Official Series Description


Lab Data Summary

Aggregate lab data for the OTERO soil series. This aggregation is based on all pedons with a current taxon name of OTERO, 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 OTERO 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
67A40A3463S1953WY015005Otero6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.914444,-104.3249969
67A79P0070S1978NE123012OTERO6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6996994,-103.063858
70C95P070395NM057002Otero7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.76091,-105.7458344
7288P053688CO063184Otero6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4480553,-102.5124969
7288P053888CO063253Otero6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3997231,-102.6863861
77E89P072689KS081002Otero7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4049988,-101.0333328

Water Balance

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

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

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

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Soil series sharing subgroup-level classification with OTERO, 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-2011-05-27-04 | Crowley County - 1968

    Relationship of soils to typography and underlying material in association 2 (Soil Survey of Crowley County, Colorado; 1968).

  2. CO-2011-05-27-07 | Otero County - 1972

    Volney-Olney-Dwyer association; part of Minnequa-Penrose soil association in background (Soil Survey of Otero County, Colorado; 1972).

  3. 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).

  4. KS-2012-01-20-19 | Cheyenne County - June 1989

    Typical pattern of soils and parent material in the Colby-Razor association (Soil Survey of Cheyenne County, Kansas; 1989).

  5. KS-2012-01-20-21 | Cheyenne County - June 1989

    Typical pattern of soils and parent material in the Manter-Satanta-Kim association (Soil Survey of Cheyenne County, Kansas; 1989).

  6. KS-2012-01-23-04 | Finney County - November 1965

    Typical cross section of the Manter-Keith association (Soil Survey of Finney County, Kansas; 1965).

  7. KS-2012-01-23-13 | Grant County - December 1969

    Relationships of soils in association 2 (Soil Survey of Grant County, Kansas; 1969).

  8. KS-2012-01-23-14 | Grant County - December 1969

    Relationships of soils in association 3 (Soil Survey of Grant County, Kansas; 1969).

  9. KS-2012-01-23-16 | Grant County - December 1969

    Relationships of soils in association 5 (Soil Survey of Grant County, Kansas; 1969).

  10. KS-2012-01-23-31 | Haskell County - October 1968

    Soils of the Richfield-Ulysses association in the central part of the county (Soil Survey of Haskell County, Kansas; 1968).

  11. KS-2012-01-23-33 | Haskell County - October 1968

    Typical topographic relation of three soil associations: Otero-Colby-Likes association in the southwestern corner; Richfield-Ulysses association to the north; and Satanta-Manter association to the east (Soil Survey of Haskell County, Kansas; 1968).

  12. KS-2012-01-25-34 | Scott County - December 1965

    An approximate geologic profile extending in an east-west direction across Scott County near Shallow Water (Soil Survey of Scott County, Kansas; 1965).

  13. KS-2012-01-26-25 | Wallace County - March 1986

    Typical pattern of soils and underlying material in the Colby-Kim-Midway association (Soil Survey of Wallace County, Kansas; 1986).

  14. NE-2012-02-08-02 | Banner County - October 1994

    Typical pattern of soils and parent material in the Tassel-Busher-Rock outcrop association (Soil Survey of Banner County, Nebraska; October 1994).

  15. NE-2012-02-08-03 | Banner County - October 1994

    Typical pattern of soils and parent material in the Otero-Bayard-Sarben association (Soil Survey of Banner County, Nebraska; October 1994).

  16. NE-2012-02-10-09 | Chase County - November 1982

    Typical landscape pattern of the soils and underlying material in the Colby association (Soil Survey of Chase County, Nebraska; November 1982).

  17. NE-2012-02-13-41 | Keith County - November 1995

    Typical pattern of soils and parent material in the Sully-Dix-Tassel association (Soil Survey of Keith County, Nebraska; November 1995).

  18. NE-2012-02-13-57 | Morrill County - August 1985

    Pattern of soils, topography, and underlying material in the Mitchell-Otero-Bridget association (Soil Survey of Morrill County, Nebraska; August 1985).

  19. NE-2012-02-13-58 | Morrill County - August 1985

    Pattern of soils, topography, and underlying material in the Tripp-Alice-Duroc association (Soil Survey of Morrill County, Nebraska; August 1985).

  20. NE-2012-02-13-59 | Morrill County - August 1985

    Pattern of soils, topography, and underlying material in the Valent-Sarben-Otero association (Soil Survey of Morrill County, Nebraska; August 1985).

  21. NE-2012-02-13-60 | Morrill County - August 1985

    A generalized cross section of Morrill County that shows the relationship of parent material, soil associations, and elevation (Soil Survey of Morrill County, Nebraska; August 1985).

  22. NM-2012-02-14-02 | Harding County - November 1973

    Typical pattern of soils in association 8 in the north-central part of the county (Soil Survey of Harding County, New Mexico; November 1973).

  23. OK-2012-02-16-03 | Beaver County - August 1962

    Parent material and parent rock of most of the soils in Beaver County, and their position on the landscape (Soil Survey of Beaver County, Oklahoma; August 1962).

  24. OK-2012-02-16-09 | Cimarron County - June 1960

    Typical landscape in the central and eastern part of Cimarron County: Associations 1, 2, 3, and 5 (Soil Survey of Cimarron County, Oklahoma; June 1960).

  25. OK-2012-02-16-30 | Ellis County - April 1966

    Major soils of associations 7, 8, and 10 (Soil Survey of Ellis County, Oklahoma; April 1966).

Map Units

Map units containing OTERO 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
Otero sandy loam, 1 to 3 percent slopesOeB69032942072w4pjco00919661:20000
Otero sandy loam, 3 to 6 percent slopesOeD29977942082w4pkco00919661:20000
Otero-Lithic Calciustepts complex, 1 to 9 percent slopesOp10519942062w4pmco00919661:20000
Otero-Olney sandy loams, 3 to 6 percent slopes, eroded34588594323354pco01719851:24000
Otero-Ordway sandy loams, 1 to 9 percent slopesOuC4075943973572co02519651:15840
Manter-Otero complex, 1 to 6 percent slopes4965639684637s2co06319961:24000
Otero sandy loam, 1 to 13 percent slopes633379968562w4plco06319961:24000
Julesburg-Otero complex, 1 to 9 percent slopes3418189683137rlco06319961:24000
Otero sandy loam, 1 to 3 percent slopes16930121052502w4pjco07320011:24000
Otero sandy loam, 3 to 6 percent slopesOtC2059948652w4pkco09919631:15840
Otero sandy loam, 1 to 3 percent slopesOtB456948642w4pjco09919631:15840
Otero-Tassel complex, 6 to 30 percent slopes4815212951413602co61719801:24000
Otero sandy loam, 3 to 9 percent slopes4713653951403601co61719801:24000
Otero sandy loam, 0 to 3 percent slopes467119951393600co61719801:24000
Otero sandy loam, 1 to 3 percent slopes5130831952323630co61819761:24000
Otero sandy loam, 3 to 5 percent slopes5213570952333631co61819761:24000
Otero sandy loam, 5 to 9 percent slopes536397952343632co61819761:24000
Otero sandy loam, 0 to 1 percent slopes50444795231362zco61819761:24000
Otero gravelly sandy loam, 3 to 9 percent slopesOrD84499552436dfco62619741:24000
Otero clay loam, 1 to 3 percent slopeOtB29089552636dhco62619741:24000
Otero clay loam, 0 to 1 percent slopesOtA22749552536dgco62619741:24000
Otero fine sandy loam, 1 to 9 percent slopes639106496502jnn6co62719801:24000
Otero sandy loam, cool, 1 to 9 percent slopes6266124965012t51zco62719801:24000
Minnequa-Otero sandy loams, 2 to 12 percent slopes473516496484jnmmco62719801:24000
Otero sandy loam, 3 to 6 percent slopesOeC50221053972w4pkco62820081:24000
Otero sandy loam, cool, 1 to 9 percent slopesOtC331028380052t51zco62820081:24000
Otero fine sandy loam, 3 to 8 percent slopes81437498351jqkvco63719861:24000
Ascalon-Otero complex, 3 to 5 percent slopesAoC27354975562yqppco64319751:20000
Ascalon-Otero complex, 5 to 9 percent slopesAoD24074975572yqpqco64319751:20000
Ascalon-Otero complex, 9 to 20 percent slopesAoE18184975582yqprco64319751:20000
Ascalon-Otero complex, 0 to 3 percent slopesAoB11104975552yqpnco64319751:20000
Otero-Nelson sandy loams, 3 to 25 percent slopes806385497732jpxwco64419801:24000
Otero sandy loam, 3 to 5 percent slopes781816497729jpxsco64419801:24000
Otero sandy loam, 0 to 3 percent slopes771512497728jpxrco64419801:24000
Otero sandy loam, 5 to 9 percent slopes791319497730jpxtco64419801:24000
Otero sandy loam, 5 to 9 percent slopes, foothills21058732102432zf0xco64419801:24000
Otero fine sandy loam, 7 to 15 percent slopes170626129114957317l70ks02319871:24000
Otero fine sandy loam, 0 to 1 percent slopes170335114957217l6zks02319871:24000
Otero-Ulysses complex, 0 to 5 percent slopes17131692827680742r9kzks05519621:24000
Manter-Otero fine sandy loams, 1 to 3 percent slopes16722053115232417p2rks05519621:24000
Otero fine sandy loam, 7 to 15 percent slopes17061336115232917p2xks05519621:24000
Otero-Schamber complex, 5 to 20 percent slopes17121312115233117p2zks05519621:24000
Otero fine sandy loam, 3 to 7 percent slopes1705355115232817p2wks05519621:24000
Otero soils, 3 to 20 percent slopes170731115233017p2yks05519621:24000
Otero fine sandy loam, 3 to 7 percent slopes170557513804461hbgjks05719621:24000
Otero-Manter complex, warm, 3 to 6 percent slopes17103013804472y7zhks05719621:24000
Otero fine sandy loam, 1 to 3 percent slopes17042888115068917md0ks06319741:24000
Otero-Manter fine sandy loams, 1 to 3 percent slopes17091152113806681hbppks06719651:24000
Otero fine sandy loam, 7 to 15 percent slopes1706778913806671hbpnks06719651:24000
Otero-Schamber complex, warm, 5 to 20 percent slopes1712129513806692y7zfks06719651:24000
Otero-Vona complex, 5 to 15 percent slopes17143213115223117nzrks07519591:24000
Otero fine sandy loam, 1 to 3 percent slopes1704487115222917nzpks07519591:24000
Otero-Manter fine sandy loams, 1 to 3 percent slopes1709326115223017nzqks07519591:24000
Otero-Ulysses complex, 0 to 5 percent slopes1713399127680782r9kzks08119651:24000
Otero-Schamber complex, warm, 5 to 20 percent slopes1712231313806262y7zfks08119651:24000
Otero-Schamber complex, 5 to 20 percent slopes1712947115239017p4wks08319661:24000
Otero-Schamber complex, 5 to 20 percent slopes17125126115227517p15ks09319611:24000
Otero-Vona complex, 5 to 15 percent slopes1714163115227617p16ks09319611:24000
Otero soils, 3 to 20 percent slopes1707784115203117ns9ks10119661:24000
Otero fine sandy loam, 3 to 7 percent slopes1705622115203017ns8ks10119661:24000
Otero fine sandy loam, 7 to 15 percent slopes17063169115053917m75ks10919621:24000
Kim-Otero complex, 6 to 25 percent slopes1634458115052317m6nks10919621:24000
Otero-Mansic complex, 5 to 25 percent slopes17083961113818022w84pks11919731:24000
Otero fine sandy loam, warm, 6 to 15 percent slopes17061009213818012y7zdks11919731:24000
Otero-Manter complex, warm, 3 to 6 percent slopes1710498513818032y7zhks11919731:24000
Otero fine sandy loam, 7 to 15 percent slopes1706181613826071hdq7ks12919951:24000
Otero fine sandy loam, 1 to 3 percent slopes17041697115198917nqyks17119631:24000
Otero soils, 3 to 20 percent slopes17071158115199117nr0ks17119631:24000
Otero fine sandy loam, 3 to 7 percent slopes1705318115199017nqzks17119631:24000
Manter-Otero fine sandy loams, 1 to 3 percent slopes167234115198517nqtks17119631:24000
Otero-Schamber complex, warm, 5 to 20 percent slopes17121989113826312y7zfks17519631:24000
Otero-Mansic complex, 1 to 4 percent slopes1711930613826302y7zgks17519631:24000
Otero-Mansic complex, 5 to 25 percent slopes1708160013826282w84pks17519631:24000
Otero-Manter complex, warm, 3 to 6 percent slopes17102213826292y7zhks17519631:24000
Kim-Otero complex, 6 to 25 percent slopes16343244114962117l8kks18119671:24000
Otero-Manter fine sandy loams, 1 to 3 percent slopes1709142613825671hdnyks18719591:24000
Otero fine sandy loam, 1 to 3 percent slopes170415115087017mkvks19519861:24000
Kim-Otero complex, 6 to 25 percent slopes163425662115019817lw5ks19919841:24000
Otero loamy very fine sand, 0 to 3 percent slopes17041251516924981tt5qne00719881:20000
Otero loamy very fine sand, 3 to 9 percent slopes1719602816924991tt5rne00719881:20000
Otero-Epping complex, 9 to 60 percent slopes1718401716925011tt5tne00719881:20000
Otero loamy very fine sand, 9 to 20 percent slopes1707199016925001tt5sne00719881:20000
Otero loamy very fine sand, 0 to 3 percent slopes17045022174492dffmne01319801:20000
Otero-Canyon loams, 6 to 20 percent slopes17171279416990511v103ne02919801:20000
Otero fine sandy loam, 0 to 1 percent slopes1703368216990961v11kne05719951:24000
Otero fine sandy loam, 0 to 1 percent slopes17032622288422dt94ne08719651:20000
Tassel-Otero-Rock outcrop complex, 15 to 60 percent slopes6042948016989201v0vwne10119901:20000
Otero loamy very fine sand, 9 to 20 percent slopes17071369316926451ttbgne12319811:20000
Otero very fine sandy loam, 0 to 3 percent slopes17091284216926461ttbhne12319811:20000
Otero very fine sandy loam, 6 to 9 percent slopes1711802016926481ttbkne12319811:20000
Otero very fine sandy loam, 3 to 6 percent slopes1710758816926471ttbjne12319811:20000
Otero loamy very fine sand, 0 to 6 percent slopes1705479216926441ttbfne12319811:20000
Otero variant very fine sandy loam, 0 to 1 percent slopes1708151116926491ttblne12319811:20000
Otero loamy very fine sand, 0 to 3 percent slopes170418322203742djgzne12319811:20000
Otero-Epping complex, 9 to 60 percent slopes171815322203792djh4ne12319811:20000
Otero loamy very fine sand, 3 to 9 percent slopes171912022203802djh5ne12319811:20000
Otero-Bayard fine sandy loams, 0 to 3 percent slopes17121674916537731shwjne15719651:20000
Otero-Bayard fine sandy loams, 3 to 6 percent slopes1713436916537741shwkne15719651:20000
Otero fine sandy loam, 1 to 6 percent slopes1701413516537791shwqne15719651:20000
Otero-Bayard fine sandy loams, 6 to 9 percent slopes1714253516537751shwlne15719651:20000
Bridget-Otero complex, 3 to 6 percent slopes, eroded1366199716537541shvxne15719651:20000
Otero fine sandy loam, 6 to 12 percent slopes1702149616537801shwrne15719651:20000
Bridget-Otero complex, 6 to 9 percent slopes1367145116537551shvyne15719651:20000
Otero-Bayard very fine sandy loams, 0 to 1 percent slopes1715124816537761shwmne15719651:20000
Otero loamy fine sand, 0 to 6 percent slopes1700106316537771shwnne15719651:20000
Otero loamy very fine sand, 0 to 3 percent slopes170455822276412ds1dne15719651:20000
Otero very fine sandy loam, 0 to 3 percent slopes170929422276852ds2tne15719651:20000
Otero-Epping complex, 9 to 60 percent slopes171829222276422ds1fne15719651:20000
Otero variant very fine sandy loam, 0 to 1 percent slopes170810122276842ds2sne15719651:20000
Otero very fine sandy loam, 3 to 6 percent slopes171010022276862ds2vne15719651:20000
Otero very fine sandy loam, 6 to 9 percent slopes17113722276872ds2wne15719651:20000
Otero loamy very fine sand, 0 to 3 percent slopes170422094357984d0hwne16519931:20000
Otero loamy fine sand, 1 to 9 percent slopesOr11589376369dmmynm02119681:31680
Otero fine sandy loamOs10195376370dmmznm02119681:31680
Otero fine sandy loamOT2548376368dmmxnm02119681:31680
Otero fine sandy loamOT4873556711vxvnm60019731:24000
Otero and Palma soilsOp6886714739451lgrmnm67419651:24000
Kim-Otero-Pastura complexKo710314739271lgr1nm67419651:24000
Otero and Palma soils, hummockyOr147014739461lgrnnm67419651:24000
Otero loamy fine sand, 1 to 5 percent slopesOa15495382066dtkqok02519581:20000
Oklark-Otero complex, 1 to 3 percent slopesMrB13275382447dtz0ok04519631:24000
Oklark-Otero complex, 3 to 5 percent slopesMrC12168382448dtz1ok04519631:24000
Otero-Berda complex, 3 to 12 percent slopesOm9171382452dtz5ok04519631:24000
Otero fine sandy loam, 3 to 8 percent slopesOtC5273382454dtz7ok04519631:24000
Otero and Mobeetie soils, 5 to 12 percent slopes, severely erodedEr4177382432dtyjok04519631:24000
Otero fine sandy loam, 0 to 3 percent slopesOtB3189382453dtz6ok04519631:24000
Vona, Otero, and Plack soils, 3 to 20 percent slopesVp25964384930dxk3ok13919591:24000
Otero-Vona complex, 3 to 12 percent slopesOv15312384915dxjmok13919591:24000
Otero fine sandy loam, 3 to 8 percent slopesOt10182384914dxjlok13919591:24000
Otero loamy fine sand, 0 to 3 percent slopesOtB1737385288dxxnok15319611:24000
Otero sandy loam, cool, 2 to 6 percent slopesP306B1527680962rvg1sd01919701:24000
Otero-Glenberg families complex696075551991vfmut63119821:24000
Otero sandy loam, cool, 6 to 10 percent slopesP306C46227457822rvg2wy01119781:24000
Otero sandy loam, cool, 2 to 6 percent slopesP306B36527457812rvg1wy01119781:24000
Otero sandy loam, 2 to 6 percent slopes132339349212cqcxwy01119781:24000
Otero sandy loam, 6 to 10 percent slopes133253349213cqcywy01119781:24000
Otero fine sandy loam, 0 to 3 percent slopesOtA42401047303hzdwy61519651:20000
Bayard and Otero fine sandy loams, 0 to 3 percent slopesBoA30481046683hxdwy61519651:20000
Otero fine sandy loam, 3 to 6 percent slopesOtB25911047313hzfwy61519651:20000
Otero-Glenberg complex, 0 to 3 percent slopes4512491046493hwswy61519651:20000
Otero fine sandy loam, 6 to 10 percent slopesOtC9341047323hzgwy61519651:20000
Bayard and Otero fine sandy loams, 3 to 6 percent slopesBoB6791046693hxfwy61519651:20000
Otero-Kim associationOK3375350899cs4bwy61919711:24000
Tassel-Otero-Rock outcrop complex, 10 to 30 percent slopes37164101048343j2rwy62119801:24000
Otero fine sandy loam, 3 to 6 percent slopes3457631048243j2fwy62119801:24000
Otero fine sandy loam, 0 to 3 percent slopes3353511048233j2dwy62119801:24000
Otero fine sandy loam, 6 to 10 percent slopes3518281048253j2gwy62119801:24000
Dix-Otero complex, 6 to 10 percent slopes1611421048043j1swy62119801:24000
Otero fine sandy loam, 0 to 6 percent slopes21B89001048653j3rwy71519741:20000
Otero fine sandy loam, 6 to 10 percent slopes21C46361048663j3swy71519741:20000
Otero loamy very fine sand, 0 to 3 percent slopes8830914153741jht7wy71519741:20000
Otero-Valent-Tassel complex, 0 to 15 percent slopes151114251049523j6kwy72119941:24000
Otero fine sandy loam, 0 to 6 percent slopes15021451049513j6jwy72119941:24000

Map of Series Extent

Approximate geographic distribution of the OTERO 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 .