| Deposit ID | 10002770 |
|---|---|
| MRDS ID | A015232 |
| Record type | Site |
| Current site name | Unnamed (Tatonduk River) |
| Related records | 10232782 |
| Geographic coordinates: | -141.10164, 65.03591 (WGS84) |
|---|---|
| Relative position | This occurrence consists of scattered redbed outcrops for nearly 2 miles along the lower Tatonduk River and extends into the high country on both sides of the river. The outcrop area encompasses most of the northwest quarter of T. 2 N., R. 33 E., of the Fairbanks Meridian, and the southwest quarter of T. 3 N., R. 33 E., of the Fairbanks Meridian. The coordinates are for the approximate center of the outcrop area, in section 6, T. 2 N., R. 33 E., of the Fairbanks Meridian. The occurrence is location 2 of Cobb (1972; MF-0390). The location is accurate. |
Political divisions (FIPS codes)
Southeast Fairbanks(Census area)
Alaska(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Charley River A-1(quadrangle 1:63,360 scale)
Charley River SE(quadrangle 1:100,000 scale)
Charley River(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Alaska(hydrologic region)
Federal lands
Yukon-Charley Rivers National Preserve(National Preserve)
National Preserve NPS(Type of land area)
NPS(Federal land areas administered by NPS)
| Country | State |
|---|---|
| United States | Alaska |
| Commodity | Importance |
|---|---|
| Iron | Primary |
| Materials | Type of material |
|---|---|
| Hematite | Ore |
| Model code | 241 |
|---|---|
| USGS model code | 34a |
| Deposit model name | Superior Fe (BC name is Lake Superior & Rapitan types iron-formation) |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Mafic Volcanic Rock > Basalt | ||
| |||
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff |
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Mafic Volcanic Rock > Basalt |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale |
| Rock unit name | Tindir Group |
| Rock description | Tindir Group |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Conglomerate |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Dolomite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff |
| (1) | -141.10164, 65.03591 |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| District name | Black |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | A015232 | |
| USGS | Alaska Resource Data File | ARDF | CY032 |
Berg, H.C., and Cobb, E.H., 1967, Metalliferous Lode Deposits of Alaska. U.S. Geological Survey Bulletin 1246, 254 p.
Kimball, A.L., 1969, Reconnaissance of Tatonduk River red beds: U.S. Bureau of Mines Open-File Report 1-69, 11 p.
Cobb, E.H., 1972, Metallic mineral resources map of the Charley River quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-390, 1 sheet, scale 1:250,000.
Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Charley River and Coleen quadrangles, Alaska: U.S. Geological Survey Open-File Report 76-632, 45 p.
Mertie, J.B., Jr., 1938, Gold placers of the Fortymile, Eagle, and Circle districts, Alaska: U.S. Geological Survey Bulletin 897-C, p. 133-261.
| Subject category | Comment text |
|---|---|
| Deposit | Model Name = Superior Fe (Cox and Singer, 1986; model 34a). |
| Deposit | Other Comments = This site is within the Yukon-Charley Rivers National Preserve. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 07-APR-00 | Cameron, C.E. | Alaska Division of Geological and Geophysical Surveys |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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