Hot Springs Creek Occurrence, Serpentine Mining District, Nome Census Area, Alaska, USAi
Regional Level Types | |
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Hot Springs Creek Occurrence | Occurrence |
Serpentine Mining District | Mining District |
Nome Census Area | Census Area |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
65° 51' 36'' North , 164° 42' 36'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Mindat Locality ID:
198055
Long-form identifier:
mindat:1:2:198055:7
GUID (UUID V4):
aaf1a115-1a46-441d-8f9a-9b3bac165a44
Location: The location of this occurrence is very approximate; it can only be located to within one or two miles. Moxham and West (1953) note cinnabar 'in concentrates panned from a shallow gully in the south side of the eastern fork of Hot Springs CreeK'. Hot Springs Creek is a tributary of the Serpentine River with headwaters in the Oonatut Granite Complex (Hudson, 1979). The location description suggests that the occurrence is in an area underlain by Oonatut Granite; the presence of cinnabar has not been confirmed and the locality was not shown by Cobb (1972; MF 417). Cobb (1975; OFR 75-429) summarized references to this locality under the name 'Hot Springs Cr.'.
Geology: Moxham and West (1953) note cinnabar 'in concentrates panned from a shallow gully in the south side of the eastern fork of Hot Springs CreeK'. Hot Springs Creek is a tributary of the Serpentine River with headwaters in the Oonatut Granite Complex (Hudson, 1979). The location description suggests that the occurrence is in an area underlain by Oonatut Granite; the presence of cinnabar here has not been confirmed. In general, only the central, late-forming part of the Oonatut Granite Complex is hydrothermally altered (Hudson, 1979). This is an evolved tin granite complex (Hudson and Arth, 1983) and its accessory mineral content (apatite, allanite, sphene, and zircon) is responsible for its slightly elevated levels of uranium and thorium (Moxham and West, 1953). The weathering of the granite has contributed these minerals to alluvial gravels in the area.
Workings: None.
Age: Not known; the Oonatut Granite is Late Cretaceous (about 70 my, Hudson, 1979) but if cinnabar is present it may be different in age.
Commodities (Major) - Hg; (Minor) - Radioactive minerals
Development Status: No
Deposit Model: Placer cinnabar concentration (?)
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
β 'Allanite Group' Formula: (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
β Cinnabar Formula: HgS |
β 'Hydrogoethite' Formula: 3Fe2O3 · 4H2O |
β Titanite Formula: CaTi(SiO4)O |
β Zircon Formula: Zr(SiO4) |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
β | Cinnabar | 2.CD.15a | HgS |
Group 9 - Silicates | |||
β | Zircon | 9.AD.30 | Zr(SiO4) |
β | Titanite | 9.AG.15 | CaTi(SiO4)O |
Unclassified | |||
β | 'Hydrogoethite' | - | 3Fe2O3 Β· 4H2O |
β | 'Allanite Group' | - | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Hydrogoethite | 3Fe2O3 · 4H2O |
H | β Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
O | Oxygen | |
O | β Titanite | CaTi(SiO4)O |
O | β Zircon | Zr(SiO4) |
O | β Hydrogoethite | 3Fe2O3 · 4H2O |
O | β Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
Si | Silicon | |
Si | β Titanite | CaTi(SiO4)O |
Si | β Zircon | Zr(SiO4) |
Si | β Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
S | Sulfur | |
S | β Cinnabar | HgS |
Ca | Calcium | |
Ca | β Titanite | CaTi(SiO4)O |
Ti | Titanium | |
Ti | β Titanite | CaTi(SiO4)O |
Fe | Iron | |
Fe | β Hydrogoethite | 3Fe2O3 · 4H2O |
Zr | Zirconium | |
Zr | β Zircon | Zr(SiO4) |
Hg | Mercury | |
Hg | β Cinnabar | HgS |
Other Databases
Link to USGS - Alaska: | BN114 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Brooks-Seward DomainDomain
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