Official Series Description


Lab Data Summary

Aggregate lab data for the EAGLEPASS soil series. This aggregation is based on all pedons with a current taxon name of EAGLEPASS, 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 EAGLEPASS 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 EAGLEPASS 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 EAGLEPASS 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 EAGLEPASS 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 EAGLEPASS 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 EAGLEPASS 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 EAGLEPASS 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 EAGLEPASS 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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Click the image to view it full size.

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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 EAGLEPASS, 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 EAGLEPASS 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
Eaglepass-Rock outcrop complex, 30 to 75 percent slopes501ec33323906272l7n0ca76319841:24000
Kyler-Eaglepass-Rock outcrop association, warmKER6136450692s224nv61119671:24000
Radol-Eaglepass-Rock outcrop association2103324224062902lry8nv70820091:24000
Eaglepass-Rock outcrop association5160167024061212lrrtnv70820091:24000
Logring-Hyzen-Canyoung association510092524061182lrrqnv70820091:24000
Eaglepass-Rock outcrop-Amtoft association3439524208462m82tnv70820091:24000
Eaglepass-Rock outcrop-Amtoft association3439585124062092tzgcnv70920121:24000
Radol-Eaglepass-Rock outcrop association2103112025157442tzfznv70920121:24000
Lodar-Eaglepass-Rock outcrop association4014109124062142lrvtnv70920121:24000
Logring-Eaglepass-Canyoung association510023124061632lrt5nv70920121:24000
Kyler-Eaglepass-Rock outcrop association10921924061952tzg0nv70920121:24000
Eaglepass-Rock outcrop complex, 15 to 75 percent slopes1492369324805762s21nnv71320141:24000
Kyler-Eaglepass-Rock outcrop association1090179724804952p84znv71320141:24000
Kyler-Eaglepass-Rock outcrop association, warm10917924804962s224nv71320141:24000
Kyler-Eaglepass-Rock outcrop association, warm1570176524781222s224nv75419921:24000
Logring-Eaglepass-Rock outcrop complex10915988478034j1fgnv75419921:24000
Eaglepass-Amtoft association16002746478668j22xnv76619941:24000
Theriot-Eaglepass-Rock outcrop association20312577476853j06cnv77419851:24000
Logring-Eaglepass-Kyler complex, 15 to 75 percent slopes70021560477015j0clnv77419851:24000
Eaglepass-Rock outcrop complex, 15 to 75 percent slopes409013224769332s21nnv77419851:24000
Eaglepass-Rock outcrop-Amtoft association3439774722157032dcm9nv77820131:24000
Radol-Eaglepass-Rock outcrop association2103549825130112tzgynv77820131:24000
Radol-Amtoft-Eaglepass association3032502425130152tzjpnv77820131:24000
Eaglepass-Zarark-Haunchee association3361193224854652pfb9nv77820131:24000
Kyler-Eaglepass-Rock outcrop association1092107422156092dcj8nv77820131:24000
Monarch-Eaglepass-Rock outcrop association410695422157302dcn5nv77820131:24000
Amtoft-Eaglepass association303466022156742dclcnv77820131:24000
Logring-Kyler-Eaglepass association367250725128982whnnnv77820131:24000
Eaglepass-Rock outcrop-Amtoft association343928896480077j3kcnv77920041:24000
Amtoft-Eaglepass association30346195479994j3gpnv77920041:24000
Kyler-Amtoft-Eaglepass association13073107479955j3ffnv77920041:24000
Kyler-Eaglepass-Rock outcrop association10923058780492v655nv77920041:24000
Amtoft-Eaglepass-Rock outcrop association40102137480108j3lcnv77920041:24000
Monarch-Eagleass-Rock outcrop association41061858480125j3lxnv77920041:24000
Radol-Amtoft-Eaglepass association30328874799922qc1ynv77920041:24000
Radol-Eaglepass-Rock outcrop association210323528172422tzhfnv77920041:24000
Eaglepass-Zarark-Haunchee association336117728172452tzhknv77920041:24000
Lodar-Eaglepass-Rock outcrop association401416626194592rbsvnv77920041:24000
Kyler-Eaglepass-Rock outcrop association, warm65088504805642s224nv78019901:24000
Zimbob-Eaglepass association11528064480175j3njnv78019901:24000
Logring-Kyler-Eaglepass association3672362954810242whnnnv78319911:24000
Kyler-Eaglepass-Rock outcrop association, warm3570176784809982s224nv78319911:24000
Eaglepass-Kyler-Rock outcrop complex, 15 to 75 percent slopes357212619481000j4j4nv78319911:24000
Eaglepass-Rock outcrop-Amtoft association19004715190455921xvdnv78319911:24000
Haunchee-Eaglepass-Rock outcrop association31403684480917j4fgnv78319911:24000
Eaglepass-Rock outcrop complex, 15 to 75 percent slopes357134794809992s21nnv78319911:24000
Logring-Eaglepass association36713048481023j4jwnv78319911:24000
Kyler-Eaglepass-Rock outcrop association, warm1091633314811212s224nv78420061:24000
Kyler-Eaglepass-Rock outcrop association109027151481120j4n0nv78420061:24000
Logring-Kyler-Eaglepass association3670106774812082whnnnv78420061:24000
Lodar-Eaglepass-Rock outcrop association40149943114452117dz1nv78420061:24000
Kyler-Amtoft-Eaglepass association1307223313956221hv82nv78420061:24000
Radol-Eaglepass-Monarch association1088115914045461j4jynv78420061:24000
Eaglepass-Rock outcrop-Amtoft association190010001454684j3kcnv78420061:24000
Lodar-Eaglepass-Radol association192281416022171qs7fnv78420061:24000
Eaglepass-Rock outcrop complex, 15 to 75 percent slopes50111144850722s21nnv79619841:63360

Map of Series Extent

Approximate geographic distribution of the EAGLEPASS 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 .