Official Series Description


Lab Data Summary

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

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Soil series sharing subgroup-level classification with THEEDLE, 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 THEEDLE 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
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes21631813877482tmwlmt64319671:20000
Theedle-Shingle loams, 3 to 30 percent slopes2554827802562tzbvwy01119781:24000
Cushman-Theedle loams, 6 to 15 percent slopes261457802542yrz2wy01119781:24000
Theedle loam, 0 to 45 percent slopes, gullied252227802552vhzywy01119781:24000
Theedle loam, 0 to 45 percent slopes, gullied2161094423497272vhzywy02719931:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes206756983497172tmwlwy02719931:24000
Kishona-Cambria-Theedle loams, 3 to 20 percent slopes154545833496222vhzxwy02719931:24000
Theedle-Kishona loams, 6 to 20 percent slopes205260103497162tzc4wy02719931:24000
Keeline-Kishona-Theedle complex, 6 to 30 percent slopes15022099349614cqswwy02719931:24000
Theedle-Kishona loams, 0 to 6 percent slopes204117113497152tzc2wy02719931:24000
Theedle-Midway-Rock outcrop complex, 10 to 60 percent slopes5D39335831030ztlwy04319761:24000
Savageton-Theedle-Worfka complex, 6 to 40 percent slopes5D0933566933013zwy04319761:24000
Theedle loam, 0 to 45 percent slopes, gullied45767763494492vhzywy04519841:24000
Kishona-Shingle-Theedle loams, 6 to 15 percent slopes55622633494602xtvvwy04519841:24000
Shingle-Theedle loams, 6 to 30 percent slopes10143424349384cqkgwy04519841:24000
Kishona-Theedle-Zigweid loams, 2 to 10 percent slopes5622550349461cqmywy04519841:24000
Shingle-Theedle-Cambria association, steeply sloping10213510349385cqkhwy04519841:24000
Theedle-Kishona loams, 2 to 15 percent slopes114116573493982tzc3wy04519841:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes164438016148492tmwlwy04519841:24000
Theedle-Kishona loams, 6 to 20 percent slopes14211933616932tzc4wy04519841:24000
Theedle-Shingle loams, 3 to 30 percent slopes1436873616992tzbvwy04519841:24000
Zigweid-Cambria-Theedle complex, 6 to 15 percent slopes1488314239462ztzfwy04519841:24000
Theedle-Shingle loams, 3 to 30 percent slopes2171057173499172tzbvwy60519951:24000
Theedle loam, 0 to 45 percent slopes, gullied233778843499332vhzywy60519951:24000
Theedle-Kishona loams, 6 to 20 percent slopes215724493499152tzc4wy60519951:24000
Theedle-Kishona loams, 0 to 6 percent slopes214372583499142tzc2wy60519951:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes216352133499162tmwlwy60519951:24000
Cushman-Theedle loams, 6 to 15 percent slopes127127653498122yrz2wy60519951:24000
Theedle-Turnercrest-Kishona complex, 3 to 15 percent slopes21810481349918cr3pwy60519951:24000
Cushman-Theedle loams, 0 to 6 percent slopes1268590349811cr07wy60519951:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes2518238516697452tmwlwy60920061:24000
Kishona-Cambria-Theedle loams, 3 to 20 percent slopes1897822016697052vhzxwy60920061:24000
Theedle-Kishona loams, 0 to 6 percent slopes2492281316697732tzc2wy60920061:24000
Theedle-Kishona loams, 6 to 20 percent slopes2501474016697742tzc4wy60920061:24000
Theedle loam, 0 to 45 percent slopes, gullied2631067916697532vhzywy60920061:24000
Keeline-Kishona-Theedle complex, 6 to 30 percent slopes183298116697711t1jlwy60920061:24000
Zigweid-Theedle loams, 3 to 15 percent slopes27458116697622v09rwy60920061:24000
Savageton-Theedle-Worfka complex, 6 to 40 percent slopes5D0933028463013zwy6171:24000
Theedle-Midway-Rock outcrop complex, 10 to 60 percent slopes5D39335829430ztlwy6171:24000
Theedle loam, 0 to 45 percent slopes, gullied2339348172522vhzywy61919711:24000
Theedle-Shingle-Kishona complex, 6 to 40 percent slopes, gullied2838288169302tzc8wy61919711:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes2164508172512tmwlwy61919711:24000
Theedle-Shingle loams, 3 to 30 percent slopes7095223836682tzbvwy61919711:24000
Theedle-Shingle-Kishona complex, 6 to 40 percent slopes, gullied2831050845024192tzc8wy62519851:24000
Zigweid-Theedle loams, 3 to 15 percent slopes311363065024592v09rwy62519851:24000
Shingle-Theedle association, rolling27622392502412jvsvwy62519851:24000
Urban land-Theedle-Shingle complex, 4 to 20 percent slopes299479502435jvtlwy62519851:24000
Zigweid-Cambria-Theedle complex, 6 to 15 percent slopes31917514213552ztzfwy62519851:24000
Theedle-Kishona loams, 6 to 20 percent slopes32113114213582tzc4wy62519851:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes3163513982962tmwlwy62519851:24000
Shingle-Theedle-Kishona complex, moist, 3 to 30 percent slopes269724423610492xtvbwy63319871:24000
Shingle-Theedle-Kishona complex, 6 to 25 percent slopes268519323610582wxz5wy63319871:24000
Shingle-Theedle loams, moist, 45 to 75 percent slopes267392123610592wxz7wy63319871:24000
Theedle-Kishona association, moist, 6 to 9 percent slopes2828121361041d3phwy63319871:24000
Theedle-Kishona association, 6 to 15 percent slopes2816775361042d3pjwy63319871:24000
Shingle-Theedle complex, 45 to 75 percent slopes2664824361057d3q0wy63319871:24000
Theedle-Kishona association, moist, 9 to 15 percent slopes2833316361040d3pgwy63319871:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes32829713612302tmwlwy63319871:24000
Shingle-Theedle-Rock outcrop association, moist, 15 to 45 percent slopes2701428361052d3pvwy63319871:24000
Theedle-Shingle loams, 3 to 30 percent slopes329593612312tzbvwy63319871:24000
Theedle-Kishona loams, 6 to 20 percent slopes7074023836672tzc4wy63319871:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes216258358175842tmwlwy70520031:24000
Theedle-Shingle loams, 3 to 30 percent slopes21765548175852tzbvwy70520031:24000
Theedle-Kishona loams, 6 to 20 percent slopes21513478175832tzc4wy70520031:24000
Theedle loam, 0 to 45 percent slopes, gullied23311038176022vhzywy70520031:24000
Theedle-Kishona loams, 6 to 20 percent slopes141163723515192tzc4wy70919831:24000
Zigweid-Cambria-Theedle complex, 6 to 15 percent slopes152117533515302ztzfwy70919831:24000
Shingle-Theedle-Cambria association, 6 to 30 percent slopes1336636351511css2wy70919831:24000
Theedle-Kishona loams, 0 to 6 percent slopes14049733515182tzc2wy70919831:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes2106143612822tmwlwy70919831:24000
Theedle loam, 0 to 45 percent slopes, gullied2125523612842vhzywy70919831:24000
Theedle-Shingle-Kishona complex, 6 to 40 percent slopes, gullied24854014279052tzc8wy70919831:24000
Kishona-Cambria-Theedle loams, 3 to 20 percent slopes23015814278482vhzxwy70919831:24000
Zigweid-Theedle loams, 3 to 15 percent slopes2492914279062v09rwy70919831:24000
Theedle-Kishona-Shingle loams, 3 to 30 percent slopes7081300168139772tmwlwy71920131:24000
Theedle-Shingle loams, 3 to 30 percent slopes7091254848139782tzbvwy71920131:24000
Theedle-Kishona loams, 6 to 20 percent slopes707322738139862tzc4wy71920131:24000
Theedle-Nihill complex, 5 to 40 percent slopes722942714693071l9y0wy71920131:24000
Shingle-Theedle-Kishona complex, 6 to 25 percent slopes697483513840331hg67wy71920131:24000
Theedle loam, 0 to 45 percent slopes, gullied716403013991452vhzywy71920131:24000

Map of Series Extent

Approximate geographic distribution of the THEEDLE 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 .