Official Series Description


Lab Data Summary

Aggregate lab data for the HIKO PEAK soil series. This aggregation is based on all pedons with a current taxon name of HIKO PEAK, 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 HIKO PEAK 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
28A85P095185UT003004Hiko Peak8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8652763,-113.1277771
28A85P093285UT021001Hiko Peak6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7430305,-113.0491257

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HIKO PEAK 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 HIKO PEAK 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 HIKO PEAK 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 HIKO PEAK 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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Competing Series

Soil series competing with HIKO PEAK 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 HIKO PEAK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the HIKO PEAK 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.

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 HIKO PEAK, 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. UT-2010-11-05-03 | Tooele County Area - 2000

    Typical pattern of soils and parent material in the Hiko Peak-Taylorsflat-Medburn general soil map unit (Soil Survey of Tooele County Area, Utah; 2000).

  2. UT-2012-03-22-14 | Tooele Area - 2000

    Typical pattern of soils and parent material in the Hiko Peak-Taylorsflat-Medburn general soil map unit (Soil Survey of Tooele Area, Utah; Tooele County and Parts of Box Elder, Davis, and Juab Counties, Utah, and Parts of White Pine and Elko Counties, Nevada; 2000).

Map Units

Map units containing HIKO PEAK 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
Armespan-Hiko Peak association13521651479972j3fznv77920041:24000
Stucky-Hiko Peak association, 8 to 25 percent slopes8615327481299j4tsut60119851:24000
Hiko Peak-Taylorsflat-Skumpah association, 1 to 12 percent slopes3914740481247j4s3ut60119851:24000
Hiko Peak-Taylorsflat complex, 1 to 12 percent slopes3813725481246j4s2ut60119851:24000
Cliffdown-Hiko Peak-Okrist, thick surface association, 3 to 12 percent slopes1712821481223j4rbut60119851:24000
Hiko Peak gravelly loam, 3 to 12 percent slopes3510164481243j4rzut60119851:24000
Plegomir-Hiko Peak-Bullump association, 3 to 25 percent slopes623584481273j4syut60119851:24000
Hiko Peak-Sheeprock-Rock outcrop association, 3 to 25 percent slopes372964481245j4s1ut60119851:24000
Hiko Peak-Kunzler association, 3 to 12 percent slopes362937481244j4s0ut60119851:24000
Hiko Peak stony sandy loam, 4 to 8 percent slopesHdC27401482520j635ut60819811:24000
Hiko Peak stony sandy loam, 8 to 15 percent slopesHdD4191482521j636ut60819811:24000
Hiko Peak stony sandy loam, 15 to 25 percent slopesHdE3712482522j637ut60819811:24000
Donnardo-Hiko Peak complex, 25 to 40 percent slopesDeF2832482487j623ut60819811:24000
Hiko Peak gravelly loam, 2 to 15 percent slopes21110826482125j5pfut61119921:24000
Hiko Peak-Taylorsflat complex, 1 to 15 percent slopes2451362482128j5pjut61119921:24000
Berent-Hiko Peak complex, 2 to 15 percent slopes539229482157j5qgut61119921:24000
Hiko Peak very stony loam, 2 to 8 percent slopes2228365482126j5pgut61119921:24000
Hiko Peak-Checkett complex, 2 to 40 percent slopes237170482127j5phut61119921:24000
Hiko Peak families complex, 2 to10 percent slopes323864831838562whrvut6171:24000
Kessler-Hiko Peak-Heist families association, 1 to 10 percent slopes381704731838622whs1ut6171:24000
Checkett-Hiko Peak families complex, 2 to 50 percent slopes81539731839082x4h6ut6171:24000
Hiko Peak-Checkett families association, 2 to 50 percent slopes33704631838572whrwut6171:24000
Hiko Peak-Heist families association, 2 to 10 percent slopes34411031838582whrxut6171:24000
Hiko Peak-Heist association, 2 to 15 percent slopes627210481857j5dsut61819951:24000
Hiko Peak fine sandy loam, 2 to 8 percent slopes577067481851j5dlut61819951:24000
Hiko Peak-Heist complex, 2 to 8 percent slopes644628481859j5dvut61819951:24000
Hiko Peak stony fine sandy loam, 5 to 15 percent slopes602690481855j5dqut61819951:24000
Hiko Peak-Pibler complex, 2 t0 15 percent slopes652328481860j5dwut61819951:24000
Hiko Peak gravelly loam, 2 to 15 percent slopes581717481852j5dmut61819951:24000
Hiko Peak-Amtoft complex, 8 to 35 percent slopes611652481856j5drut61819951:24000
Hiko Peak gravelly loam, 20 to 50 percent slopes591423481853j5dnut61819951:24000
Hiko Peak extremely stony loam, 4 to 15 percent slopes561260481850j5dkut61819951:24000
Hiko Peak-Heist complex, 0 to 2 percent slopes631170481858j5dtut61819951:24000
Firmage-Hiko Peak complex, 2 to 15 percent slopes461064481839j5d6ut61819951:24000
Hiko Peak-Crestline complex, 3 to 8 percent slopes1163523922204392djk2ut6261:24000
Hiko Peak, dry-Lynndyl association1751784322204972djlyut6261:24000
Hiko Peak-Dixie complex, 3 to 8 percent slopes119991422204422djk5ut6261:24000
Hiko Peak cobbly sandy loam, dry, 3 to 8 percent slopes173792922204952djlwut6261:24000
Hiko Peak cobbly sandy loam, dry, 8 to 15 percent slopes172706622204942djlvut6261:24000
Hiko Peak gravelly loam, cool, 8 to 15 percent slopes121520922204442djk7ut6261:24000
Hiko Peak gravelly loam, 3 to 8 percent slopes114412422204372djk0ut6261:24000
Hiko Peak very cobbly sandy loam, 15 to 30 percent slopes174211522204962djlxut6261:24000
Medburn-Hiko Peak complex, 1 to 5 percent slopes140166622204632djkvut6261:24000
Saxby-Hiko Peak-Rock outcrop complex, 5 to 20 percent slopes133106522204562djkmut6261:24000
Hiko Peak gravelly loam, 0 to 3 percent slopes11352322204362djjzut6261:24000
Hiko Peak, steep-Saxby-Rock outcrop association, 30 to 70 percent slopes14413069483508j741ut6281:24000
Red Butte-Hiko Peak, steep association, 15 to 70 percent slopes1897169483505j73yut6281:24000
Torriorthents, dry-Hiko Peak, dry association, 10 to 40 percent slopes2196641483455j72but6281:24000
Hiko Peak, dry-Tarnach-Rock outcrop association, 4 to 45 percent slopes145495924226892mb08ut6281:24000
Hiko Peak, south-Annabella complex, 5 to 30 percent slopes1414478483497j73put6281:24000
Hoye-Hiko Peak, south-Checkett association, 15 to 50 percent slopes152410624255472mdzgut6281:24000
Wala-Hiko Peak, south-Rock outcrop association, 15 to 50 percent slopes2143355483507j740ut6281:24000
Hiko Peak very cobbly sandy loam, 5 to 30 percent slopes, extremely bouldery1403180483502j73vut6281:24000
Hiko Peak-Pibler-Sanpete association, 2 to 30 percent slopes1431410483606j776ut6281:24000
Tosser-Hiko Peak, south-Annabella complex, 8 to 40 percent slopes209119524539452ncjjut6281:24000
Hiko Peak, south-Grifleys family-Annabella, steep complex, 3 to 50 percent slopes14287224539442ncjhut6281:24000
Hiko Peak gravelly loam, 2 to 15 percent slopes1393324540212nclzut6281:24000
Hiko Peak, rubbly-Saxby, rubbly-Rock outcrop association, 30 to 70 percent slopes1441826425045352r815ut6291:24000
Hiko Peak, extremely stony-Annabella complex, 5 to 30 percent slopes1411096825045332r813ut6291:24000
Wala, extremely flaggy-Hiko Peak, extremely stony-Rock outcrop association, 15 to 50 percent slopes214851825045562syg4ut6291:24000
Hiko Peak-Escalante complex, 2 to 5 percent slopesHgC4841504682jy52ut6291:24000
Tosser-Hiko Peak, very stony-Annabella complex, 8 to 40 percent slopes209364125045552syg2ut6291:24000
Hoye-Hiko Peak, extremely stony-Checkett, extremely stony association, 15 to 50 percent slopes.152311725045432r81but6291:24000
Red Butte, extremely stony-Hiko Peak, very stony association, 15 to 60 percent slopes189272825045512r81rut6291:24000
Dixie-Hiko Peak complex, 2 to 8 percent slopesDcC2409504637jy3mut6291:24000
Hiko Peak very cobbly sandy loam, 5 to 30 percent slopes, extremely bouldery140218925045322r812ut6291:24000
Hiko Peak, very stony-Grifleys family, extremely stony-Annabella complex, 3 to 50 percent slopes142162725045342r814ut6291:24000
Hiko Peak, very stony-Tarnach association, 4 to 45 percent slopes14585425045362r816ut6291:24000
Hiko Peak gravelly sandy loam, 2 to 15 percent slopes38937299483917j7k7ut63419971:24000
Hiko Peak gravelly loam, 2 to 25 percent slopes38813890483916j7k6ut63419971:24000
Kessler-Penoyer association, 1 to 20 percent slopesKPE12750484619j88wut64019671:20000
Hiko Peak cobbly loam, 2 to 10 percent slopesHKD10585484606j88gut64019671:20000
Hiko Peak-Decca association, 1 to 15 percent slopesHPE6455484607j88hut64019671:20000
Kessler-Hiko Peak association, 1 to 20 percent slopesKME5150484618j88vut64019671:20000
Decca-Hiko Peak complex, 1 to 30 percent slopesDHF4960484580j87mut64019671:20000
Escalante-Hiko Peak complex, 2 to 10 percent slopes, erodedESD24820484589j87xut64019671:20000
Hiko Peak-Fruitland association, 1 to 15 percent slopesHRE4510484608j88jut64019671:20000
Hiko Peak coarse sandy loam, 3 to 30 percent slopesHIF3790484605j88fut64019671:20000
Penoyer-Hiko Peak association, 1 to 10 percent slopesPHD710484655j8b1ut64019671:20000
Hiko Peak family, 5 to 30 percent slopes167625220nzldut6491:24000
Abela, stony-Hiko Peak families, association, 5 to 30 percent slopes101580984mhkfut6491:24000
Hiko Peak-Heist families, complex, 2 to 15 percent slopes169625218nzlbut6491:24000
Hiko Peak, very bouldery-Duco, stony-Mountainville, very stony families, association, 3 to 65 percent slopes168625219nzlcut6491:24000

Map of Series Extent

Approximate geographic distribution of the HIKO PEAK 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 .