‡Ref.: A.I.M.E. Ore Deposits of the Western States (1933): 511-512.
An occurrence on Milholland Creek.
Mineralization is hosted in gneissic gabbro. Iron ore occurs in discontinuous dikelike formations, 3 to 8 feet wide, which are parallel to the gabbro and grade into it.
Mineral List: |
Amphibole Group
var: Uralite  | | | | Description: | Alered from pyroxene. | | Reference: | [A.I.M.E. Ore Deposits of the Western States (1933): 511-512.] |
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Epidote | | | | Description: | Altered from feldspar. | | Reference: | [A.I.M.E. Ore Deposits of the Western States (1933): 511-512.] |
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Magnetite
var: Titaniferous Magnetite | | | | Reference: | [A.I.M.E. Ore Deposits of the Western States (1933): 511-512.] |
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3 entries listed. 1 valid mineral.
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