Official Series Description


Lab Data Summary

Aggregate lab data for the ANDIC CRYOCHREPTS soil series. This aggregation is based on all pedons with a current taxon name of ANDIC CRYOCHREPTS, 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 ANDIC CRYOCHREPTS 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.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
43B08N0154S2007MT049001Andic Cryochrepts6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8423233,-112.5080185

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ANDIC CRYOCHREPTS 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 ANDIC CRYOCHREPTS 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 ANDIC CRYOCHREPTS 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 ANDIC CRYOCHREPTS 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 ANDIC CRYOCHREPTS 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 ANDIC CRYOCHREPTS 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 ANDIC CRYOCHREPTS 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 ANDIC CRYOCHREPTS, 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 ANDIC CRYOCHREPTS 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
Andic Cryochrepts-Dystric Cryochrepts complex, 45 to 60 percent slopes, dissected mountain slopes31DH733113253824131njid60019891:24000
Andic Cryochrepts-Cryaquepts complex, nivational hollows36A661242686300131nyid60019891:24000
Andic Cryochrepts-Cryaquepts complex, moderately steep nivational hollows36C661072686301131nxid60019891:24000
Andic Cryochrepts, mountain ridges33A65399401014500131ntid60919891:24000
Andic Cryochrepts, moderately steep mountain slopes32CH5378121014502131nwid60919891:24000
Andic Cryochrepts, high relief rolling uplands, warm24CH5345211014366131jhid60919891:24000
Andic Cryochrepts-Dystric Cryochrepts complex, 45 to 60 percent slopes, dissected mountain slopes31DH7319201014491131njid60919891:24000
Andic Cryochrepts, low relief rolling uplands22AH5272251014357131j6id60919891:24000
Andic Cryochrepts, dissected mountain slopes, warm31CH5257471014426131lfid60919891:24000
Andic Cryochrepts, gently sloping mountain slopes32A65204351014488131nfid60919891:24000
Andic Cryochrepts-Cryaquepts complex, low relief rolling uplands22AH6137881014356131j5id60919891:24000
Andic Cryochrepts, moderately steep mountain ridges33C65124051014498131nrid60919891:24000
Andic Cryochrepts-Cryaquepts complex, gently sloping moraines46A66120961014509131p3id60919891:24000
Andic Cryochrepts, high relief rolling uplands, weathered granitic substratum24CHX107481014418131l5id60919891:24000
Andic Cryochrepts-Cryaquepts complex, low relief rolling uplands, weathered granitic substratum22A6Q102321014354131j3id60919891:24000
Cryumbrepts-Cryaquepts-Andic Cryochrepts complex, stream bottoms10AD986321014344131hsid60919891:24000
Andic Cryochrepts-Cryaquepts complex, high relief rolling uplands, weathered granitic substratum24CHQ85741014419131l6id60919891:24000
Andic Cryochrepts-Cryaquepts complex, low relief rolling uplands, weathered granitic substratum, warm22AHQ84391014355131j4id60919891:24000
Andic Cryochrepts-Cryaquepts complex, moderately steep moraines46C6659631014515131p9id60919891:24000
Andic Cryochrepts, low relief rolling uplands, weathered granitic substratum, warm22AHX57141014359131j8id60919891:24000
Andic Cryochrepts and Dystric Cryochrepts, moderately steep moraines46C6555081014516131pbid60919891:24000
Andic Cryochrepts-Cryaquepts complex, high relief rolling uplands24CH642911014420131l7id60919891:24000
Andic Cryochrepts, glacial trough walls48C6541921014522131pjid60919891:24000
Andic Cryochrepts, high relief rolling uplands24AH533651014362131jcid60919891:24000
Andic Cryochrepts, high relief rolling uplands, shallow to sand and gravel24C6529061014368131jkid60919891:24000
Andic Cryochrepts, dissected mountain slopes31C6528091014434131lpid60919891:24000
Andic Cryochrepts-Cryaquepts complex, moderately steep nivational hollows36C6623801014503131nxid60919891:24000
Andic Cryochrepts-Cryaquepts complex, nivational hollows36A6623781014504131nyid60919891:24000
Andic Cryochrepts, mountain ridges, cold33A6723261014499131nsid60919891:24000
Andic Cryochrepts-Cryaquepts complex, mountain slopes32A6622221014492131nkid60919891:24000
Andic Cryochrepts, low relief rolling uplands, weathered granitic substratum22A6X20641014353131j2id60919891:24000
Andic Cryochrepts-Dystric Cryochrepts complex, glacial cirques42D6720271014511131p5id60919891:24000
Andic Cryochrepts-Dystric Cryochrepts complex, 45 to 60 percent slopes, dissected mountain slopes31DH732686370131njid61719761:24000
Andic Cryochrepts, dissected mountain slopes, warm31CH516272686421131lfid61819651:24000
Andic Cryochrepts, moderately steep mountain slopes32CH59902686432131nwid61819651:24000
Andic Cryochrepts, high relief rolling uplands, warm24CH59422686409131jhid61819651:24000
Andic Cryochrepts-Dystric Cryochrepts complex, 45 to 60 percent slopes, dissected mountain slopes31DH77742686428131njid61819651:24000
Andic Cryochrepts, low relief rolling uplands22AH55972686400131j6id61819651:24000
Andic Cryochrepts, mountain ridges33A653302686433131ntid61819651:24000
Andic Cryochrepts-Cryaquepts complex, low relief rolling uplands22AH62762686401131j5id61819651:24000
Andic Cryochrepts, mountain ridges, cold33A671222686434131nsid61819651:24000
Andic Cryochrepts-Cryaquepts complex, moderately steep nivational hollows36C661132686436131nxid61819651:24000
Andic Cryochrepts-Cryaquepts complex, nivational hollows36A66962686435131nyid61819651:24000
Andic Cryochrepts-Dystric Cryochrepts complex, glacial cirques42D67822686437131p5id61819651:24000
Andic Cryochrepts-Cryaquepts complex, gently sloping moraines46A66742686438131p3id61819651:24000
Cryumbrepts-Cryaquepts-Andic Cryochrepts complex, stream bottoms10AD9232686391131hsid61819651:24000
Andic Cryochrepts and Dystric Cryochrepts, moderately steep moraines46C65132686440131pbid61819651:24000
Andic Cryochrepts-Cryaquepts complex, high relief rolling uplands24CH642686410131l7id61819651:24000
Rock outcrop-Andic Cryochrepts complex, glacial cirques41L914678126865322s1xcid67119891:24000
Andic Cryochrepts, mountain ridges, south aspects33U804001226865192s1wyid67119891:24000
Andic Cryochrepts, undissected mountain slopes, south aspects34U803547326865242s1x3id67119891:24000
Andic Cryochrepts, glacial trough walls48L662767226865372s1xjid67119891:24000
Andic Cryochrepts, mountain ridges33U662764626865172s1wwid67119891:24000
Andic Cryumbrepts-Andic Cryochrepts complex, avalanche paths61U962760326865802spwnid67119891:24000
Andic Cryumbrepts-Andic Cryochrepts complex, glacial trough bottoms47L911946826865362s1xhid67119891:24000
Andic Cryochrepts, glaciated mountain ridges38U801540026865312s1xbid67119891:24000
Andic Cryochrepts-Andic Cryumbrepts-Rock outcrop complex, glacial cirques42L911315126865342s1xfid67119891:24000
Andic Cryochrepts, glacial trough bottoms47L661237826865352s1xgid67119891:24000
Andic Cryochrepts, mountain slopes, south aspects32U701181526865132s1wrid67119891:24000
Andic Cryumbrepts-Andic Cryochrepts complex, dissected stream breaklands61U921046426865792spwmid67119891:24000
Andic Cryumbrepts, dense till substratum-Andic Cryochrepts complex, glaciated mountain ridges38L931044926865302s1x9id67119891:24000
Andic Cryochrepts, mountain slopes, south aspects, cold32U80901826865142s1wsid67119891:24000
Andic Cryochrepts-Dystric Cryochrepts-Rock outcrop complex, glacial cirques42L66887026865332s1xdid67119891:24000
Andic Cryochrepts-Andic Cryumbrepts complex, glacial trough walls48L91698226865392s1xlid67119891:24000
Andic Cryochrepts, dissected stream breaklands, south aspects61U70609226865782spwlid67119891:24000
Andic Cryumbrepts-Andic Cryochrepts complex, avalanche debris fans16U96490926864622s1v3id67119891:24000
Fluvents, Andic Cryochrepts, and Aquepts, stream bottoms10A90244626864572s1tyid67119891:24000
Andic Cryochrepts, dissected glacial trough walls49L66210326865402s1xmid67119891:24000
Andic Cryochrepts-Andic Cryumbrepts complex, dissected glacial trough walls49L91205726865422s1xpid67119891:24000
Andic Cryochrepts-Andeptic Cryoboralfs association, glacial trough walls73213862617088nq42mt61919881:24000
Andeptic Cryoboralfs-Andic Cryochrepts complex, steep23-985372616083np2nmt61919881:24000
Andeptic Cryoboralfs-Andic Cryochrepts complex, hilly23-869807616081np2lmt61919881:24000
Andic Cryochrepts, glaciated mountain ridges57-867023617085nq3zmt61919881:24000
Andic Cryochrepts, glaciated mountain slopes57-965252617086nq40mt61919881:24000
Andic Cryochrepts-Entic Cryandepts-Rock outcrop complex, cirque basins21-863588616077np2gmt61919881:24000
Andic Cryochrepts-Entic Cryandepts-Rock outcrop complex, cirque basins, steep21-925278616078np2hmt61919881:24000
Andeptic Cryoboralfs-Andic Cryochrepts complex, rolling23-77297616080np2kmt61919881:24000
Andic Cryochrepts-Typic Cryoboralfs complex, glacial trough walls9010719779493v53ymt63119881:24000
Andic Cryochrepts-Rock outcrop complex, cirque basins79110207779521v54vmt63119881:24000
Andic Cryochrepts, mountain ridges59A7478779479v53hmt63119881:24000
Andic Cryochrepts, moraines12C6613779433v520mt63119881:24000
Andic Cryochrepts, rhyolitic substratum584031779477v53fmt63119881:24000
Rock outcrop-Andic Cryochrepts-Lithic Cryochrepts complex, glacial trough walls40191115621770nw03mt63419881:24000
Lithic Cryochrepts-Andic Cryochrepts-Rock outcrop complex, glaciated mountain ridges40590525621826nw1xmt63419881:24000
Rock outcrop-Lithic Cryochrepts-Andic Cryochrepts complex, cirque headwalls and alpine ridges40359635621820nw1qmt63419881:24000
Andic Cryochrepts-Rock outcrop-Lithic Cryochrepts complex, glaciated mountain ridges35357523621536nvrkmt63419881:24000
Andic Cryochrepts, moraines, steep40450736621822nw1smt63419881:24000
Andic Cryochrepts, moraines, dense, brittle substratum32949600621456nvnzmt63419881:24000
Andic Cryochrepts, moraines40745342621823nw1tmt63419881:24000
Andic Cryochrepts, glaciated mountain slopes32830674621455nvnymt63419881:24000
Andic Cryochrepts-Rock outcrop complex, glaciated mountain slopes, very steep40829930621824nw1vmt63419881:24000
Humicryods-Andic Cryochrepts-Rock outcrop complex, steep and very steep*13055634673972843wa60819951:24000
Andic Cryochrepts, very steep*1839501675182880wa60819951:24000
Haplocryods-Andic Cryochrepts-Rock outcrop complex, steep and very steep*1262599367382283mwa60819951:24000
Andic Cryochrepts-Rock outcrop complex, 65 to 90 percent slopes19330747262hrjwa65719811:24000
Andic Cryochrepts, 60 to 90 percent slopes12890749752j0kwa67319831:24000
Andic Cryochrepts-Rock outcrop complex, 60 to 90 percent slopes21980750792j3xwa67319831:24000

Map of Series Extent

Approximate geographic distribution of the ANDIC CRYOCHREPTS 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 .