Vote for your favorite mineral in #MinCup26! - Sphalerite vs. Anorthite
Both zinc ore Sphalerite and calcium plagioclase feldspar Anorthite have perfect cleavage that will split cleanly if you hit them with a hammer, but only one can claim a larger split of your votes!
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Unnamed Occurrence (ARDF - PA035; near Redfish Bay), Chichagof Mining District (Chicagof Mining District), Sitka, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - PA035; near Redfish Bay)- not defined -
Chichagof Mining District (Chicagof Mining District)Mining District
SitkaCity Borough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
56° 21' 27'' North , 134° 52' 51'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
201484
Long-form identifier:
mindat:1:2:201484:8
GUID (UUID V4):
0


MAS number: 0021160021.
Location: This occurrences is a pegmatite about 600 feet in diameter that is about 1.0 mile west of the head of Redfish Bay near the middle of the south boundary of section 36, T. 63 S., R. 67 E. The location is accurate.
Geology: As described by Sainsbury (1957), this occurrence consists of a circular body of pegmatite about 600 feet in diameter. The pegmatite is in a large composite intrusive body near the contact of monzonite or granite and quartz diorite. Loney and others (1975) map the body as tonalite and granodiorite of Tertiary age. Detailed mapping by Sainsbury indicates that the pegmatite consists of two or more dikelike phases. The pegmatite is zoned with a core of quartz surrounded by a shell of variable mineralogy that includes areas of perthite, quartz, and graphic granite; microcline-perthite; and perthite, mica, and quartz. A border zone is generally quartz and graphic granite. The chief commodity of interest is microcline-perthite that occurs in zones 4 to 10 feet thick; the largest zone is at least 120 feet long and 6 to 8 feet thick. There is some optical-grade quartz. Sainsbury tentatively identified a few grains of cassiterite, but there is no indication of beryllium, columbium, or tantalum minerals. The pegmatite is not radioactive.
Workings: Probably none beyond surface examination and sampling by the U.S. Geological Survey and U.S. Bureau of Mines.
Age: The pegmatite is in a large Tertiary granitic intrusion and is probably the same age.
Reserves: None.

Commodities (Major) - Microcline-perthite, quartz? ; (Minor) - Sn?
Development Status: None
Deposit Model: Pegmatite.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


1 valid mineral.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Unclassified
'Feldspar Group'-
'Mica Group'-

List of minerals for each chemical element

OOxygen
O QuartzSiO2
SiSilicon
Si QuartzSiO2

Other Databases

Link to USGS - Alaska:PA035

Other Regions, Features and Areas containing this locality

North America PlateTectonic Plate

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