Official Series Description


Lab Data Summary

Aggregate lab data for the ULYSSES soil series. This aggregation is based on all pedons with a current taxon name of ULYSSES, 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 ULYSSES 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
67B11N0414S2011CO099002Ulysses8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0888611,-102.2312222
67B11N0416S2011CO099004Ulysses8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1325278,-102.4148056
7292KS12906192KS129061Ulysses1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.256321,-101.7728119
7240A2268S1954NE087002Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0577774,-101.1158371
7240A2269S1954NE087003Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.075833,-101.040611
7240A1811S1957KS075005Ulysses6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.844611,-101.579806
7240A1813S1957KS109003Ulysses6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9680472,-101.1636805
7240A1814S1957KS109004Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9265694,-101.2596417
7287P0017S1986KS063016Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7615389,-100.349725
7287P0026S1986KS093007Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0977778,-101.2630556
7287P0029S1986KS093013Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1033333,-101.2786444
7288P0864S1988KS193002Ulysses7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2438889,-101.1338882
7289P0136S1988NE057004Ulysses6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3301944,-101.4489722
7289P0137S1988NE057005Ulysses6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3072205,-101.4205551
7289P0741S1989KS081006Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4273083,-101.0335694
7289P0734S1989KS081007Ulysses8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4730555,-101.0061111
7289P0737S1989KS081016Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4260806,-101.0381972
7290P0719S1990NE057020Ulysses7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0165556,-101.7217056
7291P0807S1991KS081006Ulysses6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6077778,-100.6602778
7291P0809S1991KS081008Ulysses6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6294441,-100.8911133
7295P0481S1995KS181002Ulysses6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2746444,-101.6377167
7295P0486S1995KS193005Ulysses5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1612111,-101.3525333
7203N0883S2003KS171001Ulysses7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6904444,-100.7664722
7203N0884S2003KS171002Ulysses7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3349167,-100.7867778
7205N0784S2005KS193007Ulysses7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2736111,-101.1120556
7214N0264S2013KS203001Ulysses8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5747139,-101.4447028
77E89P0727S1989KS081003Ulysses8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4101,-101.034125

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ULYSSES 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 ULYSSES 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 ULYSSES 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 ULYSSES 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 ULYSSES 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 ULYSSES 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 ULYSSES 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 hills figure.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with ULYSSES, 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-2011-05-27-15 | Prowers County - 1966

    Main soils and underlying materials in soil association 2 (Soil Survey of Prowers County, Colorado; 1966).

  2. 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).

  3. 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).

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

    Typical pattern of soils and parent material in the Colby-Ulysses-Keith 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-2012-01-23-01 | Finney County - November 1965

    Typical cross section of the Pawnee River drainage basin (Soil Survey of Finney County, Kansas; 1965).

  7. 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).

  8. KS-2012-01-23-03 | Finney County - November 1965

    Typical cross section of the Scott-Finney depression (Soil Survey of Finney County, Kansas; 1965).

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

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

  10. 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).

  11. KS-2012-01-23-12 | Grant County - December 1969

    Relationships of soils in association 1. Included is a small part of association 3 (Soil Survey of Grant County, Kansas; 1969).

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

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

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

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

  14. KS-2012-01-23-15 | Grant County - December 1969

    Relationships of soils in association 4 (Soil Survey of Grant County, Kansas; 1969).

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

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

  16. 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).

  17. 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).

  18. KS-2012-01-23-22 | Greeley County - December 1961

    Typical section of the Richfield-Ulysses soil association (Soil Survey of Greeley County, Kansas; 1961).

  19. KS-2012-01-23-23 | Greeley County - December 1961

    Approximate geologic cross section (north and south) through central Greeley County (Soil Survey of Greeley County, Kansas; 1961).

  20. KS-2012-01-23-24 | Greeley County - December 1961

    Cross section of the valley of White Woman Creek in Greeley County (Soil Survey of Greeley County, Kansas; 1961).

  21. KS-2012-01-23-25 | Hamilton County - November 1961

    Geologic profile extending in a north-south direction through the central part of Hamilton County (Soil Survey of Hamilton County, Kansas; 1961).

  22. KS-2012-01-23-30 | Haskell County - October 1968

    Typical topographic relation of three soil associations in Haskell County. Tivoli-Vona association, the farthest north, blocks drainageways flowing from the Satanta-Manter and the Richfield-Ulysses associations to the south (Soil Survey of Haskell County, Kansas; 1968).

  23. 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).

  24. KS-2012-01-23-32 | Haskell County - October 1968

    Landscape showing soils of the Richfield-Spearville-Ulysses association in the southeastern part of the county (Soil Survey of Haskell County, Kansas; 1968).

  25. KS-2012-01-23-43 | Kearny County - November 1963

    Cross section of the county showing the relationship of some of the soils of the uplands to the parent material and topography (Soil Survey of Kearny County, Kansas; 1963).

  26. KS-2012-01-23-44 | Kearny County - November 1963

    An approximate geologic profile of Kearny County, extending in a north-south direction across the county near Hartland (Soil Survey of Kearny County, Kansas; 1963).

  27. KS-2012-01-23-51 | Lane County - November 1972

    Pattern of soils in association 1 (Soil Survey of Lane County, Kansas; 1972).

  28. KS-2012-01-23-52 | Lane County - November 1972

    Pattern of soils in association 2 (Soil Survey of Lane County, Kansas; 1972).

  29. KS-2012-01-24-20 | Morton County - December 1963

    Geologic cross section of the western part of the county. (Based on plate 6 of "Geology and Ground-Water Resources of Morton Co., Kans." (6).) (Soil Survey of Morton County, Kansas; 1963.)

  30. KS-2012-01-25-32 | Scott County - December 1965

    Typical cross section of the major soils of the Richfield-Ulysses association (Soil Survey of Scott County, Kansas; 1965).

  31. KS-2012-01-25-33 | Scott County - December 1965

    Typical cross section of part of the valley of Ladder (Beaver) Creek (Soil Survey of Scott County, Kansas; 1965).

  32. 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).

  33. KS-2012-01-25-35 | Scott County - December 1965

    Cross section of the Scott-Finney depression and part of sandy area to the east near the Scott-Finney county line (Soil Survey of Scott County, Kansas; 1965).

  34. KS-2012-01-26-02 | Sheridan County - March 1984

    Typical pattern of soils in the Ulysses-Colby-Keith association (Soil Survey of Sheridan County, Kansas; 1984).

  35. KS-2012-01-26-03 | Sheridan County - March 1984

    Typical pattern of soils in the Ulysses-Pendend-Colby association (Soil Survey of Sheridan County, Kansas; 1984).

  36. KS-2012-01-26-05 | Sherman County - March 1973

    Typical pattern of major soils in soil association 1 (Soil Survey of Sherman County, Kansas; 1973).

  37. KS-2012-01-26-06 | Sherman County - March 1973

    Typical pattern of major soils in soil association 2 (Soil Survey of Sherman County, Kansas; 1973).

  38. KS-2012-01-26-07 | Sherman County - March 1973

    Typical pattern of major soils in soil association 3 (Soil Survey of Sherman County, Kansas; 1973).

  39. KS-2012-01-26-08 | Sherman County - March 1973

    Major range sites in Sherman County (Soil Survey of Sherman County, Kansas; 1973).

  40. KS-2012-01-26-09 | Sherman County - March 1973

    A cross section of Sherman County soils extending through the center of the county (Soil Survey of Sherman County, Kansas; 1973).

  41. KS-2012-01-26-10 | Stanton County - December 1961

    Diagram of the Richfield-Ulysses soil association on the High Plains (Soil Survey of Stanton County, Kansas; 1961).

  42. KS-2012-01-26-11 | Stanton County - December 1961

    Diagram of the Manter-Dalhart-Ulysses soil association in the valley of Bear Creek (Soil Survey of Stanton County, Kansas; 1961).

  43. KS-2012-01-26-12 | Stanton County - December 1961

    Pattern of soils of the upland in northeastern Stanton County and cross section of part of the valley of Bear Creek (Soil Survey of Stanton County, Kansas; 1961).

  44. KS-2012-01-26-13 | Stanton County - December 1961

    Diagram of the Ulysses-Manter-Richfield soil association in the northwestern part of Stanton County (Soil Survey of Stanton County, Kansas; 1961).

  45. KS-2012-01-26-14 | Stevens County - October 1961

    Geological cross section through the central part of Stevens County (Soil Survey of Stevens County, Kansas; 1961).

  46. KS-2012-01-26-24 | Wallace County - March 1986

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

  47. 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).

  48. KS-2012-01-26-30 | Wichita County - November 1965

    Cross section of association 2 along White Woman Creek (Soil Survey of Wichita County, Kansas; 1965).

  49. KS-2012-01-26-31 | Wichita County - November 1965

    Relationship of soils to the landscape and to the common parent materials of Wichita County (Soil Survey of Wichita County, Kansas; 1965).

  50. NE-2010-09-28-02 | Dundy County -

    Typical pattern of soil and underlying material in the Blackwood-Ulysses association (Soil Survey of Dundy County, Nebraska).

  51. NE-2010-09-28-05 | Dundy County -

    Typical pattern of soil and underlying material in the Sully association (Soil Survey of Dundy County, Nebraska).

  52. NE-2012-02-10-08 | Chase County - November 1982

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

  53. 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).

  54. NE-2012-02-10-25 | Dundy County - February 1963

    Typical area in the Anselmo-Keith soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  55. NE-2012-02-10-26 | Dundy County - February 1963

    Typical area in the Colby soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  56. NE-2012-02-10-27 | Dundy County - February 1963

    Colby soil association merging with the Bridgeport-Havre soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  57. NE-2012-02-10-28 | Dundy County - February 1963

    Typical area in the Keith soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  58. 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).

  59. NE-2012-02-13-24 | Hayes County - August 1982

    The relationship of soils to topography and parent material in the Colby-Ulysses association (Soil Survey of Hayes County, Nebraska; August 1982).

  60. NE-2012-02-13-74 | Red Willow County - April 1967

    Typical pattern of soils in the Holdrege-Keith association (Soil Survey of Red Willow County, Nebraska; April 1967).

  61. NE-2012-02-13-75 | Red Willow County - April 1967

    Typical pattern of soils in the Hord, terrace-McCook-Bridgeport association (Soil Survey of Red Willow County, Nebraska; April 1967).

  62. 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).

  63. OK-2012-02-17-52 | Texas County - July 1961

    Typical pattern of the soils in association 1, Texas County, Okla (Soil Survey of Texas County, Oklahoma; July 1961).

  64. OK-2012-02-17-53 | Texas County - July 1961

    Typical pattern of the soils in association 3, Texas County, Okla (Soil Survey of Texas County, Oklahoma; July 1961).

  65. SD-2012-03-15-91 | Shannon County - April 1971

    Representative pattern of soils in association 1 (Soil Survey of Shannon County, SD; 1971).

  66. TX-2012-03-20-10 | Carson County - July 1962

    General relationship of the soils in Carson County (Soil Survey of Carson County, TX; 1962).

  67. TX-2012-03-20-11 | Carson County - July 1962

    A representative pattern of soils in one of the playas of the Pullman-Randall soil association (Soil Survey of Carson County, TX; 1962).

  68. TX-2012-03-20-14 | Carson County - July 1962

    Soil toposequence of playas (Soil Survey of Carson County, TX; 1962).

  69. TX-2012-03-20-15 | Carson County - July 1962

    Soil toposequence of the escarpment separating the High Plains from the Rolling Plains (Soil Survey of Carson County, TX; 1962).

Map Units

Map units containing ULYSSES 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
Ulysses and norka silt loams, 0 to 1 percent slopesUnA18881942173518co00919661:20000
Ulysses and norka silt loams, 1 to 3 percent slopesUnB10853942183519co00919661:20000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded19672230692052wz9wco00919661:20000
Keith-Ulysses silt loams, 1 to 4 percent slopes2092999943082tv5wco01719851:24000
Ulysses silt loam, 1 to 3 percent slopes8472826686372qv84co06319961:24000
Norka-Ulysses loams, 1 to 3 percent slopes75135349456035dbco07519741:24000
Ulysses silt loam, 0 to 3 percent slopesUsB233399490535rgco09919631:15840
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967629227680852wz9wco09919631:15840
Ulysses sandy loam, 0 to 3 percent slopesUnB523627680862r9l4co09919631:15840
Colby-Ulysses silt loams, 3 to 5 percent slopesCuC10329493135s9co11519691:15840
Colby-Ulysses silt loams, 5 to 9 percent slopesCuD2389493235sbco11519691:15840
Ulysses silt loam, 1 to 3 percent slopes18577328626686382qv84ks02319871:24000
Ulysses silt loam, 0 to 1 percent slopes1856764826688282r9kpks02319871:24000
Ulysses loam, 1 to 3 percent slopes1854210627333832r9kwks02319871:24000
Ulysses silt loam, 3 to 6 percent slopes1859367211505902wz88ks03919851:24000
Ulysses silt loam, 0 to 1 percent slopes18564593026688292r9kpks05519621:24000
Ulysses silt loam, 1 to 3 percent slopes18574284626686392qv84ks05519621:24000
Otero-Ulysses complex, 0 to 5 percent slopes17131692827680742r9kzks05519621:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967982426688922wz9wks05519621:24000
Richfield and Ulysses complexes, bench leveled1754883627680752sbwcks05519621:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded1968810627333862wz8jks05519621:24000
Ulysses loam, 1 to 3 percent slopes1854499427333852r9kvks05519621:24000
Beeler and Ulysses silt loams, 1 to 3 percent slopes1377264725091732pfb8ks05519621:24000
Ulysses and Richfield soils, silted, 0 to 1 percent slopes1847238514537762v9fxks05519621:24000
Ulysses loam, saline, 0 to 1 percent slopes185574425091742pfbyks05519621:24000
Ulysses silt loam, 1 to 3 percent slopes185714330426686402qv84ks06319741:24000
Ulysses silt loam, 3 to 6 percent slopes18593440426687382wz88ks06319741:24000
Buffalo Park-Ulysses silt loams, 6 to 15 percent slopes19612977626688472wz8gks06319741:24000
Ulysses silt loam, 0 to 1 percent slopes18561690126688302r9kpks06319741:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded1968950126058052wz8jks06319741:24000
Penden-Ulysses complex, 7 to 15 percent slopes2768324011506952twd8ks06319741:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded196714226688932wz9wks06319741:24000
Ulysses silt loam, 3 to 6 percent slopes185934026687172wz88ks06519851:24000
Ulysses silt loam, 0 to 1 percent slopes18569256226688312r9kpks06719651:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded19671740826688942wz9wks06719651:24000
Ulysses silt loam, 1 to 3 percent slopes18571121226686412qv84ks06719651:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded1968610127680772wz8jks06719651:24000
Ulysses loam, 1 to 3 percent slopes1854286827333872r9kvks06719651:24000
Manter-Ulysses complex, 1 to 6 percent slopes1674826213805821hblxks06919651:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded1968327333882wz8jks06919651:24000
Ulysses silt loam, 1 to 3 percent slopes18579831526686422qv84ks07119591:24000
Ulysses silt loam, 0 to 1 percent slopes18561850826688322r9kpks07119591:24000
Ulysses loam, 1 to 3 percent slopes1854916127333892r9kvks07119591:24000
Ulysses loam and silt loam, 3 to 5 percent slopes18501572115183817nl2ks07119591:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded196714326688952wz9wks07119591:24000
Ulysses silt loam, 0 to 1 percent slopes18563880326688332r9kpks07519591:24000
Ulysses loam, 1 to 3 percent slopes18541818027333902r9kvks07519591:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded19671384326688962wz9wks07519591:24000
Ulysses silt loam, 1 to 3 percent slopes18571360226686432qv84ks07519591:24000
Ulysses loam, 0 to 1 percent slopes18532967115223817nzzks07519591:24000
Ulysses silt loam, 0 to 1 percent slopes18564335926688342r9kpks08119651:24000
Richfield and Ulysses complexes, bench leveled17541464127680792sbwcks08119651:24000
Ulysses silt loam, 1 to 3 percent slopes18571380426686442qv84ks08119651:24000
Otero-Ulysses complex, 0 to 5 percent slopes1713399127680782r9kzks08119651:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967142226688972wz9wks08119651:24000
Ulysses loam, 1 to 3 percent slopes1854119027333912r9kvks08119651:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded196874327333922wz8jks08119651:24000
Ulysses silt loam, 0 to 1 percent slopes18568472926688352r9kpks09319611:24000
Ulysses silt loam, 1 to 3 percent slopes18573484326686452qv84ks09319611:24000
Ulysses and Richfield soils, silted, 0 to 1 percent slopes18471065411522862v9fxks09319611:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967412726688992wz9wks09319611:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded1968106027333932wz8jks09319611:24000
Richfield-Ulysses silt loams, 1 to 3 percent slopes17703170527334152sbw9ks10119661:24000
Buffalo Park-Ulysses silt loams, 6 to 15 percent slopes19611461926688482wz8gks10119661:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded19681202327333942wz8jks10119661:24000
Ulysses silt loam, 1 to 3 percent slopes18571044426686462qv84ks10119661:24000
Ulysses silt loam, 3 to 6 percent slopes18591026326687452wz88ks10119661:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967565126689002wz9wks10119661:24000
Richfield-Ulysses silt loams, 3 to 6 percent slopes1771214327682192sbwgks10119661:24000
Ulysses silt loam, 0 to 1 percent slopes1856159626688362r9kpks10119661:24000
Ulysses silt loam, 1 to 3 percent slopes185714903426686472qv84ks10919621:24000
Ulysses silt loam, 0 to 1 percent slopes18569125926688372r9kpks10919621:24000
Ulysses silt loam, 3 to 6 percent slopes18592995426687462wz88ks10919621:24000
Buffalo Park-Ulysses silt loams, 6 to 15 percent slopes19612070226688492wz8gks10919621:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded1968936311505532wz8jks10919621:24000
Ulysses silty clay loam, 1 to 3 slopes18631411115055217m7lks10919621:24000
Ulysses silt loam, 0 to 1 percent slopes18563227626688382r9kpks12919951:24000
Ulysses silt loam, 3 to 6 percent slopes185947426687622wz88ks13519711:24000
Richfield-Ulysses silt loams, 1 to 3 percent slopes1770827334162sbw9ks13519711:24000
Ulysses silt loam, 3 to 6 percent slopes18596507826687472wz88ks15319791:24000
Ulysses silt loam, 0 to 1 percent slopes18566439426688392r9kpks17119631:24000
Ulysses silt loam, 1 to 3 percent slopes18574015726686482qv84ks17119631:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded19671265826689042wz9wks17119631:24000
Ulysses silt loam, 3 to 6 percent slopes1859693726687482wz88ks17119631:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded1968164927333962wz8jks17119631:24000
Ulysses silt loam, 0 to 1 percent slopes1856862426688402r9kpks17519631:24000
Richfield and Ulysses complexes, bench leveled1754551527680822sbwcks17519631:24000
Ulysses silt loam, 1 to 3 percent slopes1857348626686492qv84ks17519631:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded196778126689052wz9wks17519631:24000
Ulysses silt loam, 3 to 6 percent slopes18599676926687492wz88ks17919821:24000
Penden-Ulysses complex, 7 to 15 percent slopes27685876611500072twd8ks17919821:24000
Ulysses silt loam, 1 to 3 percent slopes185723926686502qv84ks17919821:24000
Ulysses silt loam, 1 to 3 percent slopes185712807626686512qv84ks18119671:24000
Keith-Ulysses silt loams, 0 to 1 percent slopes16216843126689062sbw7ks18119671:24000
Buffalo Park-Ulysses silt loams, 6 to 15 percent slopes19613154126688502wz8gks18119671:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded19681114727680832wz8jks18119671:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967137926689072wz9wks18119671:24000
Ulysses silt loam, 0 to 1 percent slopes185664826688412r9kpks18119671:24000
Ulysses silt loam, 0 to 1 percent slopes18568872226688422r9kpks18719591:24000
Ulysses silt loam, 1 to 3 percent slopes18574938526686522qv84ks18719591:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967291526689082wz9wks18719591:24000
Ulysses silt loam, 0 to 1 percent slopes1856243026688432r9kpks18920051:24000
Ulysses silt loam, 1 to 3 percent slopes18576476326686532qv84ks19319781:24000
Ulysses silt loam, 1 to 3 percent slopes, eroded18581662327680842r9l2ks19319781:24000
Ulysses silt loam, 0 to 1 percent slopes1856679726688442r9kpks19319781:24000
Ulysses silt loam, 3 to 6 percent slopes1859338526687282wz88ks19319781:24000
Ulysses silt loam, 1 to 3 percent slopes1857352326686542qv84ks19519861:24000
Ulysses silt loam, 3 to 6 percent slopes18597026687532wz88ks19519861:24000
Ulysses silt loam, 1 to 3 percent slopes185717195426686552qv84ks19919841:24000
Ulysses silt loam, 0 to 1 percent slopes18565289826688452r9kpks19919841:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967508826689092wz9wks19919841:24000
Buffalo Park-Ulysses silt loams, 6 to 15 percent slopes196157026688512wz8gks19919841:24000
Ulysses silt loam, 0 to 1 percent slopes18567215526688462r9kpks20319631:24000
Ulysses silt loam, 1 to 3 percent slopes18574794526686562qv84ks20319631:24000
Buffalo Park-Ulysses silt loams, 1 to 3 percent slopes, eroded1967573426689112wz9wks20319631:24000
Buffalo Park-Ulysses silt loams, 3 to 6 percent slopes, eroded196867127333982wz8jks20319631:24000
Ulysses silt loam, 3 to 6 percent slopes18591326687552wz88ks20319631:24000
Sulco-Ulysses silt loams, 9 to 30 percent slopes, eroded1833245622195292wz8mne02919801:20000
Ulysses silt loam, 6 to 9 percent slopes, eroded1861145427682212sbwbne02919801:20000
Ulysses loam, 1 to 3 percent slopes185416227334002r9kwne02919801:20000
Ulysses-Sulco silt loams, 6 to 9 percent slopes, eroded186910726688912r9ktne02919801:20000
Ulysses loam, 3 to 6 percent slopes18556827682202sbwdne02919801:20000
Ulysses loam, 1 to 3 percent slopes1854142927334012r9kwne03319891:20000
Ulysses loam, 3 to 6 percent slopes185567327682222sbwdne03319891:20000
Keith-Ulysses silt loams, 3 to 9 percent slopes1616155923581182tvtbne04519731:20000
Ulysses silt loam, 9 to 20 percent slopes18627909358173d0pzne04519731:20000
Ulysses loam, 3 to 6 percent slopes1855754427682232sbwdne05719951:24000
Ulysses loam, 1 to 3 percent slopes1854711127334032r9kwne05719951:24000
Ulysses silt loam, 3 to 6 percent slopes18595029958822wz88ne05719951:24000
Sulco-Ulysses silt loams, 9 to 30 percent slopes, eroded18331085922193482wz8mne06319731:20000
Sulco-Ulysses silt loams, 9 to 30 percent slopes, eroded18337977616992392wz8mne08519811:20000
Ulysses silt loam, 3 to 6 percent slopes185991816992652wz88ne08519811:20000
Ulysses silt loam, 6 to 9 percent slopes, eroded186181127682242sbwbne08519811:20000
Ulysses-Sulco silt loams, 6 to 9 percent slopes, eroded18691396126688982r9ktne08719651:20000
Sulco-Ulysses silt loams, 9 to 30 percent slopes, eroded18331044022288502wz8mne08719651:20000
Ulysses silt loam, 6 to 9 percent slopes, eroded1861218027682262sbwbne08719651:20000
Ulysses silt loam, 3 to 6 percent slopes185929129958862wz88ne08719651:20000
Ulysses loam, 1 to 3 percent slopes18544827334072r9kwne08719651:20000
Ulysses loam, 3 to 6 percent slopes18553927682252sbwdne08719651:20000
Sulco-Ulysses silt loams, 9 to 30 percent slopes, eroded1833156922197592wz8mne11119711:24000
Ulysses-Sulco silt loams, 6 to 9 percent slopes, eroded186939426689012r9ktne11119711:24000
Ulysses silt loam, 6 to 9 percent slopes, eroded186110927682272sbwbne11119711:24000
Ulysses silt loam, 3 to 6 percent slopes18591422197602wz88ne11119711:24000
Ulysses-Sulco silt loams, 6 to 9 percent slopes, eroded18691040726689022r9ktne13519871:20000
Ulysses-Sulco silt loams, 3 to 6 percent slopes, eroded1868766927682282r9l6ne13519871:20000
Sulco-Ulysses silt loams, 9 to 30 percent slopes, eroded1833637116989602wz8mne13519871:20000
Sulco-Ulysses silt loams, 9 to 30 percent slopes, eroded1833537522191212wz8mne14519651:20000
Ulysses silt loam, 6 to 9 percent slopes, eroded186113127682292sbwbne14519651:20000
Ulysses-Sulco silt loams, 6 to 9 percent slopes, eroded18696426689032r9ktne14519651:20000
Ulysses silt loam, 3 to 6 percent slopes18594229958892wz88ne14519651:20000
Ulysses clay loam, 0 to 1 percent slopesUcA118159384925dxjyok13919591:24000
Perico-Ulysses complex, 1 to 3 percent slopesDuB48292384906dxjbok13919591:24000
Ulysses clay loam, 1 to 3 percent slopesUcB34599384926dxjzok13919591:24000
Perico-Ulysses complex, 0 to 1 percent slopesDuA8512384905dxj9ok13919591:24000
Perico-Ulysses complex, 3 to 5 percent slopesDuC7598384907dxjcok13919591:24000
Keith-Ulysses silt loams, 3 to 9 percent slopesKuC21053527502tvtbsd00720041:20000
Keith-Ulysses silt loams, 3 to 9 percent slopesKuC1436729255262tvtbsd61019651:20000
Thirtynine-Ulysses, cool silt loams, 6 to 9 percent slopesU380C10124853502pf6lsd61220111:20000
Keith-Ulysses silt loams, 3 to 9 percent slopesKuC1562425827112tvtbsd61320111:24000
Ulysses-Colby complex, sand substratum, 3 to 9 percent slopesUcC10962582743cv4tsd61320111:24000
Thirtynine-Ulysses, cool silt loams, 6 to 9 percent slopesU380C1425828362pf6lsd61320111:24000
Ulysses loam, 1 to 3 percent slopesUIB494527334112r9kxwy61519651:20000
Ulysses loam, 3 to 6 percent slopesUIC22211047543j05wy61519651:20000
Ulysses loam, 0 to 1 percent slopesUIA15551047523j03wy61519651:20000

Map of Series Extent

Approximate geographic distribution of the ULYSSES 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 .