Soil Data Explorer - QUINLAN

Official Series Description

Lab Data Summary

Aggregate lab data for the QUINLAN soil series. This aggregation is based on all pedons with a current taxon name of QUINLAN, 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 QUINLAN 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
78C	75-OK-75-3	75-OK015-75-3	Quinlan	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.2575444,-98.6223361
78C	94P0719	94OK059012	Quinlan	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.690834,-99.4880524
78C	87P0437	S1987OK153002	Quinlan	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.4215317,-99.4193115

Water Balance

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with QUINLAN 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 QUINLAN 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the QUINLAN 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 2D hillslope position figure.

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 QUINLAN, 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. KS-2012-01-20-24 | Clark County - December 1982

   Typical pattern of soils in the Carey-Woodward-Quinlan association (Soil Survey of Clark County, Kansas; 1982).

2. KS-2012-01-20-37 | Comanche County - June 1989

   Typical pattern of soils and parent material in the Quinlan-Woodward-Carey association (Soil Survey of Comanche County, Kansas; 1989).

3. KS-2012-01-20-38 | Comanche County - June 1989

   Typical pattern of soils and parent material in the Obaro-Abilen association (Soil Survey of Comanche County, Kansas; 1989).

4. OK-2010-09-29-20 | Woods County - 2003

   Typical pattern of soils and underlying material in the Quinlan-Woodward-Deepwood general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

5. OK-2012-02-16-25 | Dewey County - December 1963

   Typical pattern of the dominant soils in association 3 (Soil Survey of Dewey County, Oklahoma; December 1963).

6. OK-2012-02-16-26 | Dewey County - December 1963

   Typical pattern of the soils in association 4 (Soil Survey of Dewey County, Oklahoma; December 1963).

7. OK-2012-02-16-28 | Ellis County - April 1966

   Major soils of associations 1, 2, 3, and 11 (Soil Survey of Ellis County, Oklahoma; April 1966).

8. OK-2012-02-16-36 | Greer County - March 1967

   Major soils in soil association 2, and their relation to the landscape (Soil Survey of Greer County, Oklahoma; March 1967).

9. OK-2012-02-16-39 | Harmon County - September 1984

   Typical pattern of soils and underlying material in the Woodward-Quinlan map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

10. OK-2012-02-16-40 | Harmon County - September 1984

    Typical pattern of soils and underlying material in the Madge-Abilene-Shrewder map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

11. OK-2012-02-16-45 | Harper County - June 1960

    A schematic drawing showing a normal pattern of soils formed over Permian redbeds. The typical slope range is given for each soil. Alternating layers of sandstone and shale underlie these soils (Soil Survey of Harper County, Oklahoma; June 1960).

12. OK-2012-02-17-41 | Roger Mills County - August 1963

    Typical pattern of soils in associations 6, 7, and 9 (Soil Survey of Roger Mills County, Oklahoma; August 1963).

13. OK-2012-02-17-58 | Woodward County - November 1963

    Typical pattern of soils of the St. Paul-Carey-Woodward association (Soil Survey of Woodward County, Oklahoma; November 1963).

14. TX-2010-11-02-22 | Carson County -

    General relationship of the soils in Carson County (Soil Survey of Carson County, Texas).

15. TX-2010-11-03-73 | Lynn County - 2008

    Pattern of soils and underlying materials in the Potter-Obaro-Quinlan general soil map unit (Soil Survey of Lynn County, Texas; 2008).

16. TX-2012-03-20-17 | Childress County - July 1963

    Soils developed in sandstone material (Soil Survey of Childress County, TX; 1963).

17. TX-2012-03-21-87 | Stonewall County - January 1975

    Paducah-Obaro soil association (Soil Survey of Stonewall County, TX; 1975).

18. TX-2012-03-21-88 | Stonewall County - January 1975

    Quinlan-Woodward soil association (Soil Survey of Stonewall County, TX; 1975).

Map Units

Map units containing QUINLAN 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
Quinlan-Woodward loams, 6 to 15 percent slopes	5457	63888	1382519	2t6qp	ks007	1973	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	5496	32385	1382535	2w5qn	ks007	1973	1:24000
Quinlan-Clairemont complex, 0 to 50 percent slopes	5451	10004	1382517	1hdmb	ks007	1973	1:24000
Woodward-Quinlan loams, 1 to 3 percent slopes	5495	5449	1382534	2w5qp	ks007	1973	1:24000
Quinlan loam, 1 to 3 percent slopes MLRA 78C	5443	3548	1382515	2t6pw	ks007	1973	1:24000
Quinlan-Woodward loams, 15 to 30 percent slopes	5458	528	1382518	2t6qm	ks007	1973	1:24000
Quinlan loam, 3 to 6 percent slopes	5444	8	1382516	1hdm9	ks007	1973	1:24000
Quinlan-Woodward loams, 6 to 15 percent slopes	5457	42260	1381739	2t6qp	ks025	1980	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	5496	19869	1381757	2w5qn	ks025	1980	1:24000
Likes-Quinlan complex, 3 to 15 percent slopes	5244	7139	1381722	1hcsp	ks025	1980	1:24000
Quinlan-Woodward loams, 6 to 15 percent slopes	5457	49124	1381286	2t6qp	ks033	1987	1:24000
Quinlan-Woodward loams, 15 to 30 percent slopes	5458	17421	1381285	2t6qm	ks033	1987	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	5496	14832	1381300	2w5qn	ks033	1987	1:24000
Woodward-Quinlan loams, 1 to 3 percent slopes	5495	15486	1382753	1hdvy	ks077	1965	1:24000
Woodward-Quinlan loams, 0 to 1 percent slopes	5494	5443	1382752	1hdvx	ks077	1965	1:24000
Quinlan loam, 3 to 6 percent slopes	5444	3214	1382728	1hdv4	ks077	1965	1:24000
Quinlan loam, 0 to 1 percent slopes	5442	2915	1382726	1hdv2	ks077	1965	1:24000
Quinlan loam, 1 to 3 percent slopes	5443	2175	1382727	1hdv3	ks077	1965	1:24000
Woodward-Quinlan loams, 3 to 6 percent slopes	5496	593	1382754	1hdvz	ks077	1965	1:24000
Nashville-Quinlan complex, 6 to 15 percent slopes	6394	175	1382716	30yqw	ks077	1965	1:24000
Nashville-Quinlan complex, 6 to 15 percent slopes	6394	15386	1444832	30yqw	ks095	1977	1:24000
Quinlan loam, 3 to 6 percent slopes	5444	7120	1444752	1khcx	ks095	1977	1:24000
Quinlan loam, 1 to 3 percent slopes	5443	5552	1444751	1khcw	ks095	1977	1:24000
Quinlan-Woodward loams, 6 to 15 percent slopes	5457	4058	1380540	1hbkk	ks097	1983	1:24000
Quinlan-Woodward complex, 5 to 30 percent slopes	QwE	13869	381440	dsxj	ok003	1971	1:24000
Woodward-Quinlan complex, 1 to 3 percent slopes	WuB	10199	381449	dsxt	ok003	1971	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes	QwC	9380	381439	dsxh	ok003	1971	1:24000
Woodward-Quinlan-Burson complex, 3 to 5 percent slopes, eroded	WQBC2	45	622546	2w5qq	ok003	1971	1:24000
Quinlan-Rock outcrop-Yomont frequently flooded complex, 0 to 45 percent slopes	QRYG	1753	3203441	2zc1c	ok007	2021	1:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopes	QWDE	427	3101276	2t6qr	ok007	2021	1:24000
Westola occasionally flooded-Quinlan-Hardeman complex, 0 to 12 percent slopes	WQHE	394	381558	2zc1f	ok007	2021	1:24000
Quinlan-Woodward complex, 5 to 12 percent slopes	48	14790	381686	2t6qh	ok009	1978	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	64	10611	381704	2w5qn	ok009	1978	1:24000
Quinlan-Obaro complex, 5 to 12 percent slopes	46	10254	381684	2t6qb	ok009	1978	1:24000
Obaro-Quinlan complex, 3 to 5 percent slopes	41	5706	381679	dt57	ok009	1978	1:24000
Obaro-Quinlan complex, 1 to 3 percent slopes	40	3862	381678	dt56	ok009	1978	1:24000
Quinlan-Obaro complex, 3 to 5 percent slopes, eroded	45	3820	381683	dt5c	ok009	1978	1:24000
Woodward-Quinlan complex, 1 to 3 percent slopes	63	2862	381703	2w5qm	ok009	1978	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded	47	1166	381685	2t6qf	ok009	1978	1:24000
Quinlan-Woodward complex, 5 to 20 percent slopes	QwF	17892	381762	2t6qj	ok011	1965	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	WuC	9966	381929	2w5qn	ok015	1967	1:24000
Quinlan-Woodward complex, 5 to 12 percent slopes	WwE	135025	382351	2t6qh	ok039	1973	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	WwC	32443	382350	2w5qn	ok039	1973	1:24000
Quinlan and Woodward soils, 3 to 8 percent slopes, severely eroded	QwE3	16956	382339	2t6qk	ok039	1973	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded	QwC2	4407	382338	2t6qf	ok039	1973	1:24000
Quinlan-Woodward complex, 5 to 20 percent slopes	QwE	108759	382395	2t6qj	ok043	1961	1:24000
Quinlan loam, 8 to 20 percent slopes	Qm	37020	382391	2t6q0	ok043	1961	1:24000
Quinlan-Hardeman complex, 5 to 20 percent slopes	Qp	26425	382393	dtx8	ok043	1961	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded	QwC2	16100	382394	2t6qf	ok043	1961	1:24000
Quinlan loam, 5 to 20 percent slopes, severely eroded	Qn3	6958	382392	dtx7	ok043	1961	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	WwC	4751	382413	2w5qn	ok043	1961	1:24000
Quinlan-Rock outcrop complex, 12 to 45 percent slopes	Rb	3500	382396	2t6qd	ok043	1961	1:24000
Quinlan-Woodward complex, 8 to 20 percent slopes	QwE	19124	382463	dtzj	ok045	1963	1:24000
Woodward-Quinlan complex, 5 to 12 percent slopes	WwE	17243	382480	dv02	ok045	1963	1:24000
Quinlan-Rock outcrop complex, 12 to 45 percent slopes	Rb	7132	382464	2t6qd	ok045	1963	1:24000
Quinlan-Obaro-Rock outcrop complex, 8 to 20 percent slopes	Vx	5900	382474	dtzw	ok045	1963	1:24000
Woodward-Quinlan complex, 3 to 8 percent slopes, eroded	WwD2	4198	382479	dv01	ok045	1963	1:24000
Woodward-Quinlan complex, 5 to 12 percent slopes	WoQE	2067	636644	2w5qr	ok055	2005	1:24000
Quinlan-Rock outcrop complex, 12 to 45 percent slopes	QnRG	504	636641	2t6qd	ok055	2005	1:24000
Woodward-Quinlan complex, 5 to 12 percent slopes	71	19185	975508	2w5qr	ok057	1982	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	70	8362	975507	2w5qs	ok057	1982	1:24000
Quinlan-Rock outcrop complex, 12 to 45 percent slopes	48	6234	975482	2t6qd	ok057	1982	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded	49	4565	975483	2t6qf	ok057	1982	1:24000
Woodward-Quinlan complex, 1 to 3 percent slopes	69	2080	975505	11r2x	ok057	1982	1:24000
Quinlan-Rock outcrop-Yomont complex, 0 to 45 percent slopes	QRYG	53004	383109	dvnc	ok059	1998	1:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopes	QWDE	47923	383107	2t6qr	ok059	1998	1:24000
Westola-Quinlan-Hardeman complex, 0 to 12 percent slopes	WQHE	41808	383108	dvnb	ok059	1998	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	WQnC	35359	383048	2w5qn	ok059	1998	1:24000
Woodward-Quinlan complex, 1 to 3 percent slopes	WQnB	16751	383047	2w5qm	ok059	1998	1:24000
Quinlan-Woodward complex, 5 to 8 percent slopes	QnWD	8552	383049	dvlf	ok059	1998	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, severely eroded	QnWC3	3514	383111	dvnf	ok059	1998	1:24000
Quinlan-Rock outcrop-Woodward complex, 5 to 45 percent slopes	QRWG	2789	383110	dvnd	ok059	1998	1:24000
Talpa-Rock outcrop-Quinlan complex, 1 to 5 percent slopes	TRQC	1943	383106	dvn8	ok059	1998	1:24000
Quinlan-Woodward-Rock outcrop complex, 1 to 5 percent slopes	QWRC	1150	383105	dvn7	ok059	1998	1:24000
Quinlan-Woodward complex, 5 to 12 percent slopes	QnWE	656	383112	2t6qh	ok059	1998	1:24000
Quinlan-Rock outcrop complex, 12 to 45 percent slopes	Ru	11685	383858	2t6qd	ok093	1965	1:24000
Dill-Quinlan complex, 5 to 12 percent slopes	DfE	11408	383824	dwdf	ok093	1965	1:24000
Quinlan loam, 3 to 5 percent slopes, eroded	QlC2	769	383853	dwfc	ok093	1965	1:24000
Quinlan loam, 1 to 3 percent slopes MLRA 78C	QlB	707	383852	2t6pw	ok093	1965	1:24000
Quinlan-Woodward complex, 5 to 20 percent slopes	QnWE	9	697943	2t6qj	ok093	1965	1:24000
Quinlan-Woodward complex, 5 to 12 percent slopes	QwE	176193	384769	2t6qh	ok129	1961	1:24000
Quinlan-Rock outcrop complex, 12 to 45 percent slopes	Rb	55976	384771	2t6qd	ok129	1961	1:24000
Quinlan and Woodward soils, 3 to 8 percent slopes, severely eroded	Qu3	11233	384767	2t6qk	ok129	1961	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	WwC	9736	384791	2w5qn	ok129	1961	1:24000
Woodward-Quinlan complex, 1 to 3 percent slopes	WsB	4199	384788	2w5qm	ok129	1961	1:24000
Woodward-Quinlan loams, 1 to 3 percent slopes	WwB	3900	384790	2w5qp	ok129	1961	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded	QwC2	3086	384768	2t6qf	ok129	1961	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	WsC	2782	384789	dxdk	ok129	1961	1:24000
Quinlan-Obaro complex, 5 to 12 percent slopes	QuOE	19	1605237	2t6qb	ok129	1961	1:24000
Quinlan-Rock outcrop complex, 5 to 30 percent slopes	Ve	2583	384927	dxk0	ok139	1959	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	55	26463	385042	2w5qn	ok149	1976	1:24000
Quinlan-Woodward complex, 5 to 12 percent slopes	40	16731	385026	2t6qh	ok149	1976	1:24000
Quinlan-Obaro complex, 5 to 12 percent slopes	37	13274	385022	2t6qb	ok149	1976	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded	39	10617	385024	2t6qf	ok149	1976	1:24000
Dill-Quinlan complex, 5 to 12 percent slopes	21	6829	385005	dxmj	ok149	1976	1:24000
Woodward-Quinlan complex, 1 to 3 percent slopes	54	2660	385041	2w5qm	ok149	1976	1:24000
Quinlan and Dill soils, 3 to 12 percent slopes, severely eroded	41	2643	385027	dxn7	ok149	1976	1:24000
Quinlan-Rock outcrop complex, 8 to 20 percent slopes	38	1958	385023	dxn3	ok149	1976	1:24000
Dill-Quinlan complex, 3 to 5 percent slopes	20	1482	385004	dxmh	ok149	1976	1:24000
Dill-Quinlan complex, 1 to 3 percent slopes	19	92	385002	dxmf	ok149	1976	1:24000
Quinlan-Woodward-Burson complex, 12 to 45 percent slopes	QWBG	32555	385225	dxvm	ok151	1995	1:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopes	QWDE	26743	385226	2t6qr	ok151	1995	1:24000
Woodward-Quinlan-Burson complex, 3 to 5 percent slopes, eroded	WQBC2	9393	385249	2w5qq	ok151	1995	1:24000
Quinlan-Woodward-Burson complex, 5 to 12 percent slopes, eroded	QWBE2	7290	385224	dxvl	ok151	1995	1:24000
Talpa-Quinlan-Rock outcrop complex, 1 to 60 percent slopes	TQRH	1281	385236	dxvz	ok151	1995	1:24000
Quinlan-Woodward complex, 5 to 12 percent slopes	QwD	41907	385297	dxxy	ok153	1961	1:24000
Quinlan loam, 8 to 20 percent slopes	Qm	16196	385295	2t6q0	ok153	1961	1:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded	QwC2	10079	385296	2t6qf	ok153	1961	1:24000
Quinlan-Woodward complex, 5 to 12 percent slopes, eroded	QwD2	8982	385298	dxxz	ok153	1961	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	WwC	2217	385316	2w5qn	ok153	1961	1:24000
Quinlan complex	Qc	28952	362491	d568	tx011	1963	1:20000
Quinlan and Burson soils, hilly	QBG	82511	363295	d616	tx045	1972	1:20000
Burson and Quinlan soils steep	BQG	72224	363269	d60c	tx045	1972	1:20000
Obaro and Quinlan soils, rolling	OQE	28743	363286	d60x	tx045	1972	1:20000
Burson-Quinlan-Rock outcrop association, 8 to 45 percent slopes	BQG	1424	377944	dp8r	tx065	2000	1:24000
Quinlan-Woodward loams, 8 to 20 percent slopes	QuE	21378	363836	2t6qn	tx075	1961	1:20000
Woodward-Quinlan complex, 5 to 12 percent slopes	WwD	9990	363859	2w5qr	tx075	1961	1:20000
Quinlan-Woodward loams	Qw	74607	364120	d6wt	tx087	1965	1:20000
Lutie-Quinlan-Cottonwood complex	Lx	38635	364108	d6wf	tx087	1965	1:20000
Woodward-Quinlan complex, 3 to 5 percent slopes	WuC	9200	364137	2w5qs	tx087	1965	1:20000
Woodward and Quinlan loams, 3 to 12 percent slopes	Wu	33930	364636	2w5q4	tx101	1969	1:20000
Deepwood-Quinlan-Cottonwood complex, 5 to 50 percent slopes	DCG	50558	365143	2wt7h	tx125	1965	1:20000
Woodward-Deepwood-Quinlan complex, warm, 2 to 12 percent slopes	WQE	41185	365161	2wt7j	tx125	1965	1:20000
Deepwood-Woodward-Quinlan complex, warm, 2 to 45 percent slopes	DQG	19109	365112	2y7bd	tx125	1965	1:20000
Obaro-Quinlan association, 5 to 12 percent slopes	OQE	77812	365192	2t6q3	tx129	1975	1:24000
Woodward-Quinlan complex, 3 to 5 percent slopes	WwC	27790	365829	2w5qs	tx151	1964	1:24000
Quinlan-Woodward complex	Qw	21168	365803	d8n3	tx151	1964	1:24000
Woodward-Quinlan complex, 5 to 12 percent slopes	WwD	14779	365830	2w5qr	tx151	1964	1:24000
Woodward-Quinlan loams, 1 to 3 percent slopes	WwB	4993	365828	d8nx	tx151	1964	1:24000
Obaro-Quinlan association, 5 to 12 percent slopes	OBD	1447	695960	2t6q3	tx153	2004	1:24000
Woodward-Quinlan complex, 5 to 50 percent slopes	WcF	1308	391959	f4vv	tx179	1965	1:20000
Woodward-Quinlan complex, 5 to 12 percent slopes	WwD	121225	366974	2w5qr	tx191	1965	1:20000
Quinlan-Woodward complex	Qw	85576	366956	d9v9	tx191	1965	1:20000
Obaro and Quinlan soils rolling	OQE	12438	367934	dbvv	tx233	1972	1:24000
Quinlan soils, sloping	QuC	65192	368500	dcg3	tx263	1968	1:31680
Woodward and Quinlan loams, 3 to 12 percent slopes	WoC	36881	368514	2w5q4	tx263	1968	1:31680
Woodward-Deepwood-Quinlan complex, warm, 2 to 12 percent slopes	WQE	35033	368617	2wt7j	tx269	1999	1:31680
Deepwood-Woodward-Quinlan complex, warm, 2 to 45 percent slopes	DQG	28770	368607	2y7bd	tx269	1999	1:31680
Deepwood-Quinlan-Cottonwood complex, 5 to 50 percent slopes	DCG	11725	368606	2wt7h	tx269	1999	1:31680
Obaro and Quinlan association, 3 to 30 percent slopes	OBG	1448	379075	dqg7	tx305	1999	1:24000
Woodward and Quinlan loams, 3 to 12 percent slopes	WQD	68949	370900	2w5q4	tx345	1972	1:24000
Quinlan loam, 3 to 12 percent slopes	QuD	5481	370892	dfy8	tx345	1972	1:24000
Quinlan loam, 1 to 5 percent slopes	31	13799	371000	dg1r	tx353	1979	1:24000
Burson-Quinlan association, hilly	2	13772	370987	dg1b	tx353	1979	1:24000
Quinlan-Burson-Woodward association, rolling	32	4686	371001	dg1s	tx353	1979	1:24000
Burson-Quinlan-Rock outcrop association, steep	BQG	31140	3124210	dgd5	tx375	1974	1:24000
Aspermont-Quinlan association, hilly	AQF	6175	3124205	dgcz	tx375	1974	1:24000
Knoco-Quinlan-Burson association, 5 to 50 percent slopes	KQB	10418	371416	dgh5	tx381	1999	1:24000
Quinlan-Woodward complex, 5 to 30 percent slopes	QwE	2345	371410	dggz	tx381	1999	1:24000
Obaro-Quinlan association, rolling	OQE	499	371524	dgln	tx393	1979	1:24000
Quinlan soils	Qu	22471	372025	dh3t	tx415	1966	1:24000
Woodward-Quinlan complex, 5 to 12 percent slopes	WoD	39127	372314	2w5qr	tx433	1970	1:24000
Quinlan-Rough broken land complex	Qr	31117	372299	dhdn	tx433	1970	1:24000
Obaro-Quinlan association, 5 to 12 percent slopes	OuD	33018	373318	2t6q3	tx483	1970	1:24000
Gypsum outcrop and Quinlan soils, undulating	GyC	3448	373304	djg2	tx483	1970	1:24000

Map of Series Extent

Approximate geographic distribution of the QUINLAN 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).