Quartz Creek Occurrence (Ear Mountain area), Port Clarence Mining District, Nome Census Area, Alaska, USAi
Regional Level Types | |
---|---|
Quartz Creek Occurrence (Ear Mountain area) | Occurrence |
Port Clarence Mining District | Mining District |
Nome Census Area | Census Area |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
65° 54' 14'' North , 166° 19' 51'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Shishmaref | 580 (2017) | 40.9km |
Mindat Locality ID:
199537
Long-form identifier:
mindat:1:2:199537:7
GUID (UUID V4):
fcf59d08-460a-4028-aafe-3c79712cecd4
Location: Quartz Creek is an east tributrary to Tuttle Creek that drains the southwest flank of Ear Mountain. It crosses the contact zone, and has headwaters in, the Ear Mountain granite stock (Sainsbury, 1972). Ear Mountain is an isolated upland reaching 2,329 feet elevation in the north-central Teller D-3 quadrangle. Three USBM churn-drill holes were completed at about 370 feet elevation and two were completed at about 680 feet elevation on this creek (Mulligan, 1959, p. 20). Coordinates for this occurrence are for the location at the lower elevation. This is locality 51 of Cobb and Sainsbury (1972). Cobb (1975) summarized references to this location under the name 'Quartz Cr.'.
Geology: Quartz Creek crosses the contact zone, and has headwaters in, the Ear Mountain granite stock (Sainsbury, 1972). This is a Late Cretaceous (76.7 +/- 2.9 my; Hudson and Arth, 1983, p. 769) composite biotite granite that intrudes an impure and schistose carbonate sequence, with some metapelitic rocks, of unknown but probable Paleozoic age. Three USBM churn-drill holes were completed at about 370 feet elevation and two were completed at about 680 feet elevation on this creek (Mulligan, 1959, p. 20). Coordinates for this occurrence are for the location at the lower elevation. These churn-drill holes encountered 3 to 6.5 feet of gravel. The lower part of the gravel and adjacent bedrock contained a trace of tin per cubic yard in two of the holes at 370 feet elevation. Minerals identified in samples here include quartz, calcite, oligoclase, orthoclase, garnet, diopside, and traces of pyrite, limonite, idocrase, tourmaline, epidote, chlorite, biotite, actinolite, and muscovite. Tin-bearing minerals were not identified (Mulligan, 1959, p. 30) although heavy mineral concentrates from this creek contained monazite, zircon, cassiterite, zenotime, apatite, and scapolite (Killeen and Ordway, 1955, p. 81-82).
Workings: A total of 5 churn-drill holes were completed on this creek (Mulligan, 1959, p. 20).
Age: Quaternary
Reserves: Not defined
Commodities (Major) - Sn
Development Status: None
Deposit Model: Alluvial tin placer (Cox and Singer, 1986; model 39e)
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
1 valid mineral.
Detailed Mineral List:
ⓘ Cassiterite Formula: SnO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 4 - Oxides and Hydroxides | |||
---|---|---|---|
ⓘ | Cassiterite | 4.DB.05 | SnO2 |
List of minerals for each chemical element
O | Oxygen | |
---|---|---|
O | ⓘ Cassiterite | SnO2 |
Sn | Tin | |
Sn | ⓘ Cassiterite | SnO2 |
Other Databases
Link to USGS - Alaska: | TE062 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Brooks-Seward DomainDomain
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