Official Series Description


Lab Data Summary

Aggregate lab data for the HILAND soil series. This aggregation is based on all pedons with a current taxon name of HILAND, 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 HILAND 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
34A83P063183WY025006Hiland6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1450005,-107.4577789
58B98P041298WY009001HILAND7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8591652,-105.1183319
58B98P041398WY009002HILAND7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7966652,-105.2619476

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HILAND 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 HILAND 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 HILAND 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 HILAND 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 HILAND 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 HILAND 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 HILAND 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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Soil series sharing subgroup-level classification with HILAND, 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. WY-2010-11-08-03 | South Converse County -

    (Soil Survey of South Converse County, Wyoming)

Map Units

Map units containing HILAND 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
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes2532497802622tzbrwy01119781:24000
Hiland-Vonalee fine sandy loams, 6 to 15 percent slopes259101780263v5xswy01119781:24000
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes141154913495962tzbrwy02719931:24000
Hiland-Bowbac fine sandy loams, 0 to 6 percent slopes140142023495942tzbswy02719931:24000
Hiland sandy loam, 0 to 6 percent slopes1391595349592cqs5wy02719931:24000
Selpats-Hiland complex, 0 to 6 percent slopes22398921045773htgwy03119981:24000
Hiland-Cambria sandy loams, 0 to 6 percent slopes16965251045243hrrwy03119981:24000
Hiland fine sandy loam, 0 to 3 percent slopes16839651045233hrqwy03119981:24000
Worfka-Hiland-Mident complex, 1 to 35 percent slopes5C09335668930zsgwy04319761:24000
Hiland-Remmit complex, 0 to 10 percent slopes222933566612wxn0wy04319761:24000
Hiland-Bunkwater-Vonalee complex, 1 to 15 percent slopes220433566602wxmqwy04319761:24000
Hiland-Bowbac complex, 0 to 10 percent slopes498748349453cqmpwy04519841:24000
Hiland-Vonalee association, rolling508175349455cqmrwy04519841:24000
Hiland-Vonalee fine sandy loams, 0 to 6 percent slopes1387153616902yv7lwy04519841:24000
Hiland-Bowbac fine sandy loams, 0 to 6 percent slopes1372663616912tzbswy04519841:24000
Hiland-Bunkwater-Vonalee complex, 1 to 15 percent slopes220431708752wxmqwy6031:24000
Hiland-Bowbac fine sandy loams, 0 to 6 percent slopes157604153498442tzbswy60519951:24000
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes158537103498452tzbrwy60519951:24000
Decolney-Hiland fine sandy loams, 0 to 6 percent slopes129168913498142wlq6wy60519951:24000
Hiland-Vonalee fine sandy loams, 0 to 6 percent slopes159124053498492yv7lwy60519951:24000
Hiland-Vonalee fine sandy loams, 6 to 15 percent slopes1605527349851cr1jwy60519951:24000
Hiland fine sandy loam, 0 to 6 percent slopes1565334349843cr18wy60519951:24000
Decolney-Hiland fine sandy loams, 6 to 15 percent slopes13029233498152wlq7wy60519951:24000
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes1734953016696952tzbrwy60920061:24000
Hiland-Bowbac fine sandy loams, 0 to 6 percent slopes1723731516696962tzbswy60920061:24000
Hiland-Bowbac complex, 6 to 15 percent slopes175363116697932v09fwy60920061:24000
Hiland-Bowbac sandy loams, 0 to 6 percent slopes17173616697942v09gwy60920061:24000
Hiland loamy sand, 2 to 15 percent slopes17071516696972v09qwy60920061:24000
Bowbac-Hiland-Worf complex, 3 to 15 percent slopes11256816698092wxz2wy60920061:24000
Worf-like-Shingle-Hiland complex, 20 to 50 percent slopes552631708682wxmdwy6171:24000
Hiland-Bowbac-like-Lazear complex, 6 to 30 percent slopes5D0833028443013xwy6171:24000
Claprych, stony-Hiland-Ralstonflats complex, 2 to 40 percent slopes2D01330285130144wy6171:24000
Hiland-Remmit complex, 0 to 10 percent slopes222932532882wxn0wy6171:24000
Ulm-Hiland complex, 0 to 3 percent slopes213233028752w7j2wy6171:24000
Hiland sandy clay loam, 0 to 2 percent slopes, rarely flooded1A12335827630zt9wy6171:24000
Hiland clay loam, 1 to 3 percent slopes2B13335826930zt2wy6171:24000
Worfka-Hiland-Mident complex, 1 to 35 percent slopes5C09335825030zsgwy6171:24000
Cushman-Hiland-Wyotite complex, 3 to 60 percent slopes5D12335823130zrtwy6171:24000
Hiland-Amodac-like complex, 3 to 15 percent slopes2C09335835731jy5wy6171:24000
Castledale, occasionally flooded-Hiland complex, 1 to 5 percent slopes1A21335837431jyqwy6171:24000
Eaglenest-Hiland complex, 4 to 15 percent slopes230933582832wxlnwy6171:24000
Hiland sandy clay loam, 2 to 10 percent slopes120931708392w7knwy6171:24000
Hiland-Bunkwater-Vonalee complex, 1 to 15 percent slopes220431970452wxmqwy6171:24000
Hiland-Ulm complex, 6 to 20 percent slopes230431768892w7ktwy6171:24000
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes1582858172422tzbrwy61919711:24000
Hiland-Bowbac complex, 6 to 15 percent slopes102658165602v09fwy61919711:24000
Hiland-Vonalee fine sandy loams, 6 to 15 percent slopes16029817243wfdpwy61919711:24000
Hiland-Bowbac sandy loams, 0 to 6 percent slopes12118168582v09gwy61919711:24000
Hiland sandy loam, 0 to 6 percent slopes2011102595022912tzbtwy62519851:24000
Vonalee-Hiland complex, 3 to 15 percent slopes301692775024392v09dwy62519851:24000
Bowbac-Hiland fine sandy loams, 3 to 10 percent slopes132673035022102tzc7wy62519851:24000
Hiland loamy sand, 2 to 15 percent slopes199366175022872v09qwy62519851:24000
Bowbac-Hiland-Worf complex, 3 to 15 percent slopes133166865022112wxz2wy62519851:24000
Hiland loamy sand, gravelly substratum, 1 to 6 percent slopes200134585022892yb7vwy62519851:24000
Keyner-Hiland sandy loams, 0 to 6 percent slopes210120765023092ztzbwy62519851:24000
Bosler-Hiland association, rolling1314372502209jvl9wy62519851:24000
Hiland-Bowbac complex, 6 to 15 percent slopes32866914260862v09fwy62519851:24000
Eaglenest-Hiland complex, 4 to 15 percent slopes230929690672wxlnwy6291:24000
Hiland-Unnamed 2, frequently flooded complex, 5 to 15 percent slopes60115261753t4wy6291:24000
Oregon Basin-Vonalee-Hiland complex, 1 to 8 percent slopes111129690352wxk2wy6291:24000
Hiland sandy clay loam, 2 to 10 percent slopes120929119452w7knwy6291:24000
Eaglenest-Hiland complex, 1 to 3 percent slopes210131332512ynmbwy6291:24000
Bunkwater-Hiland-Winnett complex, 1 to 6 percent slopes212529119592y4yfwy6291:24000
Ulm-Hiland complex, 0 to 3 percent slopes213229118942w7j2wy6291:24000
Romound-like-Hiland complex, 1 to 3 percent slopes215032066592zc5kwy6291:24000
Hiland-Selpats complex, 1 to 3 percent slopes215532504982zv7lwy6291:24000
Hiland-Bunkwater-Vonalee complex, 1 to 15 percent slopes220429690972wxmqwy6291:24000
Hiland-Remmit complex, 0 to 10 percent slopes222929691062wxn0wy6291:24000
Hiland-Maysdorf-Bunkwater complex, 1 to 6 percent slopes223531332312ynlpwy6291:24000
Hiland gravelly sandy clay loam, 3 to 6 percent slopes224231328362yn96wy6291:24000
Bunkwater-like-Hiland-Eaglenest complex, 1 to 4 percent slopes225732066622zc5nwy6291:24000
Clapper, stony-Hiland-Cambria complex, 2 to 12 percent slopes225932066782zc64wy6291:24000
Hiland-Ulm complex, 6 to 20 percent slopes230429119502w7ktwy6291:24000
Hiland-Jimmerfield-Maysdorf complex, 6 to 12 percent slopes231531332552ynmgwy6291:24000
Hiland fine sandy loam, 4 to 8 percent slopes232631709402z1z6wy6291:24000
Hiland-Calicott-like complex, 4 to 12 percent slopes232731709412z1z7wy6291:24000
Hiland-Romberg-like-Bunkwater complex, 4 to 15 percent slopes233332066672zc5swy6291:24000
Claprych-Hiland complex, 4 to 25 percent slopes235432504882zv7bwy6291:24000
Hiland-Claprych-Remmit complex, 1 to 20 percent slopes242131709522z1zgwy6291:24000
Renohill-Threetop-Hiland complex, 1 to 4 percent slopes510632532562zyb9wy6291:24000
Hiland-Terry-Rimrock Basin complex, 2 to 10 percent slopes520329690302wxjwwy6291:24000
Shingle-like-Hiland-Rock outcrop complex, 4 to 35 percent slopes532129691122y62swy6291:24000
Hiland-Pultney-Zigweid-like complex, 3 to 10 percent slopes532431368572ypntwy6291:24000
Bunkwater-like-Hiland-Bowbac complex, 6 to 20 percent slopes536431709812z20dwy6291:24000
Romberg-like-Shingle-Hiland complex, 6 to 20 percent slopes536732030602zbrqwy6291:24000
Shingle-Bullpen-Hiland complex, 15 to 40 percent slopes546331368642ypp1wy6291:24000
Badland-Gypimack-like-Hiland complex, 4 to 15 percent slopes548532066432zc4vwy6291:24000
Worf-like-Shingle-Hiland complex, 20 to 50 percent slopes552629690872wxmdwy6291:24000
Ulm-Hiland-Bowbac-like complex, 10 to 30 percent slopes580631709852z20jwy6291:24000
Hiland-Decolney complex, 3 to 15 percent slopes1664853361153d3t3wy63319871:24000
Hiland-Bowbac complex, 3 to 15 percent slopes1642954361155d3t5wy63319871:24000
Hiland-Vonalee complex, moist, 3 to 10 percent slopes1671352361152d3t2wy63319871:24000
Hiland-Bowbac association, moist, 3 to 15 percent slopes1651259361154d3t4wy63319871:24000
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes6562723899742tzbrwy63319871:24000
Hiland-Vonalee fine sandy loams, 6 to 15 percent slopes659142389972w9zcwy63319871:24000
Hiland gravelly sandy clay loam, 3 to 6 percent slopes224232505412yn96wy65620081:24000
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes28913088175422tzbrwy70520031:24000
Decolney-Hiland fine sandy loams, 0 to 6 percent slopes26811058175442wlq6wy70520031:24000
Hiland-Bowbac fine sandy loams, 0 to 6 percent slopes2888948175412tzbswy70520031:24000
Decolney-Hiland fine sandy loams, 6 to 15 percent slopes2692448175432wlq7wy70520031:24000
Hiland-Decolney complex, 3 to 15 percent slopes290161817539wfq7wy70520031:24000
Hiland-Bowbac complex, 3 to 15 percent slopes287118817538wfq6wy70520031:24000
Hiland-Bowbac complex, 6 to 15 percent slopes1221846643515002v09fwy70919831:24000
Hiland-Bowbac sandy loams, 0 to 6 percent slopes121889903514992v09gwy70919831:24000
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes23617403612752tzbrwy70919831:24000
Hiland-Bowbac fine sandy loams, 0 to 6 percent slopes237162714278942tzbswy70919831:24000
Hiland-Bowbac complex, 0 to 10 percent slopes238514278951jxv4wy70919831:24000
Vonalee-Hiland complex, undulating22036901503099jwj0wy71319861:24000
Bowbac-Hiland complex, rolling12227879502987jwddwy71319861:24000
Hiland sandy loam, 1 to 15 percent slopes16119905503026jwfnwy71319861:24000
Hiland-Bowbac fine sandy loams, 6 to 15 percent slopes656463313991402tzbrwy71920131:24000
Hiland-Bowbac fine sandy loams, 0 to 6 percent slopes65522488139322tzbswy71920131:24000
Hiland-Vonalee fine sandy loams, 6 to 15 percent slopes6592185813947w9zcwy71920131:24000
Hiland fine sandy loam, 0 to 6 percent slopes6521807813984wb0kwy71920131:24000
Hiland fine sandy loam, 0 to 3 percent slopes645128913846261hgtcwy71920131:24000
Hiland-Bowbac complex, 3 to 15 percent slopes6541254813981wb0gwy71920131:24000
Hiland fine sandy loam, 3 to 6 percent slopes653110113846271hgtdwy71920131:24000

Map of Series Extent

Approximate geographic distribution of the HILAND 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 .