Official Series Description


Lab Data Summary

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


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TYPIC 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 TYPIC 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 TYPIC 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 TYPIC 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 TYPIC 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 TYPIC 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 TYPIC 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 TYPIC 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 TYPIC 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
Histic Pergelic Cryaquepts-Typic Cryochrepts complex, 15 to 45 percent slopes122410800517581qvmak64219901:24000
Typic Cryochrepts-Rock outcrop complex, 6 to 35 percent slopes138151860517741qw4ak64219901:24000
Histic Pergelic Cryaquepts-Typic Cryochrepts association, 15 to 45 percent slopes12178631517571qvlak64219901:24000
Typic Cryorthents-Typic Cryochrepts-Rock outcrop complex, 0 to 45 percent slopes11114005466855hnsvca74019961:24000
Rock outcrop-Typic Cryochrepts-Typic Cryoborolls complex, limestone substratum87-1A1914202411025y7wid75819981:24000
Typic Cryoboralfs-Typic Cryochrepts complex, rhyolite flows88-2A1477202411325y7zid75819981:24000
Typic Cryochrepts-Rock outcrop-Rubbleland complex, cirque headwalls22-1C1332202409625y7fid75819981:24000
Typic Cryochrepts, glaciated mountain ridges12-1C204202409525y7did75819981:24000
Typic Cryochrepts, glacial drift substratum34-1C156202409925y7jid75819981:24000
Typic Cryochrepts-Rock outcrop complex, warm, steep54-1C143202410625y7rid75819981:24000
Typic Cryochrepts, obsidian sand substratum46-3A139202410225y7mid75819981:24000
Rock outcrop-Typic Cryochrepts-Typic Cryoborolls complex, south aspect, steep54-1B137202410525y7qid75819981:24000
Typic Cryoboralfs-Typic Cryochrepts-Rock outcrop complex, structurally controlled slopes87-2B75202411125y7xid75819981:24000
Typic Cryochrepts-Rock outcrop-Rubbleland complex, cirque headwalls22-1C12033515724458mdmt62319881:24000
Typic Cryochrepts-Rock outcrop complex, steep54-1G4974115719158kpmt62319881:24000
Typic Cryochrepts, glacial drift substratum34-1C3645715716458jtmt62319881:24000
Rock outcrop-Typic Cryochrepts-Typic Cryoborolls complex, south aspect, steep54-1B3587215718858klmt62319881:24000
Rock outcrop-Typic Cryochrepts-Typic Cryoborolls complex, limestone substratum87-1A3050915723158lzmt62319881:24000
Typic Cryochrepts, obsidian sand substratum46-3A2459215718158kcmt62319881:24000
Typic Cryochrepts, glacial drift substratum, steep35-1C2394515717558k5mt62319881:24000
Typic Cryochrepts-Rock outcrop complex, volcanic substratum22-3A2001415715958jnmt62319881:24000
Typic Cryochrepts-Typic Cryoboralfs-Rock outcrop complex, structurally controlled slopes87-1D1857315723358m1mt62319881:24000
Typic Cryochrepts-Rock outcrop complex, limestone substratum, steep54-2C1553415719358krmt62319881:24000
Typic Cryochrepts-Rock outcrop complex, warm, steep54-1C1545715718958kmmt62319881:24000
Typic Cryochrepts, rhyolite flows88-1A1212515723958m7mt62319881:24000
Typic Cryoboralfs-Typic Cryochrepts-Rock outcrop complex, structurally controlled slopes87-2B1054815723558m3mt62319881:24000
Typic Cryoboralfs-Typic Cryochrepts complex, landslides71-1D983415721058l9mt62319881:24000
Typic Cryoboralfs-Typic Cryochrepts-Rock outcrop complex, calcareous substratum85-2B927715722258lpmt62319881:24000
Typic Cryochrepts, mountain slopes53-1D770115718358kfmt62319881:24000
Typic Cryochrepts-Rock outcrop-Cryaquolls complex, glaciated moutain ridges22-3C752615716058jpmt62319881:24000
Typic Cryoboralfs-Typic Cryochrepts complex, rhyolite flows88-2A657715724058m8mt62319881:24000
Typic Cryochrepts, glaciated mountain ridges12-1C643015715158jdmt62319881:24000
Typic Cryoboralfs-Typic Cryochrepts-Rock outcrop complex, mountain slopes54-2E504115719558ktmt62319881:24000
Typic Cryoboralfs-Typic Cryochrepts-Rock outcrop complex, cirque headwalls22-2A460615715858jmmt62319881:24000
Typic Cryochrepts-Typic Cryoborolls complex, glacial drift substratum34-1D357215716558jvmt62319881:24000
Typic Cryochrepts-Argic Cryoborolls association, cold13-2A352315715558jjmt62319881:24000
Typic Cryoboralfs-Typic Cryochrepts complex, mountain slopes49B50085779470v536mt63119881:24000
Typic Cryochrepts-Typic Cryoboralfs complex, mountain slopes3421154779453v52nmt63119881:24000
Typic Cryochrepts-Typic Cryoboralfs complex, glaciated mountain slopes79020490779520v54tmt63119881:24000
Typic Cryochrepts-Rubble land complex, basaltic substratum, cold57A20043779476v53dmt63119881:24000
Typic Cryochrepts, channery-Typic Cryochrepts, extremely cobbly complex, mountain ridges5919276779478v53gmt63119881:24000
Typic Cryochrepts, bouldery, granitic substratum, steep7619052779482v53lmt63119881:24000
Typic Cryochrepts, steep4417235779463v52zmt63119881:24000
Typic Cryochrepts, basaltic substratum, steep77B17158779486v53qmt63119881:24000
Typic Ustochrepts-Typic Cryochrepts complex, mountain slopes39213076779516v54pmt63119881:24000
Typic Cryochrepts-Lithic Cryochrepts-Rock outcrop complex, dip slopes32B11487779452v52mmt63119881:24000
Typic Cryochrepts, colluvial toeslopes and basins14C10907779439v526mt63119881:24000
Typic Cryochrepts-Rubble land complex, steep56A10229779474v53bmt63119881:24000
Typic Cryochrepts-Lithic Cryochrepts complex, mountain ridges779288779484v53nmt63119881:24000
Typic Cryochrepts, mountain slopes, metasedimentary substratum796383779487v53rmt63119881:24000
Typic Cryochrepts-Rock outcrop complex, mountain slopes59B6365779480v53jmt63119881:24000
Typic Cryoboralfs-Typic Cryochrepts complex, structural benches79B6289779488v53smt63119881:24000
Typic Cryochrepts and Calcic Cryoborolls, steep, cool416128779462v52ymt63119881:24000
Typic Cryochrepts, bouldery, granitic substratum76A5572779483v53mmt63119881:24000
Typic Cryochrepts-Lithic Cryochrepts-Rock outcrop complex, limestone substratum954581779498v543mt63119881:24000
Typic Cryochrepts-Rubble land complex, basaltic substratum574315779475v53cmt63119881:24000
Typic Cryochrepts-Lithic Cryochrepts-Rock outcrop complex, bouldery, granitic substratum564265779473v539mt63119881:24000
Aquolls-Typic Cryochrepts complex, moraines1364022779505v54bmt63119881:24000
Typic Cryochrepts, colluvial deposits143615779436v523mt63119881:24000
Typic Cryochrepts-Rock outcrop complex, glacial trough walls, granitic substratum892437779492v53xmt63119881:24000
Typic Cryochrepts and Typic Cryoboralfs, till substratum, hilly12B2208779432v51zmt63119881:24000
Typic Cryoboralfs-Typic Cryochrepts complex, granitic substratum1201922779503v548mt63119881:24000
Typic Cryochrepts, structural breaklands971921779499v544mt63119881:24000
Aquic Cryoboralfs-Typic Cryochrepts complex, 4 to 15 percent slopes824041465074xg1mt63619831:24000
Rock outcrop-Typic Cryochrepts-Typic Cryoborolls complex, south aspect, steep54-1B1315741454swjwmt6691:24000
Typic Cryochrepts-Typic Cryoborolls complex, glacial drift substratum34-1D578115146017n5wmt6691:24000
Typic Cryochrepts-Rock outcrop complex, volcanic substratum22-3A373741408swhdmt6691:24000
Typic Cryochrepts, glacial drift substratum, steep35-1C301115146917n65mt6691:24000
Typic Cryochrepts, glacial drift substratum34-1C179741414swhlmt6691:24000
Typic Cryochrepts-Rock outcrop complex, steep54-1G160741472swkgmt6691:24000
Typic Cryochrepts, glaciated mountain ridges12-1C12115881361q9l6mt6691:24000
Typic Cryoboralfs-Typic Cryochrepts complex, landslides71-1D100741553swn2mt6691:24000
Rock outcrop-Typic Cryochrepts-Typic Cryoborolls complex, limestone substratum87-1A72115252717p99mt6691:24000
Typic Cryochrepts-Rock outcrop complex, warm, steep54-1C56741473swkhmt6691:24000
Typic Cryochrepts-Rock outcrop-Cryaquolls complex, glaciated mountain ridges22-3C619015796559cnwy65620081:24000
Rock outcrop-Typic Cryochrepts complex, cirque headwalls22-1C68915796659cpwy65620081:24000
Typic Haplocryalfs-Typic Argicryolls-Typic Cryochrepts complex, 20 to 50 percent slopes361T5491577665957wy65620081:24000
Glossic Cryoboralfs-Typic Cryochrepts-Mollic Cryoboralfs complex, 0 to 30 percent slopes155T1281577625953wy65620081:24000
Typic Cryochrepts-Typic Cryorthents association, 40 to 70 percent slopes488T1021577675958wy65620081:24000

Map of Series Extent

Approximate geographic distribution of the TYPIC 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 .