Official Series Description


Lab Data Summary

Aggregate lab data for the BLAZON soil series. This aggregation is based on all pedons with a current taxon name of BLAZON, 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 BLAZON were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
34A82P068282WY013008Blazon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7125015,-108.4772186
67A89P081989WY021005Blazon8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5255547,-105.1533356

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLAZON 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BLAZON series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

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

Click the image to view it full size.

Geomorphic description summaries for the BLAZON 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Competing Series

Soil series competing with BLAZON share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

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

Click the image to view it full size.

Geomorphic description summaries for the BLAZON 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with BLAZON, 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 .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. WY-2012-03-23-01 | Fremont County, East Part and Dubois Area - July 1993

    Soils and their landscape positions as they relate to parent material, precipitation zones, and temperature regimes (Soil Survey of Fremont County, East Part and Dubois Area, WY; 1993).

Map Units

Map units containing BLAZON 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
Trimad-Blazon, thin solum-Rock outcrop complex, 20 to 45 percent slopes132401497631jptmco64419801:24000
Blazon, moist-Rentsac complex, 8 to 65 percent slopes1062467496949jp3mco68519791:24000
Circleville-Blazon complex2728920551531vd4ut63119821:24000
Trimad-Blazon-Rock outcrop complex, 3 to 40 percent slopes24827771046023hv8wy03119981:24000
Trimad-Weed-Blazon association, 0 to 15 percent slopes2501031044403hp1wy03119981:24000
Rock outcrop-Blazon, thin solum, complex, 30 to 60 percent slopes217861044383hnzwy03119981:24000
Chaperton, moderately saline-Blazon complex, 8 to 20 percent slopes128841044853hqhwy03119981:24000
Poposhia-Blazon silt loams, 3 to 30 percent slopes201661044353hnwwy03119981:24000
Blazon-Trimad complex, 15 to 45 percent slopes111261044243hnjwy03119981:24000
Poposhia-Blazon, thin solum-Rock outcrop complex, 5 to 35 percent slopes20241044363hnxwy03119981:24000
Blazon-Chaperton-Carthill complex, 8 to 30 percent slopes1421423923761882krm7wy0411:24000
Blazon-Byrnie-Feltner complex, 3 to 30 percent slopes32565153324840542pcvswy0411:24000
Blazon-Delphill complex, 8 to 40 percent slopes3761151324840832pcwqwy0411:24000
Chaperton, moderately saline-Blazon complex, 8 to 20 percent slopes13923404501675jv12wy60119911:24000
Blazon-Delphill complex, 20 to 45 percent slopes11616287501643jv01wy60119911:24000
Delphill-Blazon complex, 3 to 20 percent slopes15015675501688jv1hwy60119911:24000
Stunner-Tisworth-Blazon complex, 1 to 6 percent slopes23011450501800jv53wy60119911:24000
Poposhia-Blazon complex, 3 to 15 percent slopes1974188501741jv36wy60119911:24000
Blazon-Chaperton complex, moist, 3 to 20 percent slopes115616501642jv00wy60119911:24000
Rencot-Blazon complex, 15 to 40 percent slopes21514716697231t1h1wy60920061:24000
Rencot-Blazon complex, 15 to 40 percent slopes24718506502376jvrpwy62519851:24000
Blazon-Cragosen-Worfman association, hilly12716919502205jvl5wy62519851:24000
Delphill-Blazon loams, 5 to 30 percent slopes1708538502258jvmwwy62519851:24000
Blazon-Worfman loams, 6 to 30 percent slopes1268320502204jvl4wy62519851:24000
Rock River-Pinelli-Blazon complex, 3 to 20 percent slopes2594485502395jvs9wy62519851:24000
Poposhia-Blazon complex, 3 to 15 percent slopes2402339502366jvrcwy62519851:24000
Yamo-Blazon-Delphill-like complex, 4 to 35 percent slopes -- Draft490AD15259053s8wy6291:24000
Moyerson-Blazon-Rock outcrop complex, 0 to 60 percent slopes -- Draft38515254153qpwy6291:24000
Peyton-like-Blazon-Rock outcrop complex, 6 to 40 percent slopes -- Draft475BE24827572pbhywy6291:24000
Blazon-Diamondville-Rock outcrop complex, 15 to 75 percent slopes -- Draft172024827612pbj2wy6291:24000
Chaperton-Blazon-Yamo complex, 10 to 55 percent slopes -- Draft550525522722qtzvwy6291:24000
Chaperton, moderately saline-Blazon complex, 8 to 20 percent slopes113929598352x8p5wy6301:24000
Blazon-Delphill complex, 20 to 45 percent slopes111629598342x8p2wy6301:24000
Blazon-Cushool association, 2 to 20 percent slopes -- draft3446386723781052ktm2wy6301:24000
Blazon-Blackhall complex, 10 to 40 percent slopes -- draft3793400124379932mtxywy6301:24000
Seaverson-Blazon complex, 3 to 30 percent slopes -- draft4151292424554762nf3xwy6301:24000
Rentsac-Blazon, bouldery association, 10 to 50 percent slopes -- draft3831026324554732nf3twy6301:24000
Blazon-Chaperton association, 6 to 12 percent slopes -- draft305656623781022ktlzwy6301:24000
Delphill-Blazon complex, 3 to 20 percent slopes -- draft452408725730322x8pjwy6301:24000
Delphill-Blazon association. -- draft39045525730412r81wwy6301:24000
Forelle-Blazon, rubbly surface-Cushool complex, 4 to 35 percent slopes5604380014755881ljgmwy6351:24000
Blazon, rubbly surface-Spool-Earsman family, extremely stony surface, complex, 8 to 60 percent slopes9705224427716652t6d2wy6351:24000
Blazon thin solum-Blazon-Lilsnake complex, 2 to 40 percent slopes10512367503941jxd5wy63819901:24000
Blazon-Delphill complex, 6 to 30 percent slopes1067613503942jxd6wy63819901:24000
Thermopolis-Blazon-Sinkson complex, 3 to 60 percent slopes1892003504054jxhtwy63819901:24000
Rock outcrop-Blazon complex, 20 to 40 percent slopes1721687504032jxh3wy63819901:24000
Cragosen-Carmody-Blazon complex, 6 to 40 percent slopes0253494215754058xywy6471:24000
Rock outcrop-Blazon complex, 6 to 40 percent slopes0493408615757058yxwy6471:24000
Rentsac-Rock outcrop-Blazon complex, 0 to 75 percent slopes0732854315745058v1wy6471:24000
Poposhia-Blazon-Carmody complex, 3 to 45 percent slopes0452412615757458z1wy6471:24000
Blazon-Rock outcrop-Carmody complex, 2 to 40 percent slopes419220185908420djgwy6471:24000
Crownest-Cotha association6161281590555bhtwy67719751:24000
Cotha-Blazon-Rock outcrop association5118061590565bhvwy67719751:24000
Blazon-Rock outcrop association4101191590575bhwwy67719751:24000
Blazon-Patent association336991590585bhxwy67719751:24000
Blazon-Rock outcrop-Carmody complex, hilly602919190154921tq9wy67719751:24000
Poposhia-Blazon-Carmody complex, hilly552055190157121tr0wy67719751:24000
Cragosen-Carmody-Blazon complex, hilly6743190155221tqdwy67719751:24000
Cragosen-Carmody-Blazon complex, hilly13659156503001jwdvwy71319861:24000
Blazon-Rock outcrop-Carmody complex, hilly11853053502983jwd8wy71319861:24000
Poposhia-Blazon-Carmody complex, hilly18647347503051jwggwy71319861:24000
Poposhia, sodic-Blazon complex, rolling1879709503052jwghwy71319861:24000
Badland-Seaverson-Blazon complex, steep1136935502978jwd3wy71319861:24000
Rock outcrop-Blazon complex, hilly1975480503062jwgtwy71319861:24000
Blazon-Trimad complex, 15 to 45 percent slopes46414148151jh76wy71519741:20000
Blazon-Trimad complex, 15 to 45 percent slopes111325891049123j58wy72119941:24000
Trimad-Weed-Blazon association, 0 to 15 percent slopes180197911049813j7hwy72119941:24000
Trimad-Blazon, thin solum-Rock outcrop complex, 20 to 45 percent slopes177195791049783j7dwy72119941:24000
Trimad-Blazon complex, 15 to 45 percent slopes176164281049773j7cwy72119941:24000
Blazon-Chaperton complex, 3 to 20 percent slopes109100511049103j56wy72119941:24000
Poposhia-Blazon, thin solum-Rock outcrop complex, 5 to 35 percent slopes16088731049613j6vwy72119941:24000
Poposhia-Blazon silt loams, 3 to 30 percent slopes15975901049603j6twy72119941:24000
Blazon-Blazon, thin solum-Poposhia silt loams, 0 to 6 percent slopes10846951049093j55wy72119941:24000
Rock outcrop-Blazon, thin solum, complex, 30 to 60 percent slopes16625021049673j71wy72119941:24000
Blazon-Chaperton-Rock outcrop complex, 10 to 45 percent slopes11020181049113j57wy72119941:24000
Blazon-Chaperton-Fola complex, 5 to 30 percent slopes -- draft8205435026119642qsv9wy7231:24000
Blazon, rubbly surface-Spool-Earsman family, extremely stony surface, complex, 8 to 60 percent slopes9705409729702602t6d2wy7231:24000
Blazon, stony surface-Scooby-Manns, stony surface, complex, 8 to 42 percent slopes4410322249131334wy7371:24000
Chaperton-Blazon complex, 1 to 8 percent slopes -- draft2530344425723332mtk5wy7371:24000
Adel-Blazon-Rentsac association, steep -- draft61027742572293jx2twy7371:24000
Blazon loam, 8 to 30 percent slopes -- draft51920032572285jx1twy7371:24000
Delphill-Blazon association, 6 to 30 percent slopes -- draft20796825723482pb9pwy7371:24000
Blazon-Shinbara complex, 0 to 6 percent slopes -- draft23581725723992pbqjwy7371:24000
Blazon-Rentsac complex, 30 to 60 percent slopes -- draft5637392572291jx2lwy7371:24000
Blazon-Cushool association, 2 to 20 percent slopes -- draft734442325724262pr27wy7371:24000
Worfman-Blazon complex, 3 to 15 percent slopes -- draft5153212572284jx1qwy7371:24000
Blackhall-Blazon-Poposhia complex, 3 to 30 percent slopes -- draft590832572292jx2swy7371:24000

Map of Series Extent

Approximate geographic distribution of the BLAZON 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 .