Fall Creek Coal Mine

Past Producer in Bonneville county in Idaho, United States with commodities Bituminous, Uranium
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. Materials information
  8. Host and associated rocks
  9. Nearby scientific data
  10. Geologic structures
  11. Ore body information
  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 10089388
MRDS ID W019285
Record type Site
Current site name Fall Creek Coal Mine

Geographic coordinates

Geographic coordinates: -111.53221, 43.35881 (WGS84)
Elevation 2073
Relative position 23.5 MI ESE OF AMMON

Site location context

Political divisions (FIPS codes)

Bonneville(county)

Idaho(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Castle Rock(quadrangle 1:24,000 scale)

Palisades(quadrangle 1:100,000 scale)

Driggs(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Palisades(hydrologic unit)

Snake Headwaters(hydrologic accounting unit)

Upper Snake(hydrologic subregion)

Pacific Northwest(hydrologic region)

Federal lands

Caribou-Targhee National Forest(National Forest)

National Forest FS(Type of land area)

FS(Federal land areas administered by FS)

Geographic areas

Country State County
United States Idaho Bonneville

Public Land Survey System information

Meridian Township Range Section Fraction State
Boise 001S 042E 04 Idaho

Commodities

Commodity Importance
Bituminous Primary
Uranium Tertiary

Materials information

Materials Type of material
Jarosite Gangue
Pyrite Gangue

Analytical data

Result SAMPLE ABOVE AS RECEIVED WHEN AIR DRIED ABOUT SAME READINGS OBTAINED
Result CHANNEL AND GRAB SAMPLES OF COAL AVG. 0.02% U
Result AVG. U CONTENT IN TOP 1 FT OF COAL 0.045% U, MINERALIZATION THEN DECREASED DOWNWARD THRU COAL AND CARBONACEOUS SHALES
Result A COAL SAMPLE, AS RECEIVED, HAD 4.6% MOISTURE, 20.7% VOLATILE MATTER, 7.7% FIXED CARBON, 67.5% ASH, 3.3% SULFUR, 2,970 BTU'S

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Coal
    Rock unit name Bear River Formation-Coaly Shale, Limestone, Coal, Quartzite
    Rock description Bear River Formation-Coaly Shale, Limestone, Coal, Quartzite
    Stratigraphic age (youngest) Pliocene
    Stratigraphic age (youngest) Early Cretaceous
    Stratigraphic age (youngest) Early Cretaceous

Nearby scientific data

(1) -111.53221, 43.35881

Economic information

Geologic structures

Type of structure Local
Structure description Gouge, Fractures, Joints, Shear Planes, Anticline Which Trends Nw

Ore body information

  • Strike NW
    Dip 33 DEG NE
    Thickness 1.22M
    Length 804.65M

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1922
Discoverer J. H. Smith (1922)
Year of first production 1922

Mining district

District name Willow Creek - Caribou District

Land status

Ownership category National Forest
Area name Caribou National Forest

Ownership information

  • Type Owner-Operator
    Owner J. H. Smith

Workings at the site

  • Type of workings Surface/Underground
    Length 29.87M
    Overall length 6.1M

Comments on the workings information

  • 1 INCLINED SHAFT, 98 FT DOWN DIP, THE BOTTOM 15 FT CAVED; TRENCH IS 3-5 FT DEEP

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit Discovery Year: 1922, U IN 1951

Reporter information

Type Date Name Affiliation Comment
Reporter 01-MAY-1977 Siefken, Robert R. (Miller, Pat) U.S. Geological Survey

Beyond USGS

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