Official Series Description


Lab Data Summary

Aggregate lab data for the ENTIC CRYANDEPTS soil series. This aggregation is based on all pedons with a current taxon name of ENTIC CRYANDEPTS, 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 ENTIC CRYANDEPTS were used in the calculation. Source: KSSL snapshot . 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 ENTIC CRYANDEPTS 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 ENTIC CRYANDEPTS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the ENTIC CRYANDEPTS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the ENTIC CRYANDEPTS 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 .

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 ENTIC CRYANDEPTS share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the ENTIC CRYANDEPTS series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the ENTIC CRYANDEPTS 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 .

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 ENTIC CRYANDEPTS, 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 .

This figure is not available.

Block Diagrams

No block diagrams are available.

Map Units

Map units containing ENTIC CRYANDEPTS 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
Entic Cryandepts, gently sloping mountain slopes32AH5337201014496131npid60919891:24000
Entic Cryandepts, moderately steep mountain slopes32C65229801014494131nmid60919891:24000
Entic Cryandepts-Typic Cryandepts complex, high relief rolling uplands24C8B228391014367131jjid60919891:24000
Entic Cryandepts-Typic Cryandepts complex, dissected mountain slopes31C8B144911014435131lqid60919891:24000
Entic Cryandepts-Typic Cryandepts complex, steep dissected mounain slopes31D8B142791014483131n8id60919891:24000
Entic Cryandepts-Typic Cryandepts complex, low relief rolling uplands22A8B71011014352131j1id60919891:24000
Entic Cryandepts-Typic Cryandepts complex, gently sloping mountain slopes32A8B45281014497131nqid60919891:24000
Entic Cryandepts-Typic Cryandepts complex, mountain slopes32C8B30671014493131nlid60919891:24000
Entic Cryandepts, gently sloping moraines46AH519501014518131pdid60919891:24000
Dystric Cryochrepts-Entic Cryandepts complex, steep glacial trough walls48DH711671014519131pfid60919891:24000
Dystric Cryochrepts-Entic Cryandepts complex, undissected stream breaklands60E678481014537131q0id60919891:24000
Entic Cryandepts-Typic Cryandepts complex, dissected mountain slopes31C8B29082686420131lqid61819651:24000
Entic Cryandepts-Typic Cryandepts complex, gently sloping mountain slopes32A8B17452686429131nqid61819651:24000
Entic Cryandepts-Typic Cryandepts complex, steep dissected mounain slopes31D8B12242686427131n8id61819651:24000
Entic Cryandepts-Typic Cryandepts complex, mountain slopes32C8B6582686431131nlid61819651:24000
Entic Cryandepts, gently sloping mountain slopes32AH55702686430131npid61819651:24000
Entic Cryandepts-Typic Cryandepts complex, low relief rolling uplands22A8B5632686399131j1id61819651:24000
Entic Cryandepts-Typic Cryandepts complex, high relief rolling uplands24C8B3472686408131jjid61819651:24000
Entic Cryandepts, gently sloping moraines46AH5252686439131pdid61819651:24000
Entic Cryandepts, mountain slopes32U603749526865102s1wnid67119891:24000
Entic Cryandepts-Typic Cryandepts complex, mountain slopes32U953253826865152s1wtid67119891:24000
Entic Cryandepts, undissected mountain slopes34U663020626865222s1x1id67119891:24000
Typic Cryandepts-Entic Cryandepts complex, nivational hollows36U922329926865272s1x6id67119891:24000
Entic Cryandepts-Typic Cryandepts complex, high relief rolling uplands24G952053826864782s1vmid67119891:24000
Entic Cryandepts, glaciated mountain ridges38L661724726865282s1x7id67119891:24000
Entic Cryandepts-Andic Cryumbrepts complex, glaciated mountain slopes32L911564626865062s1wjid67119891:24000
Entic Cryandepts, mountain slopes, cool32U661466126865122s1wqid67119891:24000
Entic Cryandepts, glaciated mountain slopes32L661398826865052s1whid67119891:24000
Typic Cryandepts-Entic Cryandepts complex, mountain ridges33U951096926865212s1x0id67119891:24000
Typic Cryandepts-Entic Cryandepts complex, breakland drainage heads63U921070726865882spwxid67119891:24000
Entic Cryandepts, undissected stream breaklands60U60563326865542spvtid67119891:24000
Entic Cryandepts, mountain slopes, moderately well weathered granitic substratum32K66545926865042s1wgid67119891:24000
Entic Cryandepts, mountain slopes, mica schist substratum32S60540826865082s1wlid67119891:24000
Entic Cryandepts-Typic Cryandepts complex, low relief rolling uplands22G95528626864662s1v7id67119891:24000
Entic Cryandepts, dissected stream breaklands61U60472226865752spwhid67119891:24000
Entic Cryandepts-Typic Cryandepts complex, glaciated mountain ridges38L91362626865292s1x8id67119891:24000
Entic Cryandepts, dissected stream breaklands, cool61U66359626865772spwkid67119891:24000
Entic Cryandepts, undissected stream breaklands, cool60U66320326865562spvwid67119891:24000
Entic Cryandepts-Typic Cryandepts complex, mountain slopes, mica schist substratum32S95254826865092s1wmid67119891:24000
Entic Cryandepts, nivational hollows36L66183426865262s1x5id67119891:24000
Entic Cryandepts, mountain slopes, well weathered quartzite substratum32R66173926865072s1wkid67119891:24000
Entic Cryandepts, dissected stream breaklands, mica schist substratum61S6046426865712spwcid67119891:24000
Cirqueland-Entic Cryandepts complex, very steep72167808617087nq41mt61919881:24000
Andic Cryochrepts-Entic Cryandepts-Rock outcrop complex, cirque basins21-863588616077np2gmt61919881:24000
Andic Cryochrepts-Entic Cryandepts-Rock outcrop complex, cirque basins, steep21-925278616078np2hmt61919881:24000

Map of Series Extent

Approximate geographic distribution of the ENTIC CRYANDEPTS 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 .