Soil Data Explorer - CAMASPATCH

Official Series Description

Lab Data Summary

Aggregate lab data for the CAMASPATCH soil series. This aggregation is based on all pedons with a current taxon name of CAMASPATCH, 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 CAMASPATCH were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

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

There are insufficient data to create the 3D terrace figure.

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

Competing Series

Soil series competing with CAMASPATCH 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 CAMASPATCH 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 CAMASPATCH 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 CAMASPATCH, 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. WA-2010-11-05-02 | Douglas County - 2008

   Cross-section view of soils that formed in residuum and colluvium or loess over older loess over basalt and receive 12 to 15 inches of precipitation (Soil Survey of Douglas County, Washington; 2008).

2. WA-2010-11-05-03 | Douglas County - 2008

   Cross-section view of soils that formed in residuum and colluvium or loess and volcanic ash over older loess over basalt and receive 12 to 15 inches of precipitation (Soil Survey of Douglas County, Washington; 2008).

3. WA-2010-11-05-08 | Klickitat County - 2009

   Representative landscape cross section of the Van Nostern-Morrow-Bakeoven general soil map unit (Soil Survey of Klickitat County, Washington; 2009).

4. WA-2012-05-11-43 | Douglas County - May 2008

   Cross-section of soils that formed in residuum and colluvium or loess over older loess over basalt and receive 12 to 15 inches of precipitation (Soil Survey of Douglas County, Washington; May 2008).

5. WA-2012-05-11-44 | Douglas County - May 2008

   Cross-section of soils that formed in residuum and colluvium or loess and volcanic ash over older loess over basalt and receive 12 to 15 inches of precipitation (Soil Survey of Douglas County, Washington; May 2008).

6. WA-2012-05-11-46 | Klickitat County Area - December 2009

   Representative landscape cross-section of general soil map unit 9 (Soil Survey of Klickitat County Area, Washington; December 2009).

Map Units

Map units containing CAMASPATCH 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
Patron-Camaspatch-Rock outcrop complex, 20 to 50 percent north slopes	4006BO	126	3120155	21zl3	or607	2018	1:24000
Patron-Camaspatch-Rock outcrop complex, 20 to 50 percent north slopes	164E	3957	3426271	21zl3	or627		1:24000
Argabak-Camaspatch-Badge complex, 30 to 65 percent slopes	23	5416	699280	rgnf	wa017	1998	1:12000
Van Nostern-Argabak-Camaspatch complex, 3 to 30 percent slopes	450	4579	699541	rgxv	wa017	1998	1:12000
Jordy-Camaspatch complex, 15 to 30 percent slopes	209	675	699461	rgv8	wa017	1998	1:12000
Van Nostern-Camaspatch complex, 8 to 15 percent slopes	452	388	699493	rgw9	wa017	1998	1:12000
Jordy-Camaspatch complex, 8 to 15 percent slopes	208	215	699460	rgv7	wa017	1998	1:12000
Van Nostern-Camaspatch complex, 15 to 30 percent slopes	453	204	699494	rgwb	wa017	1998	1:12000
Van Nostern-Camaspatch complex, 3 to 8 percent slopes	451	196	699492	rgw8	wa017	1998	1:12000
Beca-Camaspatch complex, 15 to 30 percent slopes	51	126	700693	rj40	wa017	1998	1:12000
Jordy-Camaspatch complex, 3 to 8 percent slopes	207	84	699459	rgv6	wa017	1998	1:12000
Camaspatch-Boylston complex, 30 to 70 percent slopes	595	7840	77020	2l4j	wa637	2008	1:24000
Tanksel-Lainand-Camaspatch complex, 30 to 70 percent slopes	638	7380	77065	2l5z	wa637	2008	1:24000
Camaspatch very cobbly loam, 3 to 15 percent slopes	497	3787	76931	2l1n	wa637	2008	1:24000
Camaspatch-Boylston complex, 15 to 30 percent slopes	594	3537	77019	2l4h	wa637	2008	1:24000
Camaspatch-Tanksel-Rubble land complex, 45 to 75 percent slopes	890	2710	77269	2ldk	wa637	2008	1:24000
Camaspatch-Rubble land-Boylston complex, 30 to 70 percent slopes	886	2403	77264	2ldd	wa637	2008	1:24000
Tanksel-Patron-Camaspatch complex, 30 to 70 percent slopes	656	1978	77079	2l6f	wa637	2008	1:24000
Rubble land-Camaspatch-Rock outcrop complex, 30 to 70 percent slopes	893	1872	77272	2ldn	wa637	2008	1:24000
Argabak-Camaspatch complex, 3 to 15 percent slopes	896	1502	77275	2ldr	wa637	2008	1:24000
Patron-Camaspatch complex, 15 to 30 percent slopes	902	1450	77283	2lf0	wa637	2008	1:24000
Camaspatch-Boylston complex, 3 to 15 percent slopes	593	1392	77018	2l4g	wa637	2008	1:24000
Camaspatch very cobbly loam, 15 to 30 percent slopes	614	866	77039	2l54	wa637	2008	1:24000
Tanksel-Patron-Camaspatch complex, 15 to 30 percent slopes	650	774	77074	2l68	wa637	2008	1:24000
Camaspatch-Tanksel complex, 30 to 70 percent slopes	658	341	77081	2l6h	wa637	2008	1:24000
Camaspatch very cobbly silt loam, 15 to 45 percent slopes	488	651	76354	2kg1	wa639	2003	1:24000
Boylston-Camaspatch, moist complex, 12 to 35 percent slopes	3821	6680	86713	2x76	wa676	2014	1:12000
Boylston-Camaspatch, moist complex, 35 to 60 percent slopes	3822	4720	86712	2x75	wa676	2014	1:12000
Rubble land-Badge, stony-Camaspatch, dry complex, 35 to 70 percent slopes	4707	4470	86768	2x8z	wa676	2014	1:12000
Lainand, stony-Camaspatch, moist complex, 35 to 60 percent slopes	7204	3280	86785	2x9j	wa676	2014	1:12000
Badge, moist, stony-Rubble land-Camaspatch, moist, very stony complex, 35 to 70 percent slopes	4705	2560	86731	2x7s	wa676	2014	1:12000
Camaspatch very cobbly silt loam, dry, 12 to 35 percent slopes	742	2210	86313	2wt9	wa676	2014	1:12000
Camaspatch very cobbly silt loam, dry, 0 to 12 percent slopes	741	2060	86314	2wtb	wa676	2014	1:12000
Tronsen, extremely stony-Pushtay-Camaspatch, dry complex, 12 to 35 percent slopes	3307	1780	86663	2x5l	wa676	2014	1:12000
Lainand, stony-Camaspatch, moist complex, 20 to 35 percent slopes	7203	1590	86787	2x9l	wa676	2014	1:12000
Pushtay-Tronsen, extremely stony-Camaspatch, dry complex, 12 to 35 percent slopes	3404	1390	86699	2x6r	wa676	2014	1:12000
Badge, moist, stony-Rubble land-Camaspatch, moist, very stony complex 12 to 35 percent slopes	4704	1210	86732	2x7t	wa676	2014	1:12000
Pushtay-Tronsen, extremely stony-Camaspatch, dry complex, 35 to 60 percent slopes	3405	830	86698	2x6q	wa676	2014	1:12000
Rubble land-Badge, stony-Camaspatch, dry complex, 12 to 35 percent slopes	4706	760	86769	2x90	wa676	2014	1:12000
Tronsen, extremely stony-Pushtay-Camaspatch, dry complex, 35 to 60 percent slopes	3308	550	86662	2x5k	wa676	2014	1:12000
Kusipushtay, very stony-Camaspatch, dry complex, 12 to 35 percent slopes	7503	390	86781	2x9d	wa676	2014	1:12000
Van Nostern-Camaspatch, dry complex, 0 to 12 percent slopes	4508	370	86739	2x81	wa676	2014	1:12000
Pushtay-Tronsen, extremely stony-Camaspatch, dry complex, 0 to 12 percent slopes	3402	360	86700	2x6s	wa676	2014	1:12000
Kusipushtay, very stony-Camaspatch, dry complex, 0 to 12 percent slopes	7501	360	86784	2x9h	wa676	2014	1:12000
Tronsen, extremely stony-Pushtay-Camaspatch, dry complex, 0 to 12 percent slopes	3306	330	86665	2x5n	wa676	2014	1:12000
Camaspatch very cobbly silt loam, 15 to 45 percent slopes	1978	80	2485996	2pfwf	wa676	2014	1:12000
Camaspatch-Boylston complex, 30 to 45 percent slopes	44	2718	70917	2csn	wa681	1994	1:24000
Tanskel-Patron-Camaspatch complex, 15 to 30 percent slopes	150	2084	70816	2cpd	wa681	1994	1:24000
Camaspatch-Boylston complex, 15 to 30 percent slopes	43	1726	70908	2csc	wa681	1994	1:24000
Camaspatch-Tanksel-Lainand complex, 45 to 60 percent slopes	41	1635	70889	2crr	wa681	1994	1:24000
Camaspatch very cobbly loam, thin, 3 to 15 percent slopes	37	1510	70885	2crm	wa681	1994	1:24000
Patron-Camaspatch complex, 15 to 30 percent slopes	123	1209	70789	2cnj	wa681	1994	1:24000
Camaspatch very cobbly loam, 15 to 30 percent slopes	36	1185	70884	2crl	wa681	1994	1:24000
Boylston-Tronsen-Camaspatch complex, 30 to 45 percent slopes	183	1184	70852	2cqk	wa681	1994	1:24000
Camaspatch very cobbly loam, 3 to 15 percent slopes	35	1016	70883	2crk	wa681	1994	1:24000
Camaspatch-Boylston complex, 3 to 15 percent slopes	42	930	70897	2cs0	wa681	1994	1:24000
Tanksel-Patron-Camaspatch complex, 30 to 45 percent slopes	151	927	70817	2cpf	wa681	1994	1:24000
Camaspatch-Tanksel complex, 30 to 45 percent slopes	40	907	70888	2crq	wa681	1994	1:24000
Boylston-Tronsen-Camaspatch complex, 15 to 30 percent slopes	182	725	70851	2cqj	wa681	1994	1:24000
Camaspatch very cobbly loam, thin, 15 to 30 percent slopes	38	704	70886	2crn	wa681	1994	1:24000
Boylston-Tronsen-Camaspatch complex, 45 to 60 percent slopes	184	679	70853	2cql	wa681	1994	1:24000
Camaspatch-Colockum complex, 15 to 30 percent slopes	39	592	70887	2crp	wa681	1994	1:24000
Camaspatch-Boylston complex, 45 to 60 percent slopes	45	555	70926	2csy	wa681	1994	1:24000
Argabak-Camaspatch complex, 3 to 15 percent slopes	7	221	70748	2cm6	wa681	1994	1:24000

Map of Series Extent

Approximate geographic distribution of the CAMASPATCH 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).