Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
4640A3662S1968MT035001Ethridge6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.4968452,-112.2059174
5240A366368MT051003aEthridge7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.4332428,-110.9289322
58A40A3507S1953MT111001Ethridge6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8618736,-108.2849121
58A40A3536S1953MT111004Ethridge5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7749252,-108.7082596
58A40A3509S1953MT111009Ethridge6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8810387,-108.1243515
58A40A3534S1956MT103010Ethridge6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.2924347,-107.2165451
58A08N0152S2006MT033001Ethridge7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5220375,-107.1273499
58C96P0153S1994ND007030Ethridge8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0705566,-103.3638916

Water Balance

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

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 ETHRIDGE, 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 ETHRIDGE 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
Ethridge loam, 2 to 8 percent slopes85C21497343259cj5wmt01119921:24000
Ethridge silty clay loam, 2 to 8 percent slopes66C129053432042tvlqmt01119921:24000
Ethridge loam, 0 to 2 percent slopes85A9598343258cj5vmt01119921:24000
Bascovy-Ethridge complex, 2 to 8 percent slopes490C6156343127cj1mmt01119921:24000
Ethridge-Daglum complex, 0 to 4 percent slopes185A4072342990chx6mt01119921:24000
Tanna-Ethridge silty clay loams, 2 to 8 percent slopes164C2097342937chvhmt01119921:24000
Tanna-Ethridge silty clay loams, 8 to 15 percent slopes164D817342938chvjmt01119921:24000
Ethridge silty clay loam, warm, 2 to 8 percent slopes626C401343183cj3fmt01119921:24000
Ethridge silty clay loam, 2 to 8 percent slopes39C42003434322tvlqmt01719951:24000
Ethridge silty clay loam, warm, 0 to 2 percent slopes39A32443434312wbypmt01719951:24000
Ethridge silty clay loam, warm, 0 to 2 percent slopesSc4853420342wbypmt02119711:24000
Ethridge silty clay loam, 2 to 8 percent slopesSd3393420352tvlqmt02119711:24000
Ethridge silty clay loam, 2 to 8 percent slopes85C49893423012tvlqmt02519911:24000
Tanna-Ethridge silty clay loams, 2 to 8 percent slopes164C3597342113cgzxmt02519911:24000
Tanna-Ethridge silty clay loams, 8 to 15 percent slopes164D1003342114cgzymt02519911:24000
Ethridge loam, 2 to 8 percent slopes166C956342117ch01mt02519911:24000
Ethridge silty clay loam, 2 to 6 percent slopesL0836B91032234922qk44mt02519911:24000
Ethridge silty clay loam, warm, 0 to 2 percent slopes85A7753423002wbypmt02519911:24000
Tanna-Ethridge silty clay loams, 3 to 6 percent slopesL1025B13632234952qk4bmt02519911:24000
Ethridge silty clay loam, 0 to 2 percent slopesL0836A9532234912q2mpmt02519911:24000
Ethridge silty clay loam, 2 to 8 percent slopes885501342592chhcmt02719791:24000
Ethridge silty clay loam, 0 to 2 percent slopes8725263425912wbyqmt02719791:24000
Tanna-Ethridge-Cabston complex, 8 to 25 percent slopes2242094342462chc5mt02719791:24000
Ethridge-Cabston complex, 2 to 8 percent slopes891288342593chhdmt02719791:24000
Ethridge silty clay loam, warm, 0 to 2 percent slopes47B611633426542wbypmt03320021:24000
Ethridge silty clay loam, 2 to 8 percent slopes47C179523426552tvlqmt03320021:24000
Ethridge loam, 4 to 8 percent slopes471C6869342653chkbmt03320021:24000
Ethridge loam, 0 to 4 percent slopes471B3575342652chk9mt03320021:24000
Ethridge clay loam, 0 to 2 percent slopes381A11207343939cjwtmt04119941:24000
Ethridge silty clay loam, 0 to 4 percent slopes38B20283344196ck53mt05119921:24000
Ethridge-Kobase complex, 0 to 4 percent slopes385B11949344195ck52mt05119921:24000
Ethridge silty clay loam, warm, 0 to 2 percent slopes5847583444222wbypmt05519811:24000
Ethridge silty clay loam, 2 to 8 percent slopes5913243444232tvlqmt05519811:24000
Ethridge clay loam, 2 to 8 percent slopes51B5621344594cgkfmt06519961:24000
Ethridge clay loam, 0 to 2 percent slopes51A3351344593cgkdmt06519961:24000
Ethridge-Verson clay loams, 0 to 2 percent slopes158A1886344492ckgnmt06519961:24000
Ethridge clay loam, 2 to 8 percent slopes3413892344701ckpdmt06919891:24000
Ethridge clay loam, 0 to 2 percent slopes336562344700ckpcmt06919891:24000
Ethridge silty clay loam, warm, 0 to 2 percent slopes4815143449272wbypmt07919861:24000
Ethridge silty clay loam, 2 to 8 percent slopes4912463449342tvlqmt07919861:24000
Ethridge clay loam, 0 to 4 percent slopes38B10639345154cl50mt10119921:24000
Ethridge silty clay loam, 0 to 4 percent slopes384B4200345152cl4ymt10119921:24000
Ethridge-Evanston clay loams, 0 to 4 percent slopes386B3283345153cl4zmt10119921:24000
Lonna-Ethridge complex, 0 to 4 percent slopes582B3019345228cl7dmt10119921:24000
Ethridge-Absher clay loams, 0 to 2 percent slopesEm116591468044xrmmt60019691:24000
Ethridge clay loam, sand substratum, 2 to 4 percent slopesEd88201468004xrhmt60019691:24000
Ethridge silty clay loam, 2 to 4 percent slopesEh68501468034xrlmt60019691:24000
Ethridge silty clay loam, 0 to 2 percent slopesEg55721468024xrkmt60019691:24000
Ethridge clay loam, sand substratum, 4 to 8 percent slopesEe16841468014xrjmt60019691:24000
Ethridge clay loam, sand substratum, 0 to 2 percent slopesEc14141467994xrgmt60019691:24000
Ethridge silty clay loam, 0 to 4 percent slopes4114758346460cmj4mt60819761:24000
Ethridge-Gerdrum complex, 0 to 4 percent slopes428431346463cmj7mt60819761:24000
Ethridge silty clay loam, 0 to 2 percent slopes338B204829923962wbyqmt60819761:24000
Ethridge clay loam, 2 to 8 percent slopes81C101475774ykkmt60919711:24000
Ethridge-Kobar silty clay loams, 2 to 8 percent slopes688317341954cgtsmt61319751:24000
Ethridge silty clay loam, 0 to 2 percent slopes652354341951cgtpmt61319751:24000
Ethridge-Kobar silty clay loams, 0 to 2 percent slopes671661341953cgtrmt61319751:24000
Rentsac-Ethridge complex, 2 to 25 percent slopes1641335341828cgpqmt61319751:24000
Ethridge silty clay loam, 2 to 4 percent slopes661314341952cgtqmt61319751:24000
Ethridge silty clay loam, 0 to 4 percent slopes38B50853346750cmthmt61519921:24000
Ethridge-Kobase silty clay loams, 0 to 4 percent slopes385B30558346745cmtbmt61519921:24000
Ethridge-Lonna silty clay loams, 0 to 2 percent slopes388A14521346747cmtdmt61519921:24000
Ethridge clay loam, 0 to 4 percent slopes381B3866346740cmt5mt61519921:24000
Ethridge-Evanston complex, 0 to 4 percent slopes386B2612346746cmtcmt61519921:24000
Ethridge silty clay loam, 0 to 2 percent slopes338B61329923972wbyqmt61519921:24000
Ethridge clay loam, 1 to 4 percent slopes146B4614347261cnbzmt62420211:24000
Ethridge clay loam, 4 to 8 percent slopes146C3452347262cnc0mt62420211:24000
Ethridge clay loam, 2 to 4 percent slopes, fan476C15201912707226b7mt62420211:24000
Ethridge-Tanna clay loams, 2 to 8 percent slopes169C1221251367250s1mt62420211:24000
Ethridge-Rentsac complex, 2 to 8 percent slopes443C9301914100227s5mt62420211:24000
Boxwell-Ethridge complex, 2 to 8 percent slopes430C5061914268227ylmt62420211:24000
Boxwell-Ethridge complex, 8 to 15 percent slopes430D4421914270227ynmt62420211:24000
Ethridge clay loam, 0 to 2 percent slopes, cool476B26419126962269wmt62420211:24000
Ethridge-Reedpoint complex, 2 to 8 percent slopes153C123347271cnc9mt62420211:24000
Ethridge-Reedpoint complex, 8 to 15 percent slopes153D108251367150rcmt62420211:24000
Ethridge clay loam, 2 to 8 percent slopes81C108515151852npmt62719981:24000
Raghorn-Ethridge-Kalsted complex, 15 to 35 percent slopes713E37215128952f9mt62719981:24000
Raghorn-Ethridge-Kalsted complex, 35 to 70 percent slopes713F24115129052fbmt62719981:24000
Ethridge clay loam, 0 to 2 percent slopes81A18815151752nnmt62719981:24000
Ethridge, saline-Zatony clay loams, 2 to 8 percent slopes811C6715149152mtmt62719981:24000
Raghorn-Ethridge-Kalsted complex, 15 to 35 percent slopes2123071465884xjnmt63619831:24000
Raghorn-Ethridge-Kalsted complex, 35 to 70 percent slopes2131531465894xjpmt63619831:24000
Ethridge-Rentsac complex, 2 to 8 percent slopes443C3382517350227s5mt63720141:24000
Ethridge clay loam, 4 to 8 percent slopes146C305186027420frvmt63720141:24000
Ethridge-Reedpoint complex, 2 to 8 percent slopes153C890614967850rbmt63920001:24000
Ethridge clay loam, 4 to 8 percent slopes146C8122149667cnc0mt63920001:24000
Ethridge clay loam, 1 to 4 percent slopes146B4345149666cnbzmt63920001:24000
Ethridge-Reedpoint complex, 8 to 15 percent slopes153D320014967950rcmt63920001:24000
Boxwell-Ethridge complex, 2 to 8 percent slopes444C7901500105131mt63920001:24000
Ethridge-Tanna clay loams, 2 to 8 percent slopes169C22714970050s1mt63920001:24000
Boxwell-Ethridge complex, 8 to 15 percent slopes444D1851500115132mt63920001:24000
Ethridge clay loam, 0 to 4 percent slopes38B21444347699cnt3mt64119941:24000
Ethridge-Gerdrum clay loams, 0 to 4 percent slopes381B14729347696cnt0mt64119941:24000
Ethridge-Beaverell complex, 2 to 8 percent slopes383C3423347698cnt2mt64119941:24000
Ethridge clay loam, 4 to 8 percent slopes38C1915347700cnt4mt64119941:24000
Ethridge clay loam, 0 to 2 percent slopes51A26717125841vh2nmt65519751:24000
Ethridge-Reedpoint complex, 2 to 8 percent slopes153C170361412d42gmt65519751:24000
Ethridge clay loam, 4 to 8 percent slopes146C18361426d42xmt65519751:24000
Ethridge silty clay loam, 0 to 4 percent slopes39B35554348623cprxmt65719901:24000
Ethridge clay loam, 0 to 4 percent slopes439B26272348651cpstmt65719901:24000
Ethridge-Nunemaker silty clay loams, 0 to 4 percent slopes539B11760348709cpvpmt65719901:24000
Kobase-Ethridge clay loams, 4 to 8 percent slopes541C9862348714cpvvmt65719901:24000
Nunemaker-Ethridge silty clay loams, 4 to 8 percent slopes650C2673348765cpxhmt65719901:24000
Ethridge clay loam, 0 to 2 percent slopes51A1611341694cgkdmt66620081:24000
Ethridge clay loam, 2 to 8 percent slopes51B1513341695cgkfmt66620081:24000
Ethridge clay loam, 4 to 8 percent slopes146C81215385741nn0fmt66620081:24000
Ethridge-Reedpoint complex, 2 to 8 percent slopes153C17115387781nn70mt66620081:24000
Ethridge-Tanna clay loams, 2 to 8 percent slopes169C112251367350s1mt66620081:24000
Reedpoint-Tanna-Ethridge complex, 4 to 35 percent slopes5502E8343156661580lmt6691:24000
Ethridge-Kremlin-Yamacall complex, 0 to 8 percent slopes2202C289415648957v1mt6691:24000
Ethridge-Tanna-Reedpoint complex, 2 to 15 percent slopes5401D2718156719582gmt6691:24000
Beavwan-Ethridge-Nebies complex, 2 to 15 percent slopes2408D2089711062rvxhmt6691:24000
Evanston-Ethridge complex, 2 to 15 percent slopes5407E1191636457pc8wmt6691:24000
Ethridge-Urban land-Kremlin complex, 0 to 4 percent slopes12B460886547yrj9mt6691:24000
Ethridge-Reedpoint complex, 8 to 15 percent slopes153D187620200ntcgmt6691:24000
Ethridge clay loam, 4 to 8 percent slopes146C824813382p915mt6691:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopesL3251B816027070692qz6rnd00719981:24000
Ethridge silty clay loam, 0 to 2 percent slopesL0836A13127070342q2mpnd00719981:24000
Belfield, low precipitation-Ethridge-Maltese complex, 2 to 6 percent slopesL0617B35825634582q1xdnd01119691:20000
Belfield, low precipitation-Ethridge-Maltese complex, 2 to 6 percent slopesL0617B16627071262q1xdnd02519811:20000
Belfield, low precipitation-Ethridge-Maltese complex, 2 to 6 percent slopesL0617B276427073182q1xdnd03319851:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopesL3251B128627073432qz6rnd03319851:24000
Tanna-Ethridge silty clay loams, 3 to 6 percent slopesL1025B17627073192qk4bnd03319851:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopesL3251B155727151622qz6rnd05320031:24000
Belfield, low precipitation-Ethridge-Maltese complex, 2 to 6 percent slopesL0617B263227158862q1xdnd08719741:20000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopesL3251B19027159442qz6rnd08719741:20000
Tanna-Ethridge silty clay loams, 3 to 6 percent slopesL1025B18527158922qk4bnd08719741:20000
Ethridge silty clay loam, 2 to 6 percent slopesL0836B9427158892qk44nd08719741:20000
Ethridge silty clay loam, 0 to 2 percent slopesL0836A2127158882q2mpnd08719741:20000

Map of Series Extent

Approximate geographic distribution of the ETHRIDGE 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 .