Soil Data Explorer - COLONEL

Official Series Description

Lab Data Summary

Aggregate lab data for the COLONEL soil series. This aggregation is based on all pedons with a current taxon name of COLONEL, 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 COLONEL 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	2013NH605001	2013NH605001	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0403242,-71.7923676
143	2013NH605016	2013NH605016	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0672618,-71.8358139
143	2013NH605037	2013NH605037	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0875361,-71.7883722
143	2013NH605041	2013NH605041	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0795417,-71.7864972
143	2013NH605042	2013NH605042	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0809889,-71.7854278
143	2013NH605045	2013NH605045	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.1359944,-71.8228667
143	2013NH605059	2013NH605059	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0549389,-71.8488611
143	2013NH605062	2013NH605062	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0572278,-71.8412167
143	2013NH605069	2013NH605069	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0895806,-71.7709417
143	2013NH605071	2013NH605071	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0926694,-71.7731222
143	2013NH605075	2013NH605075	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0546528,-71.7774639
143	2013NH605076	2013NH605076	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0984639,-71.78365
143	2013NH605082	2013NH605082	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0673472,-71.8202639
143	09N0154	S08ME021002.Colonel	COLONEL	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.4093819,-69.1407318
143	09N0163	S08ME021011.Colonel	COLONEL	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.9188614,-69.1592789
143	10N0330	S09ME021014.Colonel	Colonel	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.4241111,-69.0587778
143	40A4198	S1977ME021003	Colonel	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.1066132,-69.2032547
143	00P1237	S2000VT003001	Colonel	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.089118,-73.019329
143	00P1236	S2000VT007001	Colonel	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.5352783,-72.8354721
144B	2013NH605033	2013NH605033	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0711417,-71.8406722
144B	2013NH605054	2013NH605054	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0695222,-71.8174944
144B	2013NH605055	2013NH605055	Colonel	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0722194,-71.8220667
144B	87P0593	87ME001001	Colonel	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.2708321,-70.2402802
144B	93P0832	S1993VT005002	Colonel	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.2572212,-72.2744446
144B	93P0833	S1993VT005003	Colonel	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.2858315,-72.2944412
n/a	91P0048	90ME019002	Colonel	6	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 COLONEL 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 COLONEL 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 COLONEL 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 COLONEL 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 COLONEL 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 COLONEL 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 COLONEL 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 terrace figure.

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

Soil series sharing subgroup-level classification with COLONEL, 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. ME-2010-09-03-01 | Franklin County Area and Part of Somerset County - 2003

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

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

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

3. ME-2012-02-03-07 | Oxford County Area - March 1995

   Typical pattern of the soils and underlying material in the Hermon-Monadnock-Skerry general soil map unit (Soil Survey of Oxford County Area, Maine; March 1995).

4. ME-2012-02-03-09 | Oxford County Area - March 1995

   Typical pattern of the soils and underlying material in the Colonel-Brayton-Skerry general soil map unit (Soil Survey of Oxford County Area, Maine; March 1995).

5. ME-2012-02-03-11 | Oxford County Area - March 1995

   Typical pattern of the soils and underlying material in the Lyman-Tunbridge-Monadnock general soil map unit (Soil Survey of Oxford County Area, Maine; March 1995).

Map Units

Map units containing COLONEL 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
Skerry-Colonel association, 0 to 15 percent slopes, very stony	STC	13581	315824	2x9p8	me005	1969	1:24000
Colonel-Brayton assocation, 0 to 8 percent slopes, very stony	CFB	9685	315664	blgq	me005	1969	1:24000
Colonel fine sandy loam, 0 to 8 percent slopes, very stony	CdB	5034	300098	2ty6q	me005	1969	1:24000
Colonel fine sandy loam, 3 to 8 percent slopes	CcB	2404	300105	2ty6n	me005	1969	1:24000
Colonel fine sandy loam, 8 to 15 percent slopes, very stony	CdC	587	300106	2ty6r	me005	1969	1:24000
Skerry-Colonel association, 3 to 15 percent slopes	SSC	334	315823	2x9p6	me005	1969	1:24000
Skerry-Colonel association, 15 to 35 percent slopes, very stony	STD	303	315825	2x9p9	me005	1969	1:24000
Peru-Colonel association, 3 to 15 percent slopes, very stony	DUC	156	315782	2w9nv	me005	1969	1:24000
Colonel fine sandy loam, 8 to 15 percent slopes	CcC	95	300091	2ty6p	me005	1969	1:24000
Colonel-Peru association, 3 to 15 percent slopes, very stony	CPC	126158	284979	2ty7t	me610	1992	1:20000
Brayton-Colonel association, 0 to 8 percent slopes, very stony	BSB	36403	284965	2ty7s	me610	1992	1:20000
Colonel fine sandy loam, 3 to 8 percent slopes	CnB	1786	284988	2ty6n	me610	1992	1:20000
Colonel fine sandy loam, 0 to 8 percent slopes, very stony	CoB	1631	284990	2ty6q	me610	1992	1:20000
Colonel fine sandy loam, 8 to 15 percent slopes, very stony	CoC	419	284991	2ty6r	me610	1992	1:20000
Colonel fine sandy loam, 8 to 15 percent slopes	CnC	378	284989	2ty6p	me610	1992	1:20000
Peru-Colonel association, 15 to 35 percent slopes, very stony	DUD	16	319818	2w9nx	me610	1992	1:20000
Peru-Colonel association, 3 to 15 percent slopes	DTC	3	300054	2w9nw	me610	1992	1:20000
Brayton-Colonel association, 0 to 8 percent slopes, very stony	BSB	34093	285077	2ty7r	me611	1988	1:20000
Peru-Colonel complex, 3 to 8 percent slopes, very stony	DtB	22009	285096	2trs2	me611	1988	1:20000
Peru-Colonel complex, 3 to 8 percent slopes	DsB	8289	285095	2xk0s	me611	1988	1:20000
Peru-Colonel-Tunbridge complex, 3 to 8 percent slopes, very stony	DWB	7932	285091	2tsw1	me611	1988	1:20000
Brayton-Colonel association, gently sloping, rubbly	BTB	5854	285078	9kn2	me611	1988	1:20000
Peru-Colonel-Tunbridge association, 3 to 15 percent slopes, very stony	PCC	28572	744557	szrz	me612	2016	1:24000
Brayton-Colonel complex, 0 to 8 percent slopes, very stony	BRB	21956	746267	t1k4	me612	2016	1:24000
Colonel-Peru-Brayton complex, 0 to 8 percent slopes, very stony	CDB	19535	744551	szrs	me612	2016	1:24000
Scantic-Lamoine-Colonel association, 0 to 8 percent slopes, very stony	SLB	15936	742170	sx8z	me612	2016	1:24000
Brayton-Colonel-Lyman complex, 0 to 8 percent slopes, rocky	BYB	8357	744552	szrt	me612	2016	1:24000
Colonel-Peru complex, 3 to 8 percent slopes, very stony	CpB	2923	1482979	1ls51	me612	2016	1:24000
Skerry-Becket-Colonel complex, 0 to 8 percent slopes, very bouldery	SKB	1685	2643637	2rk0h	me612	2016	1:24000
Brayton-Colonel complex, 0 to 8 percent slopes, very stony	BcB	1572	2481984	2p9q0	me612	2016	1:24000
Colonel gravelly fine sandy loam, 3 to 8 percent slopes	CoB	1177	741212	sw92	me612	2016	1:24000
Skerry-Colonel association, 0 to 15 percent slopes, very stony	STC	107657	285828	2x9p8	me613	1987	1:20000
Skerry-Colonel association, 15 to 35 percent slopes, very stony	STD	25109	285829	2x9p9	me613	1987	1:20000
Colonel fine sandy loam, 0 to 8 percent slopes, very stony	CfB	16421	285750	2ty6q	me613	1987	1:20000
Peru-Colonel association, 3 to 15 percent slopes, very stony	DUC	12098	285760	2w9nv	me613	1987	1:20000
Peru-Colonel association, 15 to 35 percent slopes, very stony	DUD	6141	285761	2w9nx	me613	1987	1:20000
Skerry-Colonel association, 3 to 15 percent slopes	SSC	5240	285827	2x9p6	me613	1987	1:20000
Colonel fine sandy loam, 3 to 8 percent slopes	CeB	3127	285748	2ty6n	me613	1987	1:20000
Colonel fine sandy loam, 8 to 15 percent slopes, very stony	CfC	1552	285751	2ty6r	me613	1987	1:20000
Peru-Colonel association, 3 to 15 percent slopes	DTC	743	285759	2w9nw	me613	1987	1:20000
Colonel fine sandy loam, 8 to 15 percent slopes	CeC	475	285749	2ty6p	me613	1987	1:20000
Colonel-Brayton-Peru association, 0 to 8 percent slopes, very stony	CPB	65089	285311	2ty7q	me615	1994	1:24000
Peru-Colonel-Lyman association, 3 to 15 percent slopes, very stony	DYC	28729	285323	2w9p0	me615	1994	1:24000
Peru-Colonel association, 3 to 15 percent slopes, very stony	DXC	20967	285322	2w9nv	me615	1994	1:24000
Colonel-Brayton-Lyman complex, undulating, very stony	CQB	8771	285312	9kwm	me615	1994	1:24000
Colonel-Hermon association, 0 to 15 percent slopes, extremely bouldery	CRC	3899	285313	2x9qb	me615	1994	1:24000
Colonel fine sandy loam, 3 to 8 percent slopes	CoB	223	285316	2ty6n	me615	1994	1:24000
Brayton-Colonel association, 0 to 8 percent slopes, very stony	BRB	50367	285532	2ty7r	me617	2004	1:24000
Peru-Colonel complex, 0 to 8 percent slopes, very stony	DHB	34312	285559	2trrw	me617	2004	1:24000
Peru-Tunbridge-Colonel complex, 3 to 15 percent slopes, very stony	DWC	26057	285562	2w9nd	me617	2004	1:24000
Lamoine-Scantic-Colonel complex, 0 to 8 percent slopes, very stony	LSB	24016	285585	2x1br	me617	2004	1:24000
Skerry-Colonel association, 0 to 8 percent slopes, very stony	SOB	17234	285618	2x9p7	me617	2004	1:24000
Skerry-Colonel-Tunbridge complex, 0 to 15 percent slopes, very stony	STC	16629	285619	2xk0d	me617	2004	1:24000
Brayton-Colonel association, 0 to 8 percent slopes, extremely stony	BTB	6464	285533	9l3r	me617	2004	1:24000
Skerry-Colonel-Rawsonville complex, 0 to 15 percent slopes, very stony	SRC	4767	1401289	1j14w	me617	2004	1:24000
Peru-Colonel complex, 3 to 8 percent slopes	DgB	3550	285565	2xk0s	me617	2004	1:24000
Peru-Colonel complex, 3 to 8 percent slopes, very stony	DkB	2816	285566	2trs2	me617	2004	1:24000
Peru-Rawsonville-Colonel complex, 3 to 15 percent slopes, very stony	DUC	778	1401264	1j142	me617	2004	1:24000
Colonel-Peru-Pillsbury association, 3 to 15 percent slopes, very stony	CNC	91076	285680	2trrg	me619	2005	1:24000
Colonel-Pillsbury-Peru association, 0 to 8 percent slopes, very stony	CPB	84439	285679	2trrj	me619	2005	1:24000
Peru-Colonel-Rawsonville association, 3 to 15 percent slopes	DTC	81834	285674	9l89	me619	2005	1:24000
Peru-Colonel-Marlow association, 3 to 15 percent slopes, very stony	DMC	49454	285677	2trrh	me619	2005	1:24000
Colonel-Skerry-Pillsbury association, 0 to 15 percent slopes, very stony	CSC	25179	285666	2x9qf	me619	2005	1:24000
Colonel-Pillsbury-Skerry association, 0 to 8 percent slopes, very stony	CRB	22875	285665	2x9qc	me619	2005	1:24000
Mahoosuc-Colonel-Pillsbury association, 1 to 16 percent slopes	MCC	867	285720	9l9s	me619	2005	1:24000
Brayton-Colonel-Peru association, 0 to 8 percent slopes, extremely stony	BCB	44403	2549914	2trrl	me620	2011	1:24000
Peru-Colonel-Rawsonville association, 3 to 15 percent slopes, very stony	DOC	32774	2549910	2qtlz	me620	2011	1:24000
Colonel-Peru-Brayton association, 3 to 15 percent slopes, very bouldery	CDB	29713	2549915	2trrr	me620	2011	1:24000
Peru-Colonel-Marlow association, 3 to 15 percent slopes, very bouldery	DCC	25508	2549912	2trs1	me620	2011	1:24000
Brayton-Colonel-Skerry association, 0 to 8 percent slopes, extremely bouldery	BSB	15879	2549900	2x9q9	me620	2011	1:24000
Brayton-Colonel-Ragmuff association, 0 to 8 percent slopes, extremely stony	BRB	11528	2549909	2qtly	me620	2011	1:24000
Skerry-Colonel association, 0 to 15 percent slopes, extremely bouldery	SCC	8817	2549901	2x9pb	me620	2011	1:24000
Peru-Colonel-Rawsonville association, 3 to 15 percent slopes, very stony	DOC	21823	2549854	2qtk7	me621	2011	1:24000
Colonel-Peru-Brayton association, 3 to 15 percent slopes, very bouldery	CDB	11326	2549856	2trrr	me621	2011	1:24000
Brayton-Colonel-Peru association, 0 to 8 percent slopes, extremely stony	BCB	9584	2549855	2trrl	me621	2011	1:24000
Peru-Colonel-Marlow association, 3 to 15 percent slopes, very bouldery	DCC	1230	2549852	2trs1	me621	2011	1:24000
Colonel-Brayton-Peru association, 0 to 8 percent slopes, very stony	CLB	89788	1909288	2ty7q	me622	2007	1:24000
Peru-Tunbridge-Colonel complex, 3 to 15 percent slopes, very stony	DXC	63847	1909278	2w9nd	me622	2007	1:24000
Colonel-Peru-Brayton association, 0 to 15 percent slopes, very stony	CNC	54495	1909289	2trrk	me622	2007	1:24000
Peru-Colonel-Marlow association, 3 to 15 percent slopes, very stony	DOC	38767	1909286	2trrh	me622	2007	1:24000
Colonel-Skerry-Brayton association, 0 to 15 percent slopes, very stony	COC	29016	1909179	2x9qd	me622	2007	1:24000
Brayton-Colonel association, 0 to 8 percent slopes, very stony	BLB	12650	1909092	2ty7r	me622	2007	1:24000
Brayton-Colonel association, 0 to 8 percent slopes, extremely stony	BNB	6378	1909093	222kn	me622	2007	1:24000
Brayton-Colonel association, 0 to 8 percent slopes, rubbly	BOB	4586	1909275	222rj	me622	2007	1:24000
Peru-Colonel complex, 0 to 8 percent slopes, very stony	DNB	4418	1909090	2trrw	me622	2007	1:24000
Lamoine-Scantic-Colonel complex, 0 to 8 percent slopes, very stony	LLB	1944	1909083	2x1br	me622	2007	1:24000
Skerry-Colonel association, 0 to 8 percent slopes, very stony	SRB	899	1909089	2x9p7	me622	2007	1:24000
Peru-Colonel-Tunbridge complex, 3 to 8 percent slopes, very stony	DTB	802	1909274	222rh	me622	2007	1:24000
Skerry-Colonel association, 0 to 8 percent slopes, very stony	759B	148	280743	2x9p7	nh607	2000	1:24000
Skerry-Colonel association, 15 to 35 percent slopes, very stony	759D	27	280739	2x9p9	nh607	2000	1:24000
Colonel-Cabot complex, 3 to 15 percent slopes, extremely bouldery	87C	8042	282996	2w9nr	vt005	2006	1:20000
Colonel-Cabot complex, 8 to 15 percent slopes, very stony	73C	3541	282973	2w9nn	vt005	2006	1:20000
Colonel-Cabot complex, 3 to 8 percent slopes, very stony	73B	1420	282972	2w9nl	vt005	2006	1:20000
Colonel-Cabot complex, 3 to 8 percent slopes	72B	408	282969	2w9nk	vt005	2006	1:20000
Colonel-Cabot complex, 8 to 15 percent slopes	72C	251	282970	2w9nm	vt005	2006	1:20000
Colonel-Cabot complex, 15 to 35 percent slopes, very stony	73D	213	282974	2w9nq	vt005	2006	1:20000
Colonel-Cabot complex, 15 to 25 percent slopes	72D	8	282971	2w9np	vt005	2006	1:20000
Cabot-Colonel complex, 8 to 15 percent slopes, very stony	SIE12	72774	2409964	2w9nf	vt009	2012	1:
Peru-Colonel complex, 15 to 35 percent slopes, very stony	SIE33	42169	2409969	2trrp	vt009	2012	1:
Tunbridge-Peru-Colonel complex, 15 to 35 percent slopes, very stony	SIE43	41922	2409977	2trrq	vt009	2012	1:
Tunbridge-Colonel-Cabot complex, 8 to 15 percent slopes, very stony	SIE42	37510	2409976	2w9nt	vt009	2012	1:
Wilmington-Colonel complex, 0 to 8 percent slopes, very stony	SIE21	20230	2409966	2xk1f	vt009	2012	1:
Monadnock-Sunapee-Colonel complex, 8 to 15 percent slopes, very stony	SIE62	10621	2503893	2q31h	vt009	2012	1:
Cabot-Colonel complex, 8 to 15 percent slopes	SIE12N	1035	2505002	2w9nj	vt009	2012	1:
Colonel-Peru complex, 8 to 15 percent slopes, very stony	SIE32	974	2420415	2m7mx	vt009	2012	1:
Wilmington-Colonel complex, 3 to 8 percent slopes	SIE21N	519	2505003	2q47l	vt009	2012	1:
Tunbridge-Colonel-Cabot complex, 8 to 15 percent slopes, rocky	SIE42N	499	2505007	2w9ns	vt009	2012	1:
Monadnock-Sunapee-Colonel complex, 8 to 15 percent slopes	SIE62N	126	2505011	2q47v	vt009	2012	1:
Peru-Colonel complex, 15 to 25 percent slopes	SIE33N	79	2505005	2xk0r	vt009	2012	1:
Tunbridge-Peru-Colonel complex, 15 to 25 percent slopes, rocky	SIE43N	59	2505008	2q47r	vt009	2012	1:
Colonel-Peru complex, 8 to 15 percent slopes	SIE32N	8	2505004	2q47m	vt009	2012	1:
Colonel-Cabot complex, 8 to 15 percent slopes, very stony	259C	12805	283435	2w9nn	vt019	2005	1:20000
Colonel-Cabot complex, 3 to 8 percent slopes, very stony	259B	6468	283434	2w9nl	vt019	2005	1:20000
Colonel-Cabot complex, 3 to 8 percent slopes	247B	4457	283430	2w9nk	vt019	2005	1:20000
Colonel-Cabot complex, 8 to 15 percent slopes	247C	1865	283431	2w9nm	vt019	2005	1:20000
Colonel-Cabot complex, 15 to 35 percent slopes, very stony	259D	1209	283436	2w9nq	vt019	2005	1:20000
Colonel-Cabot complex, 15 to 25 percent slopes	247D	52	283432	2w9np	vt019	2005	1:20000
Colonel fine sandy loam, 8 to 15 percent slopes, very stony	19C	12338	282578	2ty6r	vt023	1996	1:20000
Colonel fine sandy loam, 8 to 15 percent slopes	14C	7243	282543	2ty6p	vt023	1996	1:20000
Colonel fine sandy loam, 3 to 15 percent slopes, extremely bouldery	99C	4066	282802	2trr9	vt023	1996	1:20000
Colonel fine sandy loam, 15 to 35 percent slopes, very stony	19D	3330	282579	2trr8	vt023	1996	1:20000
Colonel fine sandy loam, 0 to 8 percent slopes, very stony	19B	3088	282577	2ty6q	vt023	1996	1:20000
Colonel fine sandy loam, 3 to 8 percent slopes	14B	2843	282542	2ty6n	vt023	1996	1:20000
Colonel fine sandy loam, 15 to 35 percent slopes, extremely bouldery	99D	1042	282803	2trrb	vt023	1996	1:20000
Colonel fine sandy loam, 15 to 25 percent slopes	14D	747	282544	2trr7	vt023	1996	1:20000
Peru, Skerry, and Colonel soils, 8 to 15 percent slopes, very stony	18C	21317	283141	2w9r1	vt027	2000	1:20000
Peru, Skerry, and Colonel soils, 8 to 15 percent slopes	17C	6969	283138	2w9qy	vt027	2000	1:20000
Peru-Colonel-Marlow association, 3 to 35 percent slopes, very stony	203D	6813	283338	9hty	vt027	2000	1:20000
Peru, Skerry, and Colonel soils, 15 to 25 percent slopes	17D	2508	283139	2w9qz	vt027	2000	1:20000
Peru, Skerry, and Colonel soils, 3 to 8 percent slopes	17B	2489	283137	2w9qx	vt027	2000	1:20000
Peru, Skerry, and Colonel soils, 0 to 8 percent slopes, very stony	18B	2268	283140	2w9r0	vt027	2000	1:20000

Map of Series Extent

Approximate geographic distribution of the COLONEL 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).