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Utah Dept of Highways # 14128

Past Producer in Beaver county in Utah, United States with commodity Sand and Gravel, Construction
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Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Public Land Survey System information
  6. Commodities
  7. Host and associated rocks
  8. Nearby scientific data
  9. Geologic structures
  10. Ore body information
  11. Controls for ore emplacement
  12. Economic information about the deposit and operations
  13. Mining district
  14. Land status
  15. Ownership information
  16. Workings at the site
  17. Links to other databases
  18. Bibliographic references
  19. General comments
  20. Reporter information

Geologic information

Identification information

Deposit ID 10101518
MRDS ID D004421
Record type Site
Current site name Utah Dept of Highways # 14128

Geographic coordinates

Geographic coordinates: -113.77999, 38.56968 (WGS84)
Elevation 1661
Relative position 1 1/2 MILES SE OF WARM POINT ON STATE HIGHWAY 21

Site location context

Political divisions (FIPS codes)

Beaver(county)

Utah(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Halfway Summit(quadrangle 1:24,000 scale)

Wah Wah Mountains North(quadrangle 1:100,000 scale)

Richfield(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Pine Valley(hydrologic unit)

Great Salt Lake(hydrologic accounting unit)

Great Salt Lake(hydrologic subregion)

Great Basin(hydrologic region)

Federal lands

Bureau of Land Management(Bureau of Land Management UT)

Bureau of Land Management UT BLM(Type of land area)

BLM(Federal land areas administered by BLM)

Geographic areas

Country State County
United States Utah Beaver

Public Land Survey System information

Meridian Township Range Section Fraction State
Salt Lake 026S 017W 05 Utah

Comments on the location information

  • SE 1/4, SE 1/4, SW 1/4, SEC 5

Commodities

Commodity Importance
Sand and Gravel, Construction Secondary

Comments on the commodity information

  • PRIMARILY VOLCANIC WITH SOME CARBONATE AND MINOR QUARTZITE PEBBLES AND COBBLES.

Analytical data

Result SEIVE ANALYSIS: GREATER 3"= 0%, GREATER 1"= 11.9%, 1"= 100%, #4= 60.9%, #10=50, #40=23.1, #200=4.9, LL= 17.2, N.P., A-1-9

Host and associated rocks

  • Host or associated Host
    Rock type Unconsolidated Deposit > Gravel
    Rock unit name Gravels
    Rock description Gravels
    Stratigraphic age (youngest) Holocene
    Stratigraphic age (youngest) Holocene

Nearby scientific data

(1) -113.77999, 38.56968
ListMap

Economic information

Geologic structures

Type of structure Regional
Structure description Basin & Range

Ore body information

  • General form TABULAR/BLANKET
    Thickness 4.57M
    Length 609.6M
    Width 152.4M
    Depth to top 0M
    Depth to bottom 4.57M

Controls for ore emplacement

  • Floodplain

Economic information about the deposit and operations

Development status Past Producer
Commodity type Non-metallic
Deposit size Small
Significant No

Mining district

District name Pine Valley (North)

Land status

Ownership category BLM Administrative Area

Ownership information

  • Type Owner-Operator
    Owner U.S. Bureau Of Land Management

Workings at the site

  • Type of workings Surface
    Area 2.628HA
    Overall length 300M
    Overall width 182.88M

Comments on the workings information

  • AV DEPTH 5 FEET.

Reference information

Bibliographic references

  • Deposit

    EVERTS, M.L., 1979, UT. GEOL. & MINERAL SURVEY; ON-SITE INVESTIGATION

  • Deposit

    1966 DIREXPL UTAH DEPT. OF HIGHWAYS, MATERIALS RESEARCH DI

  • Production

    EVERTS, M.L., 1979, GEOLOGIST.

General comments

Subject category Comment text
Deposit ANGULAR TO SUB-ROUNDED PEBBLES AND COBBLES, WITH SAND AND SILT INTERBEDDING: TABULAR EQUANT AND PROLATE.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-JUL-1979 Everts, Michael L. Bureau of Land Management

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.

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