Soil Data Explorer - CULLASAJA

Official Series Description

Lab Data Summary

Aggregate lab data for the CULLASAJA soil series. This aggregation is based on all pedons with a current taxon name of CULLASAJA, 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 CULLASAJA 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
130B	86P0743	86NC113023	Cullasaja	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.0577774,-83.4641647
130B	93P0266	91NC171003	Cullasaja	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.5,-80.9180527
130B	04N1080	S2004NC009002	Cullasaja	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.4050827,-81.4731979

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CULLASAJA 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 CULLASAJA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the CULLASAJA 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 2024-10-23).

Geomorphic description summaries for the CULLASAJA 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 2024-10-23).

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

Competing Series

Soil series competing with CULLASAJA share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the CULLASAJA 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 2024-10-23).

Geomorphic description summaries for the CULLASAJA 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 2024-10-23).

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 CULLASAJA, 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 2024-10-23).

Block Diagrams

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

1. NC-2012-02-07-07 | Clay County - 1998

   Typical relationship of soils, aspect, landscape position, and parent material in the Edneyville-Plott-Chestnut-Cullasaja general soil map unit in the intermediate mountains (Soil Survey of Clay County, North Carolina; 1998).

2. NC-2012-02-07-17 | Haywood County Area - October 1997

   Typical relationship between soils, aspect, landscape position, and parent material of intermediate mountains in an area of the Plott-Edneyville-Chestnut general soil map unit (Soil Survey of Haywood County Area, North Carolina; October 1997).

3. NC-2012-02-07-19 | Jackson County - June 1997

   Relationship of soils, aspect, parent material, and landscape position in the Plott-Edneyville-Chestnut-Cullasaja soil map unit (Soil Survey of Jackson County, North Carolina; June 1997).

Map Units

Map units containing CULLASAJA 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
Cullasaja cobbly loam, 15 to 30 percent slopes, extremely bouldery	CtD	4132	548059	ld9b	nc011	1997	1:12000
Cullasaja cobbly loam, 30 to 50 percent slopes, extremely bouldery	CtE	3702	548060	ld9c	nc011	1997	1:12000
Cullasaja cobbly loam, 8 to 15 percent slopes, extremely bouldery	CtC	393	548058	ld99	nc011	1997	1:12000
Cullasaja cobbly fine sandy loam, 8 to 30 percent slopes, very bouldery	CsD	25	548057	ld98	nc011	1997	1:12000
Cullasaja cobbly loam, 30 to 50 percent slopes, extremely bouldery	CtE	164	2679214	2r92b	nc027	2012	1:12000
Cullasaja cobbly loam, 15 to 30 percent slopes, extremely bouldery	CtD	123	2679213	2r929	nc027	2012	1:12000
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, stony	CuD	4224	546399	lbks	nc043	1991	1:12000
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, stony	CuE	4035	546400	lbkt	nc043	1991	1:12000
Tuckasegee-Cullasaja complex, 8 to 15 percent slopes, stony	TsC	1144	546465	lbmx	nc043	1991	1:12000
Cullasaja-Tuckasegee complex, 50 to 95 percent slopes, stony	CuF	247	546401	lbkv	nc043	1991	1:12000
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, very stony	101E	1792	2509136	2p7p3	nc089	1974	1:20000
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, very stony	101D	1520	2509135	2p7p2	nc089	1974	1:20000
Cullasaja-Tuckasegee complex, 8 to 15 percent slopes, stony	101C	202	2509134	2p7p1	nc089	1974	1:20000
Cullasaja very cobbly fine sandy loam, 30 to 50 percent slopes, extremely bouldery	99E	96	2509132	2p7nx	nc089	1974	1:20000
Cullasaja-Tuckasegee complex, windswept, 30 to 50 percent slopes, very bouldery	102E	17	2509289	2p835	nc089	1974	1:20000
Cullasaja-Tuckasegee complex, 50 to 95 percent slopes, very stony	101F	14	2509137	2p7p4	nc089	1974	1:20000
Cullasaja very cobbly fine sandy loam, 15 to 30 percent slopes, extremely bouldery	99D	7	2509131	2p7nw	nc089	1974	1:20000
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, stony	CuD	21507	547055	lc7y	nc099	1991	1:12000
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, stony	CuE	11257	547056	lc7z	nc099	1991	1:12000
Cullasaja-Tuckasegee complex, 8 to 15 percent slopes, stony	CuC	3277	547054	lc7x	nc099	1991	1:12000
Cullasaja very cobbly fine sandy loam, 30 to 50 percent slopes, extremely bouldery	CsE	965	547053	lc7w	nc099	1991	1:12000
Cullasaja-Tuckasegee complex, 50 to 90 percent slopes, stony	CuF	503	547057	lc80	nc099	1991	1:12000
Cullasaja very cobbly fine sandy loam, 15 to 30 percent slopes, extremely bouldery	CsD	241	547052	lc7v	nc099	1991	1:12000
Cullasaja-Tusquitee complex, 10 to 45 percent slopes	CuE	1771	547184	lcd3	nc111	1989	1:24000
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, stony	CuD	18847	545818	l9z1	nc113	1990	1:12000
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, stony	CuE	8623	545819	l9z2	nc113	1990	1:12000
Tuckasegee-Cullasaja complex, 8 to 15 percent slopes, stony	TsC	1681	545876	lb0x	nc113	1990	1:12000
Cullasaja very cobbly fine sandy loam, 30 to 50 percent slopes, extremely bouldery	CsE	670	545817	l9z0	nc113	1990	1:12000
Cullasaja very cobbly fine sandy loam, 15 to 30 percent slopes, extremely bouldery	CsD	307	545816	l9yz	nc113	1990	1:12000
Cullasaja-Tuckasegee complex, 50 to 95 percent slopes, stony	CuF	144	545820	l9z3	nc113	1990	1:12000
Cullasaja cobbly fine sandy loam, 8 to 30 percent slopes, very bouldery	CsD	1157	547558	lcs5	nc121	1997	1:12000
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, very stony	101E	4003	2501801	2q8m9	nc175	1968	1:15840
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, very stony	101D	3709	2501800	2q8m8	nc175	1968	1:15840
Cullasaja-Tuckasegee complex, 8 to 15 percent slopes, stony	101C	686	2501799	2q8m7	nc175	1968	1:15840
Cullasaja very cobbly fine sandy loam, 30 to 50 percent slopes, extremely bouldery	99E	627	2501797	2q8m6	nc175	1968	1:15840
Cullasaja very cobbly fine sandy loam, 15 to 30 percent slopes, extremely bouldery	99D	201	2501796	2q8m5	nc175	1968	1:15840
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, very stony	HdE	140	2390385	2l7d6	nc175	1968	1:15840
Cullasaja very cobbly fine sandy loam, 30 to 50 percent slopes, extremely bouldery	Sc	99	2390394	2l7dh	nc175	1968	1:15840
Cullasaja-Tuckasegee complex, 50 to 95 percent slopes, very stony	101F	85	2501802	2q8mb	nc175	1968	1:15840
Cullasaja-Tuckasegee complex, windswept, 30 to 50 percent slopes, very bouldery	102E	32	2501866	2q8mf	nc175	1968	1:15840
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, very stony	HdF	24	2390386	2l7d7	nc175	1968	1:15840
Cullasaja-Tuckasegee complex, windswept, 15 to 30 percent slopes, very bouldery	102D	20	2501865	2q8md	nc175	1968	1:15840
Cullasaja very cobbly fine sandy loam, 8 to 15 percent slopes, extremely bouldery	99C	7	2501850	2q8mc	nc175	1968	1:15840
Cullasaja very cobbly loam, 15 to 30 percent slopes, very stony	CsD	8943	563313	lx5d	nc189	2001	1:12000
Cullasaja very cobbly loam, 30 to 50 percent slopes, very stony	CsE	7353	563314	lx5f	nc189	2001	1:12000
Cullasaja very cobbly loam, 30 to 50 percent slopes, extremely bouldery	CtE	3953	563320	lx5m	nc189	2001	1:12000
Cullasaja very cobbly loam, 8 to 15 percent slopes, very stony	CsC	3915	563312	lx5c	nc189	2001	1:12000
Cullasaja very cobbly loam, 15 to 30 percent slopes, extremely bouldery	CtD	2594	563319	lx5l	nc189	2001	1:12000
Cullasaja very cobbly loam, 8 to 15 percent slopes, extremely bouldery	CtC	449	563317	lx5j	nc189	2001	1:12000
Cullasaja cobbly loam, 30 to 50 percent slopes, extremely bouldery	CrE	91	563298	lx4x	nc189	2001	1:12000
Cullasaja cobbly loam, 15 to 30 percent slopes, extremely bouldery	CrD	38	563286	lx4j	nc189	2001	1:12000
Cullasaja cobbly loam, 8 to 15 percent slopes, extremely bouldery	CrC	30	563281	lx4c	nc189	2001	1:12000
Cullasaja very cobbly sandy loam, 15 to 60 percent slopes, extremely bouldery	CuE	770	1383427	1hfkp	nc193	1993	1:24000
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, very stony	CtD	1640	1912607	22670	nc605	2007	1:12000
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, very stony	CtE	1403	1912608	22671	nc605	2007	1:12000
Cullasaja-Tuckasegee-Cruso complex, 8 to 15 percent slopes, very stony	CsC	317	622562	nwtn	nc605	2007	1:12000
Tuckasegee-Cullasaja complex, 15 to 30 percent slopes, very stony	TuD	4494	546815	lc06	nc606	1991	1:12000
Tuckasegee-Cullasaja complex, 30 to 50 percent slopes, extremely stony	TvE	3299	546816	lc07	nc606	1991	1:12000
Cullasaja very cobbly loam, 30 to 50 percent slopes, extremely bouldery	CtE	612	546756	lby9	nc606	1991	1:12000
Cullasaja very cobbly loam, 15 to 30 percent slopes, extremely bouldery	CtD	395	546755	lby8	nc606	1991	1:12000
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, very stony	101E	48	2509028	2q1w6	nc606	1991	1:12000
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, very stony	101D	15	2509027	2q1w5	nc606	1991	1:12000
Cullasaja-Tuckasegee complex, windswept, 30 to 50 percent slopes, very bouldery	102E	8	2509091	2q1w7	nc606	1991	1:12000
Cullasaja very cobbly loam, 15 to 30 percent slopes, very stony	CuD	478	526526	knwq	tn091	2000	1:24000
Cullasaja-Tuckasegee complex, 30 to 50 percent slopes, very stony	CuE	364	553546	ll0b	tn640	2007	1:24000
Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, very stony	CuD	253	553547	ll0c	tn640	2007	1:24000
Cullasaja-Rubble land complex, 50 to 95 percent slopes, extremely stony	CuF	72	561378	lv4z	tn640	2007	1:24000
Tuckasegee-Cullasaja complex, 8 to 15 percent slopes, stony	TuC	17	553534	lkzy	tn640	2007	1:24000
Tuckasegee-Cullasaja complex, 15 to 30 percent slopes, very stony	TuD	1	3244657	lc06	tn640	2007	1:24000
Cullasaja-Tuckasegee complex, 15 to 25 percent slopes, very stony	13D	2105	581968	mjl5	va067	2004	1:24000
Cullasaja-Tuckasegee complex, 25 to 60 percent slopes, very stony	13E	1849	581969	mjl6	va067	2004	1:24000
Cullasaja-Tuckasegee-Dellwood complex, 0 to 15 percent slopes, very stony	14C	362	581971	mjl8	va067	2004	1:24000
Cullasaja cobbly loam, 7 to 15 percent slopes, very stony	18C	10	1670572	1t2cf	va077	2006	1:24000
Cullasaja cobbly loam, 15 to 35 percent slopes, very stony	18D	1	1612539	1r3zd	va077	2006	1:24000
Tuckasegee-Cullasaja complex, 15 to 25 percent slopes, very stony	47D	1063	1473808	1lgm6	va141	2008	1:24000
Tuckasegee-Cullasaja complex, 25 to 45 percent slopes, very stony	47E	525	1473809	1lgm7	va141	2008	1:24000
Tuckasegee-Cullasaja complex, 8 to 15 percent slopes, very stony	47C	209	1473807	1lgm5	va141	2008	1:24000
Cullasaja-Tuckasegee complex, 15 to 35 percent slopes, very stony	11	1289	2409549	2lwbd	va606		1:24000
Cullasaja-Tuckasegee complex, 7 to 15 percent slopes, very stony	10M	431	2409550	2lwbf	va606		1:24000
Cullasaja-Tuckasegee complex, 35 to 60 percent slopes, very stony	12	430	2409548	2lwbc	va606		1:24000

Map of Series Extent

Approximate geographic distribution of the CULLASAJA 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 2024-10-30).