Soil Data Explorer - REDRAVEN

Official Series Description

Lab Data Summary

Aggregate lab data for the REDRAVEN soil series. This aggregation is based on all pedons with a current taxon name of REDRAVEN, 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 REDRAVEN 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
n/a	92P0282	92ID079004	Redraven	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 REDRAVEN 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 REDRAVEN 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 REDRAVEN 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 REDRAVEN 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 terrace figure.

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

Competing Series

Soil series competing with REDRAVEN 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 REDRAVEN 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 REDRAVEN 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 terrace figure.

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

Soil series sharing subgroup-level classification with REDRAVEN, 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 REDRAVEN 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
Redraven medial silt loam, 35 to 65 percent slopes, bouldery	155	1246	152850	541n	id601	2002	1:24000
Redraven medial silt loam, 15 to 35 percent slopes	154	225	152849	541m	id601	2002	1:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 20 to 40 percent slopes	2lg2x	37	2850804	2lg2x	id601	2002	1:24000
Redraven-Roman-Molly families, complex, glaciated ridges, granitic geology	2lg2s	28	2850803	2lg2s	id601	2002	1:24000
Rock outcrop-Roman family-Molly family, complex, glaciated ridges, granitic geology	2lg2p	12	2850802	2lg2p	id601	2002	1:24000
Redraven-Rubycreek-Muddycreek families, complex, moderately steep glaciated mountain slopes, belt geology, south aspects	2lg0x	7	2850787	2lg0x	id601	2002	1:24000
Roman-Redraven-Molly families, complex, shallow incised glaciated mountain slopes, granitic geology, south aspects	2lg32	4	2850805	2lg32	id601	2002	1:24000
Redraven-Rubycreek-Muddycreek families, complex, glaciated mountain slopes, belt geology, south aspects	2lg0w	2	2850786	2lg0w	id601	2002	1:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 15 to 45 percent slopes	2lg2t	44	2850848	2lg2t	id604	1981	1:24000
Redraven-Roman-Molly families, complex, steep glaciated mountain slopes, granitic geology	2lg2w	37	2850849	2lg2w	id604	1981	1:24000
Redraven-Roman-Molly families, complex, glaciated ridges, granitic geology	2lg2s	33	2850847	2lg2s	id604	1981	1:24000
Roman-Redraven-Molly families, complex, moderately steep glaciated mountain slopes, granitic geology, south aspects	2lg2y	29	2850851	2lg2y	id604	1981	1:24000
Redraven-Roman-Molly families, complex, steep glaciated mountain slopes, granitic geology, south aspects	2lg2z	24	2850852	2lg2z	id604	1981	1:24000
Roman-Redraven-Molly families, complex, shallow incised glaciated mountain slopes, granitic geology, north aspects	2lg30	14	2850853	2lg30	id604	1981	1:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 20 to 40 percent slopes	2lg2x	12	2850850	2lg2x	id604	1981	1:24000
Rock outcrop-Molly family-Redraven family, complex, steep glaciated mountain slopes, granitic geology	2lg2r	5	2850846	2lg2r	id604	1981	1:24000
Redraven cobbly silt loam, 15 to 35 percent slopes	81	435	153499	54ql	id608	1994	1:24000
Redraven bouldery medial silt loam, 15 to 35 percent slopes	82	416	153500	54qm	id608	1994	1:24000
Redraven-Typic Fulvicryands families, complex, dissected alpine glaciated lower to mid mountain slopes, timber-brush-fern glade mosaic, south aspects	2lg1d	60	2936816	2lg1d	id608	1994	1:24000
Redraven-Typic Fulvicryands families, complex, dissected alpine glaciated lower mountain slopes, toeslopes, and bottoms, timber-brush-fern glade mosaic, north aspects	2lg1c	46	2936804	2lg1c	id608	1994	1:24000
Redraven-Handoff-Aquandic Cryaquepts familes, complex, glacial trough bottoms and toeslopes	2lg09	31	2936779	2lg09	id608	1994	1:24000
Redraven-Typic Fulvicryands families, complex, steep glacial cirque headwalls, timbered	2lg1b	26	2936796	2lg1b	id608	1994	1:24000
Redraven-Typic Fulvicryands families, complex, very steep dissected glaciated slopes, trough walls, avalanche chutes, timber-brush-fern glade mosaic, north aspects	2lg1f	25	2936788	2lg1f	id608	1994	1:24000
Redraven family-Rock outcrop-Typic Fulvicryands family, complex, steep glacial cirque headwalls	2lg19	2	2936812	2lg19	id608	1994	1:24000
Redraven-Rubycreek-Muddycreek families, complex, glaciated mountain slopes, belt geology, south aspects	224	23834	2396761	2lg0w	id670		1:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 15 to 45 percent slopes	321	21068	2396821	2lg2t	id670		1:24000
Redraven-Typic Fulvicryands families, complex, dissected alpine glaciated lower mountain slopes, toeslopes, and bottoms, timber-brush-fern glade mosaic, north aspects	243	19045	2396776	2lg1c	id670		1:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 20 to 40 percent slopes	324	18754	2396824	2lg2x	id670		1:24000
Redraven family-Rock outcrop-Typic Fulvicryands family, complex, steep glacial cirque headwalls	241	12857	2396774	2lg19	id670		1:24000
Redraven-Rubycreek-Muddycreek families, complex, moderately steep glaciated mountain slopes, belt geology, south aspects	225	9183	2396762	2lg0x	id670		1:24000
Redraven-Typic Fulvicryands families, complex, steep glacial cirque headwalls, timbered	242	8572	2396775	2lg1b	id670		1:24000
Redraven family, glaciated mountain slopes, timbered, north aspects	210	8543	2396748	2lg0g	id670		1:24000
Redraven-Handoff-Aquandic Cryaquepts familes, complex, glacial trough bottoms and toeslopes	200	8455	2396743	2lg09	id670		1:24000
Redraven-Roman-Molly families, complex, moderately steep glaciated mountain slopes, granitic geology	322	7412	2396822	2lg2v	id670		1:24000
Redraven-Typic Fulvicryands families, complex, weakly dissected glacial trough walls, timber-brush-fern glade mosaic, northerly aspects	206	6927	2396746	2lg0d	id670		1:24000
Roman-Redraven-Molly families, complex, moderately steep glaciated mountain slopes, granitic geology, south aspects	325	6260	2396825	2lg2y	id670		1:24000
Redraven-Handoff-Hydric Cryofibrists families, complex, low relief glaciated depressions, timber-brush-fern glade mosaic	211	5089	2396750	2lg0j	id670		1:24000
Redraven family, glaciated mountain slopes, timbered, south aspects	209	4832	2396747	2lg0f	id670		1:24000
Roman-Redraven-Molly families, complex, shallow incised glaciated mountain slopes, granitic geology, north aspects	331	3541	2396827	2lg30	id670		1:24000
Redraven-Typic Fulvicryands families, complex, very steep dissected glaciated slopes, trough walls, avalanche chutes, timber-brush-fern glade mosaic, north aspects	245	3518	2396778	2lg1f	id670		1:24000
Redraven-Typic Fulvicryands families, complex, dissected alpine glaciated lower to mid mountain slopes, timber-brush-fern glade mosaic, south aspects	244	3423	2396777	2lg1d	id670		1:24000
Redraven-Typic Fulvicryands families, complex, weakly weathered metasedimentary belt, glacial cirque basins	230	3378	2396765	2lg10	id670		1:24000
Redraven-Rubycreek-Muddycreek families, complex, steep shallow incised glaciated mountain slopes, belt geology, south aspects	234	3368	2396772	2lg17	id670		1:24000
Redraven-Roman-Molly families, complex, steep glaciated mountain slopes, granitic geology	323	3241	2396823	2lg2w	id670		1:24000
Typic Fulvicryands-Redraven families-Rock outcrop complex, very steep dissected glaciated slopes, trough walls, avalanche chutes, timber-brush-fern glade mosaic, south aspects	246	3171	2396779	2lg1g	id670		1:24000
Redraven-Rubycreek-Muddycreek families, complex, shallow incised glaciated mountain slopes, belt geology, south aspects	233	2830	2396771	2lg16	id670		1:24000
Rock outcrop-Roman family-Molly family, complex, glaciated ridges, granitic geology	315	2541	2396817	2lg2p	id670		1:24000
Roman-Redraven-Molly families, complex, shallow incised glaciated mountain slopes, granitic geology, south aspects	333	2416	2396829	2lg32	id670		1:24000
Redraven-Roman-Molly families, complex, steep glaciated mountain slopes, granitic geology, south aspects	326	2410	2396826	2lg2z	id670		1:24000
Redraven-Roman-Molly families, complex, glaciated ridges, granitic geology	320	2176	2396820	2lg2s	id670		1:24000
Roman-Redraven-Mollly families, complex, moderately to deeply incised draws on glaciated mountain slopes, granitic geology, south aspects	334	1995	2396830	2lg33	id670		1:24000
Roman-Redraven-Molly families, complex, moderately to deeply incised draws on glaciated mountain slopes, granitic geology, north aspects	332	1360	2396828	2lg31	id670		1:24000
Rock outcrop-Molly family-Redraven family, complex, steep glaciated mountain slopes, granitic geology	317	1135	2396819	2lg2r	id670		1:24000
Rock outcrop-Roman family-Molly family, complex, glaciated mountain slopes, granitic geology	316	1010	2396818	2lg2q	id670		1:24000
Redraven-Rubycreek-Muddycreek families, complex, steep glaciated mountain slopes, belt geology, south aspects	226	1006	2396763	2lg0y	id670		1:24000
Typic Fulvicryands-Redraven families, complex, weakly dissected glacial trough walls, timber-brush-fern glade mosaic, all aspects	205	867	2396745	2lg0c	id670		1:24000
Redraven-Handoff families, complex, stream terraces, toe slopes, and alluvial fans	136	784	2396730	2lfzw	id670		1:24000
Redraven-Typic Fulvicryands families-Rock outcrop complex, steep glacial cirque headwalls, timbered	342	771	2396833	2lg36	id670		1:24000
Redraven-Typic Fulvicryands families-Rock outcrop complex, weakly weathered metasedimentary belt, glacial cirque basins	229	655	2396764	2lg0z	id670		1:24000
Redraven medial silt loam, 35 to 65 percent slopes, bouldery	541n	99	2936735	541n	id670		1:24000
Redraven cobbly silt loam, 15 to 35 percent slopes	54ql	75	2851003	54ql	id670		1:24000
Redraven bouldery medial silt loam, 15 to 35 percent slopes	54qm	55	2851004	54qm	id670		1:24000
Rock outcrop-Roman family-Molly family, complex, glaciated ridges, granitic geology	2lg2p	99	2850947	2lg2p	wa651	1981	1:24000
Redraven-Roman-Molly families, complex, glaciated upper mountain slopes, granitic geology, 15 to 45 percent slopes	2lg2t	44	2850920	2lg2t	wa651	1981	1:24000
Rock outcrop-Roman family-Molly family, complex, glaciated mountain slopes, granitic geology	2lg2q	19	2850925	2lg2q	wa651	1981	1:24000
Redraven-Roman-Molly families, complex, glaciated ridges, granitic geology	2lg2s	8	2850954	2lg2s	wa651	1981	1:24000
Roman-Redraven-Molly families, complex, moderately to deeply incised draws on glaciated mountain slopes, granitic geology, north aspects	2lg31	3	2850952	2lg31	wa651	1981	1:24000
Redraven-Roman-Molly families, complex, moderately steep glaciated mountain slopes, granitic geology	2lg2v	2	2850938	2lg2v	wa651	1981	1:24000

Map of Series Extent

Approximate geographic distribution of the REDRAVEN 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).