993	1:15840
Grayling sand, banded substratum, hilly	211D	127	189673	6cch	mi039	1993	1:15840
Grayling sand, 0 to 6 percent slopes	GrB	6385	1588057	1q9hn	mi041	1969	1:24000
Grayling sand, 6 to 18 percent slopes	GrD	366	1588058	1q9hp	mi041	1969	1:24000
Grayling-Covert-Pipestone association	GW	4026	2673492	2qz5y	mi051	1966	1:15840
Grayling association, undulating	GSB	2444	189784	6ch2	mi051	1966	1:15840
Grayling association, rolling	GSC	885	189785	6ch3	mi051	1966	1:15840
Grayling-Croswell-Au Gres association	GU	663	189786	6ch4	mi051	1966	1:15840
Grayling sand, 0 to 6 percent slopes	GrB	505	196661	6lmx	mi051	1966	1:15840
Grayling sand, 0 to 6 percent slopes	GuB	321	189442	2v14v	mi055	1963	1:15840
Grayling sand, calcareous substratum, nearly level and undulating	209B	38636	191731	6fhw	mi069	1995	1:15840
Grayling sand, 0 to 6 percent slopes	81B	15864	191951	6fqz	mi069	1995	1:15840
Grayling sand, very deep water table, nearly level and undulating	212B	12426	191743	6fj8	mi069	1995	1:15840
Grayling sand, nearly level and undulating	210B	5407	191734	6fhz	mi069	1995	1:15840
Grayling sand, calcareous substratum, rolling	209C	4255	191732	6fhx	mi069	1995	1:15840
Grayling sand, 6 to 18 percent slopes	81D	2687	191953	6fr1	mi069	1995	1:15840
Grayling sand, rolling	210C	2321	191735	6fj0	mi069	1995	1:15840
Grayling sand, hilly	210D	1599	191736	6fj1	mi069	1995	1:15840
Grayling sand, banded substratum, nearly level and undulating	211B	1340	191738	6fj3	mi069	1995	1:15840
Grayling sand, 18 to 35 percent slopes	81E	1033	191954	6fr2	mi069	1995	1:15840
Graycalm-Grayling sands, nearly level and undulating	223B	945	191762	6fjw	mi069	1995	1:15840
Grayling sand, calcareous substratum, hilly	209D	857	191733	6fhy	mi069	1995	1:15840
Grayling sand, steep	210E	831	191737	6fj2	mi069	1995	1:15840
Graycalm-Grayling sands, rolling	223C	262	191763	6fjx	mi069	1995	1:15840
Graycalm-Grayling sands, steep	223E	126	191765	6fjz	mi069	1995	1:15840
Graycalm-Grayling sands, hilly	223D	105	191764	6fjy	mi069	1995	1:15840
Grayling sand, 0 to 6 percent slopes	81B	9185	190671	2v14v	mi079	1998	1:12000
Grayling sand, 6 to 18 percent slopes	81D	2329	190672	6ddq	mi079	1998	1:12000
Grayling sand, 18 to 35 percent slopes	81E	1348	190673	6ddr	mi079	1998	1:12000
Grayling sand, 18 to 45 percent slopes	81F	35	643102	pl67	mi079	1998	1:12000
Grayling sand, 0 to 6 percent slopes	10B	22308	394972	f801	mi103	1999	1:24000
Grayling sand, 6 to 18 percent slopes	10D	3119	394973	f802	mi103	1999	1:24000
Grayling sand, 0 to 4 percent slopes, rocky	111B	945	394978	f807	mi103	1999	1:24000
Grayling sand, 18 to 35 percent slopes	10E	630	394974	f803	mi103	1999	1:24000
Grayling sand, 3 to 12 percent slopes	50B	4534	415484	fybq	mi109	1985	1:20000
Grayling sand, 0 to 6 percent slopes	19B	3633	192422	2v14v	mi113	1983	1:15840
Grayling sand, 0 to 6 percent slopes	81B	31135	192337	2v14v	mi119	1997	1:12000
Grayling sand, 6 to 18 percent slopes	81D	4178	192338	6g4g	mi119	1997	1:12000
Grayling sand, 18 to 35 percent slopes	81E	1023	192339	6g4h	mi119	1997	1:12000
Grayling sand, 0 to 6 percent slopes	10B	11825	189867	2v14v	mi129	1987	1:15840
Grayling sand, 6 to 18 percent slopes	10C	2020	189868	6cks	mi129	1987	1:15840
Grayling sand, 18 to 35 percent slopes	10E	258	189869	6ckt	mi129	1987	1:15840
Grayling sand, 0 to 6 percent slopes	GrB	2845	190033	2v14v	mi133	1966	1:15840
Grayling sand, 18 to 25 percent slopes	GrE	113	190035	6cr5	mi133	1966	1:15840
Grayling, banded substratum-Graycalm sands, nearly level and undulating	211B	22651	241399	8362	mi135	2003	1:12000
Grayling sand, 0 to 6 percent slopes	81B	15611	241409	2v14v	mi135	2003	1:12000
Grayling, banded substratum-Graycalm sands, rolling	211C	14670	241430	8372	mi135	2003	1:12000
Grayling sand, nearly level and undulating	210B	10212	241396	835z	mi135	2003	1:12000
Grayling, banded substratum-Graycalm sands, hilly	211D	6001	241466	8387	mi135	2003	1:12000
Grayling sand, steep	210E	5874	241400	8363	mi135	2003	1:12000
Grayling sand, rolling	210C	5842	241397	8360	mi135	2003	1:12000
Grayling, banded substratum-Graycalm sands, steep	211E	4941	241467	8388	mi135	2003	1:12000
Grayling sand, very deep water table, nearly level and undulating	212B	4198	241431	8373	mi135	2003	1:12000
Grayling sand, hilly	210D	3953	241398	8361	mi135	2003	1:12000
Graycalm-Grayling sands, nearly level and undulating	223B	1759	241403	8366	mi135	2003	1:12000
Gerrish-Grayling sands, 0 to 6 percent slopes	496B	1731	209071	70k7	mi135	2003	1:12000
Graycalm-Grayling sands, hilly	223D	1624	241404	8367	mi135	2003	1:12000
Graycalm-Grayling sands, rolling	223C	1553	241405	8368	mi135	2003	1:12000
Grayling sand, 6 to 18 percent slopes	81D	906	241394	835x	mi135	2003	1:12000
Graycalm-Grayling sands, steep	223E	608	197597	6mm3	mi135	2003	1:12000
Grayling sand, 18 to 35 percent slopes	81E	540	241415	836l	mi135	2003	1:12000
Grayling sand, 18 to 45 percent slopes	81F	52	241395	835y	mi135	2003	1:12000
Grayling sand, 0 to 6 percent slopes	81B	4089	191520	2v14v	mi137	1998	1:12000
Grayling sand, 6 to 18 percent slopes	81D	1116	191521	6f93	mi137	1998	1:12000
Grayling sand, 18 to 45 percent slopes	81F	362	191522	6f94	mi137	1998	1:12000
Grayling sand, 18 to 35 percent slopes	81E	82	191552	6fb3	mi137	1998	1:12000
Grayling sand, 0 to 6 percent slopes	39B	3217	190888	2v14v	mi141	1989	1:15840
Grayling sand, 8 to 15 percent slopes	39C	676	190889	6dmq	mi141	1989	1:15840
Grayling sand, 0 to 6 percent slopes	81B	27469	190989	2v14v	mi143	1999	1:12000
Grayling sand, 6 to 18 percent slopes	81D	6091	190990	6dqz	mi143	1999	1:12000
Grayling sand, 18 to 45 percent slopes	81F	2596	191004	6drf	mi143	1999	1:12000
Gerrish-Grayling sands, 0 to 6 percent slopes	496B	2186	191051	6dsy	mi143	1999	1:12000
Gerrish-Grayling sands, 6 to 18 percent slopes	496D	250	191052	6dsz	mi143	1999	1:12000
Gerrish-Grayling sands, 18 to 45 percent slopes	496F	105	191053	6dt0	mi143	1999	1:12000
Grayling-Cromwell complex, 0 to 3 percent slopes	F120A	8	2943745	1hkk6	mn031	2013	1:24000
Graycalm-Grayling complex, 12 to 25 percent slopes	D77D	6008	2732652	2ndr1	mn035	2009	1:24000
Graycalm-Grayling complex, 2 to 15 percent slopes	D77C	4608	2732650	2ndqv	mn035	2009	1:24000
Graycalm-Grayling-Meehan complex, 1 to 8 percent slopes	D78B	3686	2732651	2ndqw	mn035	2009	1:24000
Graycalm-Grayling complex, 25 to 45 percent slopes	D77F	2176	2732653	2ndr2	mn035	2009	1:24000
Graycalm-Grayling complex, pitted, 2 to 15 percent slopes	D76C	1845	2732649	2ndqn	mn035	2009	1:24000
Graycalm-Grayling-Rifle complex, 0 to 25 percent slopes	D80D	1741	2732656	2ndr5	mn035	2009	1:24000
Graycalm-Grayling complex, pitted, 2 to 20 percent slopes	D76D	1726	2732699	2slny	mn035	2009	1:24000
Graycalm-Grayling-Water complex, 0 to 25 percent slopes	D82D	1288	2732660	2ndrk	mn035	2009	1:24000
Graycalm-Grayling complex, 2 to 8 percent slopes	C112B	2007	1673535	1t5g0	mn065	2006	1:12000
Graycalm-Grayling complex, 8 to 15 percent slopes	C112C	675	1673536	1t5g1	mn065	2006	1:12000
Graycalm-Grayling complex, 0 to 2 percent slopes	C112A	638	1673534	1t5fz	mn065	2006	1:12000
Graycalm-Grayling complex, 15 to 30 percent slopes	C112E	322	1673537	1t5g2	mn065	2006	1:12000
Grayling-Grytal-Cromwell complex, 0 to 8 percent slopes, pitted	F4-20D	41	2742227	2rn2d	mn075	2013	1:24000
Graycalm-Grayling complex, 8 to 15 percent slopes	C112C	154	1676437	1t8gm	mn095	2006	1:12000
Graycalm-Grayling complex, 2 to 8 percent slopes	C112B	153	1676436	1t8gl	mn095	2006	1:12000
Graycalm-Grayling complex, 15 to 30 percent slopes	C112E	94	1676438	1t8gn	mn095	2006	1:12000
Grayling sand, 0 to 7 percent slopes	C153	6493	2484665	2pdhh	mn115	2009	1:24000
Grayling sand, 0 to 3 percent slopes	C152	5323	2484664	2pdhg	mn115	2009	1:24000
Grayling sand, 2 to 17 percent slopes	C154	1917	2484666	2pdhj	mn115	2009	1:24000
Grayling sand, 17 to 35 percent slopes	C155	1217	2484667	2pdhk	mn115	2009	1:24000
Grayling-Cromwell complex, 2 to 8 percent slopes	F120B	1498	449624	h2w0	mn615	2007	1:24000
Grayling-Grytal-Cromwell complex, pitted, 0 to 8 percent slopes	F123B	1495	1387291	1hklb	mn615	2007	1:24000
Grayling-Grytal-Cromwell complex, pitted, 0 to 18 percent slopes	F123D	1288	1424732	1jtk3	mn615	2007	1:24000
Grayling-Cromwell complex, 8 to 18 percent slopes	F120D	1015	1424909	1jtqt	mn615	2007	1:24000
Grayling-Cromwell complex, 18 to 45 percent slopes	F120F	267	1424908	1jtqs	mn615	2007	1:24000
Grayling-Cromwell complex, 0 to 3 percent slopes	F120A	265	1387256	1hkk6	mn615	2007	1:24000
Graycalm-Grayling complex, 1 to 8 percent slopes	B13B	1351	1861802	20hc4	mn617	2007	1:24000
Grayling-Cromwell complex, 2 to 8 percent slopes	F120B	1903	1715828	1vlg9	mn619	2009	1:24000
Grayling-Grytal-Cromwell complex, pitted, 0 to 8 percent slopes	F123B	1631	1715838	1vlgm	mn619	2009	1:24000
Grayling-Grytal-Cromwell complex, pitted, 0 to 18 percent slopes	F123D	905	1715839	1vlgn	mn619	2009	1:24000
Grayling-Cromwell complex, 18 to 45 percent slopes	F120F	722	1715830	1vlgc	mn619	2009	1:24000
Grayling-Cromwell complex, 0 to 3 percent slopes	F120A	721	1715827	1vlg8	mn619	2009	1:24000
Grayling-Cromwell complex, 8 to 18 percent slopes	F120D	688	1715829	1vlgb	mn619	2009	1:24000
Graycalm-Grayling-Leander complex, pitted, 0 to 18 percent slopes	A2D	1327	822891	wm8w	mn621	2006	1:24000
Graycalm-Grayling-Leander complex, pitted, 0 to 45 percent slopes	A2E	1210	822892	wm8x	mn621	2006	1:24000
Grayling sand, beaches, 2 to 12 percent slopes	599C	203	1444587	1kh6l	wi003	2006	1:12000
Grayling sand, 0 to 6 percent slopes	399B	46333	448344	h1jq	wi013	2004	1:12000
Friendship-Wurtsmith-Grayling complex, 0 to 6 percent slopes	396B	20879	448340	h1jl	wi013	2004	1:12000
Grayling sand, 6 to 12 percent slopes	399C	17053	448345	h1jr	wi013	2004	1:12000
Grayling sand, 12 to 30 percent slopes	399D	11568	448346	h1js	wi013	2004	1:12000
Grayling sand, 0 to 6 percent slopes	399B	10596	781215	v6xh	wi031	2005	1:12000
Grayling sand, 6 to 12 percent slopes	399C	4499	781216	v6xj	wi031	2005	1:12000
Grayling sand, 12 to 30 percent slopes	399D	3537	781217	v6xk	wi031	2005	1:12000
Friendship-Wurtsmith-Grayling complex, 0 to 6 percent slopes	396B	423	781213	v6xf	wi031	2005	1:12000
Grayling loamy sand, 0 to 6 percent slopes	GaB	8106	395795	f8vl	wi078	1998	1:12000
Grayling loamy sand, 6 to 15 percent slopes	GaC	5984	395883	f8yf	wi078	1998	1:12000
Grayling sand, 0 to 6 percent slopes	GyB	5508	395884	f8yg	wi078	1998	1:12000
Grayling loamy sand, 15 to 35 percent slopes	GaD	3374	395882	f8yd	wi078	1998	1:12000
Grayling sand, 6 to 15 percent slopes	GyC	1950	395886	f8yj	wi078	1998	1:12000
Grayling sand, 15 to 35 percent slopes	GyD	393	395885	f8yh	wi078	1998	1:12000
Grayling sand, 0 to 6 percent slopes	399B	9343	2427709	2mh76	wi095	1978	1:15840
Grayling sand, 6 to 12 percent slopes	399C	5714	2427712	2mh79	wi095	1978	1:15840
Grayling sand, 12 to 30 percent slopes	399D	2203	2427714	2mh7c	wi095	1978	1:15840
Grayling-Trade River-Seep complex, 20 to 80 percent slopes	8F	229	2427721	2mh7l	wi095	1978	1:15840
Friendship-Wurtsmith-Grayling complex, 0 to 6 percent slopes	396B	178	2427686	2mh6g	wi095	1978	1:15840
Grayling sand, 0 to 6 percent slopes	399B	11158	435509	gm5p	wi129	2002	1:12000
Grayling sand, 12 to 30 percent slopes	399D	8353	435511	gm5r	wi129	2002	1:12000
Grayling sand, 6 to 12 percent slopes	399C	7674	435510	gm5q	wi129	2002	1:12000
Friendship-Wurtsmith-Grayling complex, 0 to 6 percent slopes	396B	216	435507	gm5m	wi129	2002	1:12000

Map of Series Extent

Approximate geographic distribution of the GRAYLING 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).