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Sunshine / Mineral Mountain |
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Pays |
USA
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Etat / Province |
Idaho |
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Près de |
Wallace |
Statut |
LAND HOLDING
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Marché minier |
Silver Valley |
Superficie |
0 km² / 46 acres |
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Latitude / Longitude |
47 N 30 / 116 W 02 |
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Légende
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Risques / Pays : Tres bas |
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| VanEck Vectors Global Alternative Energy ETF Leaser: 100% |
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Titre | Profil de la Compagnie | Tous les projets | Site web de la compagnie | Page projet de la compagnie |
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In 2004, Sterling leased the Mineral Mountain claim groups pursuant to a 25-year lease, renewable for an additional 25 years. The lease, which expires in 2029, required the issuance to the lessor of 30,000 shares of the Company’s common stock, and pr Plus... |
| VanEck Vectors Global Alternative Energy ETF Owner: 33,3% |
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Titre | Profil de la Compagnie | Tous les projets | Site web de la compagnie | Page projet de la compagnie |
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In mid-2003, Mineral Mountain leased its property to Sterling Mining Company on a 25 year exploration and production lease. In addition to receiving 25,000 shares of Sterling stock, Mineral Mountain receives a $3,600/year royalty and has retained a 3 Plus... |
| VanEck Vectors Global Alternative Energy ETF Owner: 30% |
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Titre | Profil de la Compagnie | Tous les projets | Site web de la compagnie | Page projet de la compagnie |
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Mineral Mountain is the owner of an undivided one-third interest in the "Mineral Mountain Area" near Osburn, Idaho, and consisting of the four original Mineral Mountain patented lode mining claims together with those portions of six Chester and three Polaris claims, 300 feet north of the center of the Chester Vein on the Polaris Fault
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The Mineral Mountain Mine consists of a 500 foot drift that explores the Mineral Mountain vein. There is no record of production from the original Mineral Mountain Mine. Exploration drifts from the ConSil Mine explored beneath the Mineral Mountain pr Plus...
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The Mineral Mountain property straddles the Polaris Fault, which hosts the silver deposits are currently being exploited in the nearby Galena Mine. Much of the property is underlain by belt rocks of the St. Regis and lower Wallace rocks, consisting of quartzites and argillites. It is these quartzite units that host many of the silver veins in the silver valley.
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Données mises à jour le : 17/09/2007
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Conditions d'utilisation
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Toutes les informations présentes sur cette page proviennent de sources internes et externes considérées comme fiables. Ces informations peuvent ne pas être à jour, il est vous donc vivement conseillé de recouper ces informations avant de faire quoi que ce soit. Merci de nous contacter dans le cas ou une information manquerait ou s'avererait incorrecte.
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