Soil Data Explorer - CRYUMBREPTS

Official Series Description

Lab Data Summary

Aggregate lab data for the CRYUMBREPTS soil series. This aggregation is based on all pedons with a current taxon name of CRYUMBREPTS, 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 CRYUMBREPTS were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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 CRYUMBREPTS 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.

There are insufficient data to create the water balance bar figure.

There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the CRYUMBREPTS 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).

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the CRYUMBREPTS 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CRYUMBREPTS 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 2D hillslope position figure.

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

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 CRYUMBREPTS 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).

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the CRYUMBREPTS 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CRYUMBREPTS 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 2D hillslope position figure.

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

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.

Soil series sharing subgroup-level classification with CRYUMBREPTS, 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).

This figure is not available.

Block Diagrams

No block diagrams are available.

Map Units

Map units containing CRYUMBREPTS 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
Rock outcrop-Cryumbrepts association, extremely steep	183	58150	50313	1pc0	ak600	1996	1:24000
Tallac-Cryumbrepts, wet complex, 2 to 30 percent slopes	TBE	28334	464807	hlns	ca719	1982	1:24000
Jocal-Jocal variant-Cryumbrepts, wet complex, 50 to 75 percent s lopes	JZG	18562	464714	hlks	ca719	1982	1:24000
Rock outcrop, metamorphic-Tinker-Cryumbrepts, wet complex, 30 to 75 percent slopes	MMRG	15518	464756	hlm4	ca719	1982	1:24000
Waca-Meiss-Cryumbrepts, wet complex, 30 to 50 percent slopes	WEF	13499	464836	hlpq	ca719	1982	1:24000
Tinker-Rock outcrop, granitic-Cryumbrepts, wet complex, 2 to 30 percent slopes	TIE	13153	464810	hlnw	ca719	1982	1:24000
Rock outcrop, granitic-Tinker-Cryumbrepts, wet complex, 30 to 75 percent slopes	RSG	12258	464789	hln6	ca719	1982	1:24000
Meiss-Waca-Cryumbrepts, wet complex, 30 to 75 percent slopes	MLG	11598	464752	hlm0	ca719	1982	1:24000
Crozier-Mariposa-Cryumbrepts, wet complex, 30 to 75 percent slopes	CUG	10766	464637	hlh9	ca719	1982	1:24000
Rock outcrop, granitic-Tinker-Cryumbrepts, wet complex, 2 to 30 percent slopes	RSE	9966	464788	hln5	ca719	1982	1:24000
Waca-Meiss-Cryumbrepts, wet complex, 2 to 30 percent slopes	WEE	9484	464835	hlpp	ca719	1982	1:24000
Tinker-Rock outcrop, granitic-Cryumbrepts, wet complex, 30 to 75 percent slopes	TIG	9005	464811	hlnx	ca719	1982	1:24000
Waca-Cryumbrepts, wet-Windy complex, 2 to 30 percent slopes	WBE	6146	464830	hlpj	ca719	1982	1:24000
Tallac-Cryumbrepts, wet complex, 30 to 50 percent slopes	TBF	5555	464808	hlnt	ca719	1982	1:24000
Tinker-Rock outcrop, metamorphic-Cryumbrepts, wet complex, 2 to 30 percent slopes	XRE	5546	464842	hlpx	ca719	1982	1:24000
Smokey-Lorack-Cryumbrepts, wet complex, 2 to 30 percent slopes	SOE	5494	464799	hlnj	ca719	1982	1:24000
Meiss-Waca-Cryumbrepts, wet complex, 2 to 30 percent slopes	MLE	4544	464751	hllz	ca719	1982	1:24000
Smokey-Lorack-Cryumbrepts, wet complex, 30 to 50 percent slopes	SOF	4140	464800	hlnk	ca719	1982	1:24000
Ahart-Waca, rhyolitic substratum-Cryumbrepts, wet complex, 2 to 30 percent slopes	ADE	3925	464602	hlg5	ca719	1982	1:24000
Rock outcrop, metamorphic-Tinker-Cryumbrepts, wet complex, 2 to 30 percent slopes	MMRE	3798	464755	hlm3	ca719	1982	1:24000
Waca-Gullied land-Cryumbrepts, wet complex, 30 to 50 percent slo pes	WCF	3703	464832	hlpl	ca719	1982	1:24000
Ahart-Waca, rhyolitic substratum-Cryumbrepts, wet complex, 30 to 50 percent slopes	ADF	3621	464603	hlg6	ca719	1982	1:24000
Chaix variant-Rock outcrop-Cryumbrepts, wet complex, 30 to 50 percent slopes	CKF	3568	464623	hlgv	ca719	1982	1:24000
Putt-Rock outcrop-Cryumbrepts, wet complex, 2 to 30 percent slop es	PTE	3465	464770	hlml	ca719	1982	1:24000
Tahoma variant-Hotaw variant-Cryumbrepts, wet complex, 2 to 30 p ercent slopes	MUE	3383	464763	hlmc	ca719	1982	1:24000
Tinker-Rock outcrop, metamorphic-Cryumbrepts, wet complex, 30 to 50 percent slopes	XRF	2941	464843	hlpy	ca719	1982	1:24000
Lorack-Smokey-Cryumbrepts, wet complex, 2 to 30 percent slopes	LOE	2666	464734	hllf	ca719	1982	1:24000
Ledford variant-Ledford-Cryumbrepts, wet complex, 30 to 50 percent slopes	LDF	2338	464733	hlld	ca719	1982	1:24000
Celio variant-Rock outcrop-Cryumbrepts, wet complex, 30 to 50 percent slopes	GBF	1833	464669	hljb	ca719	1982	1:24000
Bucking-Bucking variant-Cryumbrepts, wet complex, 2 to 30 percent slopes	BDE	1582	464612	hlgh	ca719	1982	1:24000
Jorge-Cryumbrepts, wet-Tahoma complex, 2 to 30 percent slopes	JSE	1570	464701	hlkc	ca719	1982	1:24000
Lorack-Smokey-Cryumbrepts, wet complex, 30 to 50 percent slopes	LOF	1334	464735	hllg	ca719	1982	1:24000
Jorge-Waca-Cryumbrepts, wet complex, 2 to 30 percent slopes	JXE	1319	464709	hlkm	ca719	1982	1:24000
Bucking-Bucking variant-Cryumbrepts, wet complex, 30 to 50 percent slopes	BDF	1277	464613	hlgj	ca719	1982	1:24000
Tallac-Gullied land-Cryumbrepts, wet complex, 30 to 60 percent s lopes	THF	1217	464809	hlnv	ca719	1982	1:24000
Tahoma variant-Hotaw variant-Cryumbrepts, wet complex, 30 to 75 percent slopes	MUF	1059	464764	hlmd	ca719	1982	1:24000
Umpa-Cryumbrepts, wet complex, 2 to 30 percent slopes	UNE	1017	464823	hlp9	ca719	1982	1:24000
Cryumbrepts, wet, 2 to 15 percent slopes	CYD	965	464617	hlgn	ca719	1982	1:24000
Rouen variant-Cryumbrepts, wet-Aspen variant complex, 2 to 30 pp ercent slopes	TXE	866	464819	hlp5	ca719	1982	1:24000
Haypress-Toiyabe-Cryumbrepts, wet complex, 30 to 75 percent slopes	HBG	736	464678	hljm	ca719	1982	1:24000
Chaix variant-Rock outcrop-Cryumbrepts, wet complex, 2 to 30 percent slopes	CKE	690	464622	hlgt	ca719	1982	1:24000
Hotaw, rhyolitic substratum-McCarthy-Cryumbrepts, wet complex, 3 0 to 75 percent slopes	HTF	633	464688	hljy	ca719	1982	1:24000
Gefo variant-Cryumbrepts, wet complex, 2 to 15 percent slopes	GID	576	464672	hljf	ca719	1982	1:24000
Trojan-Sattley-Cryumbrepts, wet complex, 2 to 30 percent slopes	TUE	512	464815	hlp1	ca719	1982	1:24000
Ledford-Ledford variant-Cryumbrepts, wet complex, 2 to 30 percen t slopes	LDE	491	464732	hllc	ca719	1982	1:24000
Jorge-Waca-Cryumbrepts, wet complex, 30 to 50 percent slopes	JXF	485	464710	hlkn	ca719	1982	1:24000
Putt-Rock outcrop-Cryumbrepts, wet complex, 30 to 75 percent slo pes	PTG	428	464771	hlmm	ca719	1982	1:24000
Haypress-Toiyabe-Cryumbrepts, wet complex, 2 to 30 percent slopes	HBE	419	464677	hljl	ca719	1982	1:24000
Jorge-Cryumbrepts, wet complex, 30 to 75 percent slopes	JSG	316	464702	hlkd	ca719	1982	1:24000
Zeibright-Putt-Cryumbrepts, wet complex, 30 to 60 percent slopes	ZFF	279	464848	hlq3	ca719	1982	1:24000
Rock outcrop-Cryumbrepts association, 15 to 75 percent slopes	199	17375	464948	hltb	ca724	1985	1:24000
Xerumbrepts-Cryumbrepts, wet association, 5 to 50 percent slopes	220	15697	464969	hlv0	ca724	1985	1:24000
Tinker-Rock outcrop, granitic-Cryumbrepts, wet complex, 2 to 30 percent slopes	TIEtf	14922	1591355	1qdy1	ca724	1985	1:24000
Rock outcrop, granitic-Tinker-Cryumbrepts, wet complex, 30 to 75 percent slopes	RSGtf	13087	1591353	1qdxz	ca724	1985	1:24000
Cryumbrepts association, 5 to 50 prcent slopes	120	12572	464870	hlqt	ca724	1985	1:24000
Tinker-Rock outcrop, granitic-Cryumbrepts, wet complex, 30 to 75 percent slopes	TIGtf	11130	1591357	1qdy3	ca724	1985	1:24000
Tallac-Cryumbrepts, wet association, 15 to 30 percent slopes	203	4290	464952	hltg	ca724	1985	1:24000
Waca-Lithic Cryumbrepts-Cryumbrepts, wet association 5 to 30 percent slopes	214	1752	464963	hltt	ca724	1985	1:24000
Waca-Lithic Cryumbrepts-Cryumbrepts, wet association, 30 to 50 percent slopes	215	336	464964	hltv	ca724	1985	1:24000
Tinker-Cryumbrept, wet-Rock outcrop association, 2 to 30 percent slopes	206	220	464955	hltk	ca724	1985	1:24000
Xerumbrepts-Cryumbrepts, wet association, 5 to 50 percent slopes	220ef	87	1670106	1t1wd	ca731	1981	1:24000
Cryumbrepts very bouldery-Cryumbrepts very gravelly association, 2 to 30 percent slopes	178	716	488071	jcw7	ca802	1996	1:24000
Cryumbrepts-Rock outcrop-Rubble land complex, 20 to 80 percent slopes	129	68986	2453674	2nc7s	co664	1987	1:24000
Cryumbrepts-Cryaquepts-Andic Cryochrepts complex, stream bottoms	10AD9	8632	1014344	131hs	id609	1989	1:24000
Cryaquepts-Cryumbrepts complex, stream bottoms	10A99	5517	1014342	131hq	id609	1989	1:24000
Cryandepts-Cryumbrepts complex, glacial trough bottoms	47A66	4506	1014524	131pl	id609	1989	1:24000
Cryaquepts-Cryumbrepts complex, stream bottoms	10A99	419	2686390	131hq	id618	1965	1:24000
Cryumbrepts-Cryaquepts-Andic Cryochrepts complex, stream bottoms	10AD9	23	2686391	131hs	id618	1965	1:24000
Cryumbrepts, very steep	26F	6757	469452	hrhm	or033	1979	1:20000
Cryumbrepts, gently rolling	29	854	68995	29sn	wa677	1979	1:24000

Map of Series Extent

Approximate geographic distribution of the CRYUMBREPTS 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).