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Bonanza; Downing Prospect, Hope Mining District, Kenai Peninsula Borough, Alaska, USAi
Regional Level Types
Bonanza; Downing ProspectProspect
Hope Mining DistrictMining District
Kenai Peninsula BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
60° 49' 27'' North , 149° 31' 10'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Hope192 (2017)12.2km
Girdwood2,250 (2017)23.2km
Moose Pass219 (2014)38.3km
Cooper Landing289 (2017)40.7km
Anchorage298,695 (2017)48.3km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Chugach Gem & Mineral SocietyAnchorage, Alaska48km
Mindat Locality ID:
196595
Long-form identifier:
mindat:1:2:196595:0
GUID (UUID V4):
0


In his description of this deposit, Tuck (1933) also included references to the Whistler (SR020), Francisco (SR017), and to another (unnamed) prospect on Bonanza Creek. The Bonanza property is about halfway between the Francisco and Whistler properties. The Francisco, Whistler, and Bonanza are also known as the Downing mine (Jansons and others, 1984). Tysdal (1978 [MF-880-A]) considered these to be separate prospects.
Location: The Bonanza prospect in the Downing mine area (see additional comments). The prospect is at an elevation of about 2,100 feet on the north bank of Bonanza Creek. It is in the S1/2 section 31, T. 9 N., R. 1 W., of the Seward Meridian. The Bonanza prospect is located about half way between the Francisco (SR017) and Whistler (SR020) properties. This is location 9 of Cobb and Richter (1972), location 8 of MacKevett and Holloway (1977), locations 17, 19, and 20 of Cobb and Tysdal (1980), location 19 of Tysdal (1978 [MF-880-A]), and location S-294 of Jansons and others (1984). The location is accurate to within half a mile.
Geology: This deposit consists of a 6 foot width of 2- to 3-inch-wide quartz stringers parallel to schistose slate of the Valdez Group of Late Cretaceous age (Nelson and others, 1985). The stringers contain a little arsenopyrite and pyrite. In addition to the stringers, there is abundant vuggy quartz float (Tysdal, 1978 [MF-880-A]). Tuck (1933) sampled the stringer lode, but the assays showed only traces of gold and silver.
Workings: The veins are exposed by prospect pits, and there may be a caved adit (Tysdal, 1978 [MF-880-A]). Tuck (1933) sampled across the vein stringers, but the assays indicated only traces of gold and silver.
Age: Cretaceous or younger; the veins cut rocks of the Valdez Group of Late Cretaceous age.
Production: The U.S. Bureau of Mines reported a recorded production of 150 ounces of gold (Jansons and others, 1984). This might include production from the Whistler (SR020) and Francisco (SR017) prospects, as well as the Bonanza.

Commodities (Major) - Au; (Minor) - Ag
Development Status: Undetermined.
Deposit Model: Low-sulfide Au-quartz veins (Cox and Singer, 1986; model 36a)

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


4 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘGold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
ⓘPyrite2.EB.05aFeS2
ⓘArsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
Oⓘ QuartzSiO2
SiSilicon
Siⓘ QuartzSiO2
SSulfur
Sⓘ ArsenopyriteFeAsS
Sⓘ PyriteFeS2
FeIron
Feⓘ ArsenopyriteFeAsS
Feⓘ PyriteFeS2
AsArsenic
Asⓘ ArsenopyriteFeAsS
AuGold
Auⓘ GoldAu

Other Databases

Link to USGS - Alaska:SR018

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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