Official Series Description


Lab Data Summary

Aggregate lab data for the LAS ANIMAS soil series. This aggregation is based on all pedons with a current taxon name of LAS ANIMAS, 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 LAS ANIMAS 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
6489P026988NE165094Las Animas6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4350014,-103.7125015
67A87P064387NE165327Las Animas6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0202789,-103.9375
67A87P064487NE165328Las Animas6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0175018,-103.9311142

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LAS ANIMAS 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 LAS ANIMAS 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 LAS ANIMAS 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 LAS ANIMAS 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 mountains figure.

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Competing Series

Soil series competing with LAS ANIMAS 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 LAS ANIMAS 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 LAS ANIMAS 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with LAS ANIMAS, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CO-2011-05-27-10 | Otero County - 1972

    Rocky Ford-Numa-Kornman soil association (Soil Survey of Otero County, Colorado; 1972).

  2. CO-2011-05-27-11 | Otero County - 1972

    Cross section of Otero County showing relief, drainage, and relation of soils to underlying geologic formations (Soil Survey of Otero County, Colorado; 1972).

  3. CO-2011-05-27-17 | Prowers County - 1966

    Soils on bottom lands and terraces, and the underlying materials of soil association 7 (Soil Survey of Prowers County, Colorado; 1966).

  4. CO-2011-05-27-19 | Prowers County - 1966

    Cross sections showing relationships of the soils to the landscape and to the underlying geologic formations in Prowers County. The upper cross section shows relationships in the western part of the county, and the lower shows those in the eastern part of the county (Soil Survey of Prowers County, Colorado; 1966).

  5. KS-2012-01-23-02 | Finney County - November 1965

    Typical cross section of the valley of the Arkansas River (Soil Survey of Finney County, Kansas; 1965).

  6. KS-2012-01-23-05 | Ford County - August 1965

    A geologic cross section west of Dodge City showing the major soil associations in Ford County (Soil Survey of Ford County, Kansas; 1965).

  7. KS-2012-01-23-18 | Gray County - January 1968

    Soils of the Mansic-Ulysses soil association are on the right; on the left are soils of the Pratt-Tivoli soil association (Soil Survey of Gray County, Kansas; 1968).

  8. KS-2012-01-23-20 | Gray County - January 1968

    Approximate geologic cross section through the central part of Gray County and the general location of soils on the landscape (Soil Survey of Gray County, Kansas; 1968).

  9. NE-2012-02-10-29 | Dundy County - February 1963

    The Bridgeport-Havre soil association, on the right, merges with the Sandy alluvial land-Las association (Soil Survey of Dundy County, Nebraska; February 1963).

  10. OK-2012-02-17-60 | Woodward County - November 1963

    Typical pattern of soils of the Port association (Soil Survey of Woodward County, Oklahoma; November 1963).

  11. OK-2012-02-17-61 | Woodward County - November 1963

    Typical pattern of soils of the Lincoln-Las Animas association (Soil Survey of Woodward County, Oklahoma; November 1963).

Map Units

Map units containing LAS ANIMAS 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
Las Animas loam, 0 to 1 percent slopes, occasionally floodedLm1718942542yz49co01119651:15840
Las Animas sandy loam, 0 to 2 percent slopes, occasionally floodedLm1365943682yz42co02519651:15840
Las Animas sandy loam, 0 to 3 percent slopes, occasionally flooded14525171052263jhdco07320011:24000
Las Animas silty clay, 0 to 3 percent slopes, occasionally floodedLm2989947332xyrhco08919661:15840
Las Animas soilsLt31389484535pjco09919631:15840
Las Animas fine sandy loam2743159507035xsco12519761:24000
Las Animas loam2818629507135xtco12519761:24000
Las Animas fine sandy loam, 0 to 2 percent slopes, frequently floodedLm9753955022xyrgco62619741:24000
Ellicott-Las Animas complex, 0 to 2 percent slopes, occasionally floodedEL261224842762pd2yco62719801:24000
Riverwash-Las Animas complex721421496512jnnjco62719801:24000
Ellicott-Las Animas complex, 0 to 2 percent slopes, occasionally floodedEL458024992512pd2yco62820081:24000
Las Animas loam, 0 to 1 percent slopesLs1971053493jmcco62820081:24000
Las Animas loam, occasionally flooded11824617114955117l69ks02319871:24000
Las Animas loamy fine sand, occasionally flooded118383713803732zt6nks04719671:24000
Las Animas-Lincoln complex, occasionally flooded11873213803752zt78ks04719671:24000
Las Animas sandy loam, occasionally flooded1185113803742zt77ks04719671:24000
Las-Las Animas complex, occasionally flooded12354387115231617p2hks05519621:24000
Las Animas-Lincoln loamy sands, occasionally flooded11884216115231217p2cks05519621:24000
Las Animas sandy loam, occasionally flooded1185193811523102zt77ks05519621:24000
Las Animas soils, occasionally flooded119047115231117p2bks05519621:24000
Las Animas loamy sand, occasionally flooded118445115230917p28ks05519621:24000
Las Animas-Lincoln complex, occasionally flooded1187654613804372zt78ks05719621:24000
Las Animas sandy loam, occasionally flooded1185282413804352zt77ks05719621:24000
Las Animas-Tivoli complex, 0 to 6 percent slopes, occasionally flooded1189119413804381hbg8ks05719621:24000
Las Animas-Lesho complex, alkali, occasionally flooded118638813804361hbg6ks05719621:24000
Lesho, saline-Las Animas complex, occasionally flooded2155178713806621hbphks06719651:24000
Las Animas soils, occasionally flooded1190417013805691hblhks06919651:24000
Las Animas-Lesho complex, alkali, occasionally flooded1186324813805701hbljks06919651:24000
Las Animas sandy loam, occasionally flooded118597313805682zt77ks06919651:24000
Las-Las Animas complex, occasionally flooded1235913805721hbllks06919651:24000
Las Animas loamy sand, occasionally flooded11843314115221817nzbks07519591:24000
Las Animas sandy loam, occasionally flooded1185278011522192zt77ks07519591:24000
Las variant-Las Animas complex, occasionally flooded1233364115222517nzkks07519591:24000
Las Animas loamy sand, occasionally flooded11843713115226517p0vks09319611:24000
Las Animas sandy loam, occasionally flooded1185261711522662zt77ks09319611:24000
Las-Las Animas complex, occasionally flooded12352101115227017p10ks09319611:24000
Las Animas sandy loam, occasionally flooded1185207811505252zt77ks10919621:24000
Las Animas sandy loam, occasionally flooded1185266313826201hdqnks17519631:24000
Las Animas-Lisco very fine sandy loams, occasionally flooded11892936357806d0b4ne01319801:20000
Las Animas-Lisco complex, occasionally flooded1188105022174482dfflne01319801:20000
Las Animas loam, frequently flooded118470516986951v0mmne03319891:20000
Las Animas loam, channeled, frequently flooded118318622196952dhs2ne03319891:20000
Las Animas soils, 0 to 2 percent slopes11871815358124d0ndne04519731:20000
Las Animas loam, channeled, frequently flooded1183135916988131v0rfne04920001:24000
Las Animas loam, occasionally flooded118246716988141v0rgne04920001:24000
Las Animas loam, channeled, occasionally flooded1186181116925491tt7cne10520041:24000
Las Animas loam, occasionally flooded1182139316994621v1fcne14519651:20000
Las Animas sand, occasionally flooded119814816994351v1dhne14519651:20000
Las Animas fine sandy loam, occasionally flooded1180313016537561shvzne15719651:20000
Las Animas loam, occasionally flooded118259416537571shw0ne15719651:20000
Las Animas fine sandy loam, channeled, frequently flooded1181322276592ds1zne15719651:20000
Las Animas loam, occasionally flooded11825781006103cphne16119921:20000
Las Animas-Lisco complex, occasionally flooded11885498357933d0g7ne16519931:20000
Las Animas fine sandy loam, occasionally flooded118022843579312zj4pne16519931:20000
Las Animas fine sandy loam, channeled, frequently flooded11816043579322zj4qne16519931:20000
Las Animas fine sandy loam, 0 to 2 percent slopes15542349624cqt6wy02719931:24000
Baroid-Las Animas variant sandy loams82255152128539cwy04319761:24000
Baroid-Las Animas complex, wet, 0 to 3 percent slopes -- Draft509A628115224153f0wy6031:24000
Las Animas-Lisco complex, 0 to 2 percent slopes, occasionally flooded9228614153781jhtcwy71519741:20000
Las Animas fine sandy loam, channeled, 0 to 2 percent slopes932714153791jhtdwy71519741:20000

Map of Series Extent

Approximate geographic distribution of the LAS ANIMAS 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 .