Official Series Description


Lab Data Summary

Aggregate lab data for the HOLTER soil series. This aggregation is based on all pedons with a current taxon name of HOLTER, 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 HOLTER 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
43B92P050391MT049012Holter6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9174004,-112.1933899

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HOLTER 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 HOLTER 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 HOLTER 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 HOLTER 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with HOLTER 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 HOLTER 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 HOLTER 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 HOLTER, 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 HOLTER 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
Holter-Detra complex, 3 to 25 percent slopes, extremely stony1024896497061jp77co68619921:31680
Holter-Detra family complex, 3 to 25 percent slopes, extremely stony253710506241jzscco69219981:24000
Darret, very bouldery-Abac, extremely bouldery-Holter, very bouldery complex, 8 to 35 percent slopes540E373039581wf1cmt60219631:20000
Darret, very bouldery-Abac, extremely bouldery-Holter, very bouldery complex, 8 to 35 percent slopes540E1902694634wf1cmt62420211:24000
Holter-Castner channery loams, 8 to 45 percent slopes3061E3215165252t0mt62719981:24000
Holter-Castner channery loams, 8 to 45 percent slopes61E501221478724yw2mt63019911:24000
Castner-Holter-Rock outcrop complex, 15 to 60 percent slopes360F254561477964ysmmt63019911:24000
Tolex-Holter-Castner channery loams, 8 to 45 percent slopes763E115291479054yx4mt63019911:24000
Darret, very bouldery-Abac, extremely bouldery-Holter, very bouldery complex, 8 to 35 percent slopes540E115124862652pg53mt6321:24000
Holter-Castner complex, 8 to 35 percent slopes61E17024862972pg64mt6321:24000
Windham-Holter-Lap complex, 8 to 35 percent slopes763E10524862742pg5dmt6321:24000
Castner-Holter-Rock outcrop complex, 15 to 60 percent slopes360F1830940844ysmmt6321:24000
Darret, very bouldery-Abac, extremely bouldery-Holter, very bouldery complex, 8 to 35 percent slopes540E5018816892wf1cmt63720141:24000
Windham-Holter-Lap complex, 8 to 35 percent slopes763E21061480744z2lmt63720141:24000
Holter-Castner complex, 8 to 35 percent slopes61E15321480584z22mt63720141:24000
Perma-Holter-Sharrott families complex, steep mountain slopes30K3142324226672m9zkmt63819851:24000
Holter-Tolman families complex, dissected mountain slopes31K3728624226682m9zlmt63819851:24000
Holter-Repp-Sharrott families complex, breaklands61K545824226662m9zjmt63819851:24000
Holter-Whitlash families, complex, dissected mountain slopes31K566723754420tb14mt64520131:12000
Holter-Tolman families, complex, dissected mountain slopes31K373670633773p8h9mt64520131:12000
Perma-Holter-Sharrott families, complex, steep mountain slopes30K312318633763p8gzmt64520131:12000
Holter-Tolman families, complex, steep mountain slopes30M702212633765p8h1mt64520131:12000
Holter-Specie-Sharrott families, complex, breaklands61K5498413895591hmyhmt64520131:12000
Holter-Tolman families, complex, moderately steep mountain slopes32M71846633780p8hjmt64520131:12000
Holter-Tolman families, complex, moderately steep mountain slopes, moist32K31468633777p8hfmt64520131:12000
Tolman-Holter families-Rock outcrop complex, breaklands61M7025424238172mc5nmt64520131:12000
Holter-Whitlash families, complex, dissected mountain slopes31K561431015027251chmt64720071:24000
Holter-Tolman families, complex, dissected mountain slopes31K37640015027051cfmt64720071:24000
Holter-Specie-Sharrott families, complex, breaklands61K54630715036351gfmt64720071:24000
Perma-Holter-Sharrott families, complex, steep mountain slopes30K31500515025051bsmt64720071:24000
Holter-Tolman families, complex, steep mountain slopes30M70293715025351bwmt64720071:24000
Holter-Tolman families, complex, moderately steep mountain slopes, moist32K31213215029551d7mt64720071:24000
Tolman-Holter families-Rock outcrop complex, breaklands61M70210615036551ghmt64720071:24000
Holter-Tolman families, complex, moderately steep mountain slopes32M71185815029851dbmt64720071:24000
Holter-Tolman-Wilde families, complex, breaklands61M7478215037951gymt64720071:24000
Totelake-Holter-Sharrott families, association, dissected mountain slopes31W156915027351cjmt64720071:24000
Darret, very bouldery-Abac, extremely bouldery-Holter, very bouldery complex, 8 to 35 percent slopes540E48329952532pg53mt66620081:24000
Holter, moist-Midfork families association, 10 to 40 percent slopes2051845512426k66wut6461:24000
Holter, very stony-Clasoil-Roaringlion-like complex, 4 to 35 percent slopes940833583132ynpgwy6171:24000
Holter, very stony-Clasoil-Roaringlion-like complex, 4 to 35 percent slopes940831333172ynpgwy6291:24000
Holter-Bowery-like, very bouldery-Mec complex, 8 to 45 percent slopes941932090642zdqxwy6291:24000
Macmeal, bouldery-Holter, stony-Rock outcrop complex, 45 to 70 percent slopes460432090372zdq1wy6291:24000
Kellygulch-like-Holter-Rock outcrop complex, 35 to 70 percent slopes461032504492zv65wy6291:24000
Holter, very stony-Clasoil-Roaringlion-like complex, 4 to 35 percent slopes940833029092ynpgwy65620081:24000
Kellygulch-like-Holter-Rock outcrop complex, 35 to 70 percent slopes461032505262zv65wy65620081:24000

Map of Series Extent

Approximate geographic distribution of the HOLTER 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 .