Silver Island Mountain Mining Area

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  • ExpUt
    Senior Member
    True Mojave
    • Jul 2008
    • 557

    Silver Island Mountain Mining Area

    Spent a couple of gorgeous days exploring and documenting the mines of the Silver Island Mountains with Corey & Jess (GoldRushExpedition.com) and a couple of other ExpeditionUtah members. We had the entire mountain range to ourselves, literally not a sole in site We visited a handful of mine and cave sites, several of which took some serious hiking.

    I visited several of these mines last June on a similar trip to the range, following that I did some brief online searching and didn't come up with much info. I've been playing around for the last few minutes on Google and I'm coming up with the same void. There are likely 50+ openings in the range, several semi-permanent cabins (ruins) and some obvious "tent city" sites so I would imagine there is some better info out there. Was it called a different name? Anyone have any info on the area?
    Kurt Williams
    CruiserOutfitters.com
    ExpeditionUtah.com
    MojaveUnderground.com
  • rhartill
    Advanced Explorer
    Mojave Outlaw
    • Jun 2008
    • 226

    #2
    Silver Island Mtns in Box Elder County?

    B115 from the UGS (Geology Mineral Resources of Box Elder County) has some info on the Silver Island Mtns Mining District, also known as CRATER LAKE Mining District...

    the scanned text is as follows: Crater Island Mining District
    The Crater Island mining district (figure 36) is
    located III the southwest part of Box Elder County at
    the nurthern end of the Silver Island Mountains about
    12 miles suutheast of the Lucin mining district. It is
    ahout 25 miles northeast of Wendover. Utah, the nearest
    tllwn and paved road. Crater Island is a mountainous
    mass approximatel:: six miles long north-south and
    4 miles \vide cast-west. It is separated from the major
    part uf the range by a narrow neck or bar of gravel called
    the Donner-Reed Pass. Otherwise this mountain would
    be a true island surrounded by the mud-nat "sea" of the
    Great Salt Lake Desert
    Claiming of the miner~!l occurrences commenced
    about 1873 but no production was reported until 1908.
    In earlier years the district was regarded as an area of the
    larger Silver Island mining district (l1111stly in Tooele
    County), but the term Crater Island district began tD be
    used after 1901. It is impossible to separate thc value of
    the Box Elder County portion of the district as records
    were generally combined. The Silver Island district was
    important for silver. lead, copper, ~ll1d a slllall amount of
    gold.
    Butler (1920) reports that from 1908 to 1913 the
    Silver Island mining district produced metals valued at
    S90)19, but Anderson (1960, p. 159) thinks that
    almost all production was from the Carrie Mack mine in
    Tooele County. Bureau of Mines' Mineral Yearbooks
    show that the Crater Island mining district was active
    betwecn 1934 and 1948, whell 94 Ollnces of gold, 1,194
    ounces of silver, 23,666 pounds of copper and 91
    pounds of lead were produced and valued at S7,854.
    Recently, tungsten deposits were discovered on Crater
    Island: there was no production through 1974, but
    development work was being carried out.
    Geologically, Crater Island is a mass 0 f Paleozoic
    rock. badly broken by north-south trending faults and
    intruded by granitic rock (quart! monzonite and granodiorite)
    (figure 37). The largest outcrop of igneolls
    rock, the Crater Island stock, is at the south end of the


    island. Some smaller intrusive outcrops occur at
    Desolate Point to the southeast. and two outcrops,
    the North and Sheepwagon stocks, each olle mik by l.~
    mile, are found to the northeast. The Paleol.llic rocks are
    dominated by carbonates.
    The mines and prospects of Crater Island are
    mostly scattered on the east side of the mountain mass.
    AnJerson (1960, p. 160) notes that the mineralization is
    limited to ( I) portions of the tactite zones between the
    granitic and Paleozoic rocks, (2) quartz and calcite veins,
    and (3) slight random occurrences in the highly jointed
    Swan Peak Quartzite. Some LlUlts show local ironstaining
    and alteration. Mincralization has been noted in
    Ordovician, Cambrian, and Permian rock and to a slight
    extent in the granitic rocks.

    The reference to Anderson, 1960 (sic) is as follows:

    Anderson, W. L., 1957, Geology of the northern Silver Island
    Mountains, Box Elder and Tooele Counties, Utah: University
    of Utah M. S. thesis.
    At the U of U Library:
    Collection: ML: ARC available by request
    Call No.: QE3.5 1957 .A5

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    • Derek
      Advanced Explorer
      Mojave Outlaw
      • Jul 2008
      • 340

      #3
      Isn't most of the that mountain now a wilderness lock down err I mean study area? If so I'm sure that this further complicates travel to the mine locations.
      -Derek
      Mojave Mine Team

      Comment

      • ExpUt
        Senior Member
        True Mojave
        • Jul 2008
        • 557

        #4
        Originally posted by cheever
        Isn't most of the that mountain now a wilderness lock down err I mean study area? If so I'm sure that this further complicates travel to the mine locations.
        Thankfully its not. Several of the other major ranges in the area have been absorbed into Wilderness, the Cedar Range, Deep Creeks, etc. This range has been inventoried and proposed for Wilderness, but fingers crossed it doesn't happen. Regardless, most of the mines are fully accessible from the current road, there are a couple of faint roads we traveled to mine sites but the majority of the sites in the range require hiking.
        Kurt Williams
        CruiserOutfitters.com
        ExpeditionUtah.com
        MojaveUnderground.com

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