Soil Data Explorer - CREEDMOOR

Official Series Description

Lab Data Summary

Aggregate lab data for the CREEDMOOR soil series. This aggregation is based on all pedons with a current taxon name of CREEDMOOR, 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 CREEDMOOR 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
136	83P0548	83NC125005	Creedmoor	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.3833351,-79.4499969
136	87P0413	87NC007001	Creedmoor	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.9963875,-80.206665
136	88P0665	88NC077003	Creedmoor	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1133347,-78.7166672
136	40A1304	S1969VA075014	CREEDMOOR	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.5917206,-77.649704
136	81P0635	S1981NC105001A	CREEDMOOR	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5000954,-79.2497559
136	81P0636	S1981NC105001B	CREEDMOOR	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5028763,-79.2497559
136	81P0637	S1981NC105001C	CREEDMOOR	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5167618,-79.2497559
136	81P0638	S1981NC105001D	Creedmoor	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5000954,-79.2497559
136	81P0639	S1981NC105001E	Creedmoor	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5000954,-79.2497559
136	81P0640	S1981NC105001F	Creedmoor	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5000954,-79.2497559
136	81P0641	S1981NC105001G	Creedmoor	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5000954,-79.2497559
136	81P0642	S1981NC105001H	Creedmoor	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5000954,-79.2497559
136	81P0643	S1981NC105001I	CREEDMOOR	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5000954,-79.2497559
136	82P0317	S1981NC157006	Creedmoor	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.333416,-79.7497711
136	82P0318	S1981NC157007	CREEDMOOR	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.333416,-79.7497711

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CREEDMOOR 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 CREEDMOOR 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 CREEDMOOR 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 CREEDMOOR 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 CREEDMOOR 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 CREEDMOOR 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 CREEDMOOR 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 mountains figure.

Soil series sharing subgroup-level classification with CREEDMOOR, 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

No block diagrams are available.

Map Units

Map units containing CREEDMOOR 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
Creedmoor fine sandy loam, 2 to 8 percent slopes	CrB	14049	114509	3v4v	nc007	1999	1:24000
Creedmoor-Green Level complex, 2 to 6 percent slopes	CrB	20119	1485534	1lvtg	nc037	2005	1:24000
Creedmoor-Green Level complex, 6 to 10 percent slopes	CrC	14571	1485536	1lvtj	nc037	2005	1:24000
Creedmoor-Green Level complex, 10 to 15 percent slopes	CrD	4884	1485532	1lvtd	nc037	2005	1:24000
Creedmoor sandy loam, 2 to 6 percent slopes	CrB	6047	112305	3rvr	nc063	1971	1:15840
Creedmoor sandy loam, 6 to 10 percent slopes	CrC	2630	112306	3rvs	nc063	1971	1:15840
Creedmoor coarse sandy loam, 2 to 6 percent slopes	CrB	27578	112759	3sbd	nc077	1993	1:24000
Creedmoor coarse sandy loam, 6 to 10 percent slopes	CrC	12604	112760	3sbf	nc077	1993	1:24000
Urban land-Iredell-Creedmoor complex, 2 to 10 percent slopes	UrC	1779	112785	3sc7	nc077	1993	1:24000
Creedmoor fine sandy loam, 2 to 8 percent slopes	CrB	4057	113580	3t5w	nc105	1982	1:24000
Creedmoor fine sandy loam, 8 to 15 percent slopes	CrD	833	113581	3t5x	nc105	1982	1:24000
Creedmoor-Brickhaven complex, 2 to 8 percent slopes	CrB	3388	2233565	2dz6h	nc123	2007	1:24000
Creedmoor fine sandy loam, 2 to 6 percent slopes	CrB	2210	113897	3tj3	nc125	1987	1:24000
Creedmoor fine sandy loam, 6 to 10 percent slopes	CrC	864	113898	3tj4	nc125	1987	1:24000
Creedmoor fine sandy loam, 2 to 8 percent slopes	CrB	784	114097	3tqk	nc135	1975	1:20000
Creedmoor fine sandy loam, 2 to 8 percent slopes	CrB	3137	114700	3vc0	nc153	1996	1:24000
Creedmoor loam, 2 to 8 percent slopes	CrB	1328	115345	3w0t	nc179	1991	1:24000
Creedmoor-Green Level complex, 10 to 15 percent slopes	CrD	21709	2538475	2qqfp	nc183	1966	1:24000
Creedmoor-Green Level complex, 2 to 6 percent slopes	CrB	15556	2538476	2qqfq	nc183	1966	1:24000
Creedmoor-Green Level complex, 6 to 10 percent slopes	CrC	10423	2538478	2qqfs	nc183	1966	1:24000
Creedmoor-Green Level-Urban land complex, 2 to 10 percent slopes	CuC	7267	3050248	2xh9q	nc183	1966	1:24000
Creedmoor fine sandy loam, 2 to 7 percent slopes	8B	3269	118205	3z02	va007	1994	1:24000
Brickhaven-Creedmoor complex, 2 to 7 percent slopes	9B	2130	2479369	2p6zn	va029	2010	1:24000
Brickhaven-Creedmoor complex, 7 to 15 percent slopes	9C	1404	2479371	2p6zq	va029	2010	1:24000
Creedmoor sandy loam, 2 to 6 percent slopes, eroded	CsB2	681	118714	3zjh	va037	1970	1:15840
Creedmoor sandy loam, 6 to 10 percent slopes, eroded	CsC2	379	118715	3zjj	va037	1970	1:15840
Creedmoor fine sandy loam, 2 to 6 percent slopes	61B	15691	118923	3zr7	va041	1974	1:15840
Mayodan, clayey substratum-Creedmoor sandy loams, 6 to 12 percent slopes	201C	6148	118860	3zp6	va041	1974	1:15840
Creedmoor fine sandy loam, 6 to 12 percent slopes	61C	4046	118924	3zr8	va041	1974	1:15840
Mayodan, clayey substratum-Creedmoor sandy loams, 12 to 20 percent slopes	201D	1572	118861	3zp7	va041	1974	1:15840
Mayodan-Creedmoor-Edgehill very gravelly sandy loams, 2 to 12 percent slopes	251C	1104	118880	3zpv	va041	1974	1:15840
Mayodan-Creedmoor-Edgehill very gravelly sandy loams, 20 to 40 percent slopes	251F	958	118882	3zpx	va041	1974	1:15840
Mayodan-Creedmoor-Edgehill very gravelly sandy loams, 12 to 20 percent slopes	251D	954	118881	3zpw	va041	1974	1:15840
Creedmoor gravelly fine sandy loam, 6 to 12 percent slopes	123C	714	118826	3zn3	va041	1974	1:15840
Creedmoor gravelly fine sandy loam, 2 to 6 percent slopes	123B	687	118825	3zn2	va041	1974	1:15840
Creedmoor fine sandy loam, 6 to 12 percent slopes, eroded	61C2	659	118925	3zr9	va041	1974	1:15840
Mayodan, clayey substratum-Creedmoor sandy loams, 2 to 6 percent slopes	201B	475	118859	3zp5	va041	1974	1:15840
Creedmoor-Worsham sandy loams, 6 to 12 percent percent slopes	202C	282	118864	3zpb	va041	1974	1:15840
Creedmoor-Worsham sandy loams, 2 to 6 percent slopes	202B	19	118863	3zp9	va041	1974	1:15840
Brickhaven-Creedmoor complex, 2 to 7 percent slopes	5B	7552	1587395	1q8t9	va049	2005	1:24000
Brickhaven-Creedmoor complex, 7 to 15 percent slopes	5C	2295	1587396	1q8tb	va049	2005	1:24000
Creedmoor fine sandy loam, 2 to 7 percent slopes	8B	2353	119062	3zwq	va075	1976	1:15840
Creedmoor fine sandy loam, 2 to 7 percent slopes, eroded	8B2	1304	119063	3zwr	va075	1976	1:15840
Creedmoor fine sandy loam, 7 to 15 percent slopes, eroded	8C2	1199	119065	3zwt	va075	1976	1:15840
Creedmoor fine sandy loam, 7 to 15 percent slopes	8C	366	119064	3zws	va075	1976	1:15840
Mayodan-Creedmoor complex, 2 to 7 percent slopes	45B	1395	119123	3zyp	va085	1976	1:15840
Creedmoor fine sandy loam, 2 to 7 percent slopes	19B	600	119086	3zxh	va085	1976	1:15840
Creedmoor variant fine sandy loam, 2 to 7 percent slopes	20B	350	119089	3zxl	va085	1976	1:15840
Creedmoor sandy loam, 2 to 6 percent slopes, eroded	CvB2	529	119224	401y	va087	1973	1:15840
Creedmoor sandy loam, 2 to 6 percent slopes	CvB	420	119223	401x	va087	1973	1:15840
Creedmoor sandy loam, 6 to 10 percent slopes, eroded	CvC2	250	119225	401z	va087	1973	1:15840
Creedmoor fine sandy loam, 1 to 4 percent slopes	7B	17	122396	43c8	va089	1995	1:24000
Calverton and Creedmoor silt loams, 0 to 7 percent slopes	CbB	531	516940	kbxh	va113	1967	1:15840
Creedmoor fine sandy loam, 2 to 7 percent slopes	9B	3280	120217	412z	va145	1984	1:15840
Creedmoor fine sandy loam, undulating phase	Ct	1434	120250	4141	va147	1950	1:20000
Creedmoor fine sandy loam, rolling phase	Cs	393	120249	4140	va147	1950	1:20000
Creedmoor fine sandy loam, eroded rolling phase	Cr	281	120248	413z	va147	1950	1:20000

Map of Series Extent

Approximate geographic distribution of the CREEDMOOR 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).