Official Series Description


Lab Data Summary

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

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Sibling Summary

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

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

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Geomorphic description summaries for the FRISCO 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 .

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Competing Series

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

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

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Geomorphic description summaries for the FRISCO 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 .

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

Soil series sharing subgroup-level classification with FRISCO, 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

No block diagrams are available.

Map Units

Map units containing FRISCO 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
Frisco-Catamount, moist families complex, 5 to 40 percent slopes7702B7462420087tlyqco64220121:24000
Frisco-Catamount, moist families complex, 5 to 40 percent slopes7702B54411762994tlyqco6451:24000
Frisco, sandstone substratum-Howlett, moist-Scout, moist families complex, 5 to 40 percent slopes7501B39152762988tlyjco6451:24000
Scout, moist-Frisco familes complex, 40 to 75 percent slopes7502C19344762989tlykco6451:24000
Herd-Frisco families complex, sandstone substratum, 5 to 40 percent slopes7503B15529762990tlylco6451:24000
Frisco, dry-Howlett families complex, sandstone substratum, 5 to 40 percent slopes4512B3201762976tly4co6451:24000
Frisco family, very stony-Finn family, very stony-Water complex, 0 to 20 percent slopes666A26650509375k31gco6471:24000
Frisco-Tamarron complex, 10 to 40 percent slopes249B8785509316k2zkco6471:24000
Frisco family very stony sandy loam, 35 to 65 percent slopes, very stony767D2609509399k327co6471:24000
Reddles-Frisco complex, 3 to 25 percent slopes, very stony75C9270506916k0h4co6481:24000
Frisco, very stony-Dorpat complex, 3 to 25 percent slopes78D8193506919k0h7co6481:24000
Frisco-Peeler gravelly sandy loams, 25 to 65 percent slopes3333663497857jq1xco64919771:24000
Frisco-Peeler gravelly sandy loams, 6 to 25 percent slopes329408497856jq1wco64919771:24000
Frisco-Peeler gravelly sandy loams, 2 to 6 percent slopes31960497855jq1vco64919771:24000
Frisco, very stony-Tepete families, complex, 0 to 40 percent slopes, landslides430B28390507544k14dco6501:24000
Frisco family very cobbly loam, 10 to 40 percent slopes, very stony603B15511507546k14gco6501:24000
Frisco family, very stony-Finn family, very stony-Water complex, 0 to 20 percent slopes666A79103176977k31gco6501:24000
Frisco family very stony sandy loam, 35 to 65 percent slopes, very stony737D20603176980k327co6501:24000
Reddles-Frisco complex, 3 to 25 percent slopes, very stony75C343106903k0h4co65519841:24000
Frisco, very stony-Rock outcrop-Silverjack complex, 30 to 60 percent slopes912164299083921v94co66019941:24000
Frisco gravelly loam, 5 to 30 percent slopes92147229908622kmmzco66219681:24000
Frisco, very stony-Rock outcrop-Silverjack complex, 30 to 60 percent slopes912291299094121v94co66219681:24000
Frisco-Agneston association, 5 to 50 percent slopes14014053224536802nc7zco66419871:24000
Leighcan-Frisco association, 5 to 60 percent slopes1507171424538212ncdjco66419871:24000
Frisco-Scout association, 15 to 60 percent slopes1426379424536822nc81co66419871:24000
Leighcan-Frisco association, moist, 5 to 60 percent slopes1511746724538222ncdkco66419871:24000
Leighcan-Frisco complex, 5 to 35 percent slopes, very bouldery1521564824538232ncdlco66419871:24000
Frisco-Mulgon association, 2 to 35 percent slopes1411301224536812nc80co66419871:24000
Frisco very stony loam, slumped slopes, 5 to 60 percent slopes1391197124536782nc7xco66419871:24000
Frisco very stony loam, 5 to 35 percent slopes138378024538192ncdgco66419871:24000
Frisco-Horsethief complex, 30 to 75 percent slopes15433185507094k0nwco67220031:24000
Frisco loam, 10 to 25 percent slopes15114996507091k0nsco67220031:24000
Tamarron-Frisco complex, 30 to 60 percent slopes8905920507281k0vxco67220031:24000
Frisco-Horsethief complex, 10 to 30 percent slopes1535638507093k0nvco67220031:24000
Ute-Frisco complex, 0 to 20 percent slopes8265487507270k0vkco67220031:24000
Frisco loam, 25 to 45 percent slopes1525162507092k0ntco67220031:24000
Frisco-Quazar complex, 30 to 60 percent slopes3873436507163k0r3co67220031:24000
Tamarron-Frisco complex, 15 to 30 percent slopes8911133507282k0vyco67220031:24000
Frisco-Quazar complex, 15 to 30 percent slopes388647507164k0r4co67220031:24000
Frisco, very stony-Rock outcrop-Silverjack complex, 30 to 60 percent slopes9127040299084021v94co67419981:24000
Frisco gravelly loam, 5 to 30 percent slopes921275329908632kmmzco67419981:24000
Frisco-Horsethief complex, 10 to 30 percent slopes117238505166jynpco67419981:24000
Frisco, very stony-Rock outcrop-Silverjack complex, 30 to 60 percent slopes91214299094521v94co67619831:24000
Frisco, very stony-Rock outcrop-Silverjack complex, 30 to 60 percent slopes91213408190210221v94co67720181:24000
Frisco gravelly loam, 5 to 30 percent slopes921598723723672kmmzco67720181:24000
Frisco-Peeler complex, 25 to 65 percent slopes5F24601497311jph9co69019741:24000
Frisco-Peeler complex, 6 to 25 percent slopes5E5919497310jph8co69019741:24000
Mikesell-Herd-Frisco families, complex, 20 to 60 percent slopes375512984239535zid7131:24000
Leighcan-Frisco association, moist, 5 to 60 percent slopesLfF7927701602tl90nm6721:24000
Frisco, extremely stony-Kingmine-Trout Creek families association, 8 to 45 percent slopes488281724042942lpvwut6471:24000
Mikesell-Herd-Frisco families, complex, 20 to 60 percent slopes37573083460535zwy62319711:20000
Frisco-Jaegie complex, 0 to 25 percent slopes63129598302wswzwy6301:24000
Jaegie-Frisco complex, 15 to 50 percent slopes6301177028284392tz4mwy6301:24000
Frisco-Taglake families, complex, 10 to 25 percent slopes11119212708641rsddwy6321:24000
Frisco-Taglake families, complex, 25 to 40 percent complex11218808708649rsdnwy6321:24000
Frisco family-Aquic Haplocryalfs complex, 10 to 25 percent slopes, very stony11017418708642rsdfwy6321:24000
Frisco family very stony loam, 10 to 25 percent slopes, very stony10512612708639rsdbwy6321:24000
Frisco family-Aquic Haplocryalfs complex, 0 to 10 percent slopes, very stony10911806708643rsdgwy6321:24000
Frisco family, very stony-Kettles association, 0 to 25 percent slopes10810506708644rsdhwy6321:24000
Frisco family stony loam, 0 to 10 percent slopes, very stony1048906708640rsdcwy6321:24000
Frisco family, very stony-Taglake family, very stony-Rock outcrop complex, 40 to 85 percent slopes1074324708637rsd8wy6321:24000
Frisco family very stony sandy loam, 25 to 40 percent slopes, very stony1062524708638rsd9wy6321:24000
Aquic Haplocryalfs, very stony-Frisco family complex, 0 to 10 percent slopes1151768708646rsdkwy6321:24000
Cloud Peak-Redfist-Frisco families, complex, 15 to 60 percent slopes60056185723320blrwy6471:24000
Frisco-Troutville association, 2 to 40 percent slopes, extremely stony196846015803059frwy65019821:24000
Cloud Peak-Redfist-Frisco families, complex, 15 to 60 percent slopes43L13434157758594zwy65620081:24000
Frisco-Enentah families, complex, 5 to 30 percent slopes3506396157876598swy65620081:24000
Frisco-Taglake-Helmville families, complex, 5 to 40 percent slopes2603874157810596nwy65620081:24000
Mikesell-Herd-Frisco families, complex, 20 to 60 percent slopes3758541152023535zwy66320121:24000
Frisco-Fulcher-Woodhurst families, complex, 30 to 60 percent slopes4253452152039536hwy66320121:24000
Midfork-Frisco-Stubbs families, complex29721557730565412xtsvwy66519961:62500
Rock outcrop-Handran association413271590915bjzwy67719751:24000

Map of Series Extent

Approximate geographic distribution of the FRISCO 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 .