| Deposit ID | 10001727 |
|---|---|
| MRDS ID | A012511 |
| Record type | Site |
| Current site name | Unnamed (west of the Middle Fork Chandalar River) |
| Related records | 10112117 |
| Geographic coordinates: | -147.82335, 68.03976 (WGS84) |
|---|---|
| Relative position | Site is at an elevation of about 3,750 ft. in a small drainage approximately 2 miles west of the Middle Fork Chandalar River and about 7 miles south of the confluence of Beaucoup Creek and Middle Fork Chandalar River (south-center sec. 19, T. 16 S., R. 19 E., of the Umiat Meridian). It is described as Area B on fig. 1 in Detra (1977). Location accurate within 1/4-mile radius. |
Political divisions (FIPS codes)
North Slope(Borough)
Alaska(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Philip Smith Mountains A-2(quadrangle 1:63,360 scale)
Arctic SW(quadrangle 1:100,000 scale)
Philip Smith Mountains(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Alaska(hydrologic region)
Federal lands
Arctic National Wildlife Refuge(National Wildlife Refuge)
National Wildlife Refuge FWS(Type of land area)
FWS(Federal land areas administered by FWS)
| Country | State |
|---|---|
| United States | Alaska |
| Commodity | Importance |
|---|---|
| Lead | Primary |
| Zinc Critical | Primary |
| Silver | Secondary |
| Copper | Secondary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Galena | Ore |
| Sphalerite | Ore |
| Tetrahedrite | Ore |
| Quartz | Gangue |
| Model code | 224 |
|---|---|
| USGS model code | 32a |
| Deposit model name | Mississippi Valley, S.E. Missouri Pb-Zn |
| Mark3 model number | 42 |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Volcanic Breccia (Agglomerate) |
| Rock unit name | Skajit Limestone;Beaucoup Formation; Brown Shale Member |
| Rock description | Skajit Limestone;Beaucoup Formation; Brown Shale Member |
| (1) | -147.82335, 68.03976 |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| District name | Chandalar |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | A012511 | |
| USGS | Alaska Resource Data File | ARDF | PS007 |
Cathrall, J.B., Cooley, E.F., Detra, D.E., and O'Leary, R.M., 1977, A listing and statistical summary of spectrographic and chemical analysis of stream-sediment and rock samples from the Philip Smith Mountains quadrangle, Alaska: U.S. Geological Survey Open-File Report 77-244, 79 p.
Detra, D.E., 1977, Delineation of an anomalous lead-zinc area in the Philip Smith Mountains A-2 quadrangle, Alaska: U.S. Geological Survey Open-File Report 77-223, 11 p.
Barker, J.C., 1978, Mineral Investigations of certain lands in the eastern Brooks Range: a summary report: US Bureau of Mines Open-File No. 63-78
Dutro, J.T., Jr., 1978, Potential stratabound lead-zinc mineralization, Philip Smith Mountains quadrangle, Alaska, in Johnson, K. M., ed., The United States Geological Survey in Alaska, Accomplishments during 1977: U.S. Geological Survey Circular 772-B, p. B9-B11.
Menzie, W.D., Reiser, H.N., Brosgi, W.P., and Detterman, R.L., 1985, Map showing distribution of mineral resources (excepting oil and gas) in the Philip Smith Mountains quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Investigations Map MF-879-C, 2 sheets, scale 1:250,000.
Schmidt, J.M., 1997, Shale-hosted Zn-Pb-Ag and barite deposits of Alaska, in Goldfarb, R.J., and Miller, L.D., eds., Mineral Deposits of Alaska, 1997: Economic Geology Monograph 9, p. 35-65.
Maas, K.M., 1987, Availability of land for Mineral exploration and development in northern Alaska, 1986: U.S. Bureau of Mines Special Publication, 34 p., 33 sheets.
| Subject category | Comment text |
|---|---|
| Deposit | Model Name = Mississippi Valley Zn-Pb (?) (Cox and Singer, 1986; model 32a). |
| Deposit | Other Comments = See also locations PS006 and PS008. Site is in an area thought to have potential for carbonate-hosted lead-zinc deposits (Menzie and others, 1985). The pH of the stream that cuts the mineralization is less than 4.5. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 17-NOV-1999 | J.M. Britton | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
These are landing pages for further research — the state agencies don't currently expose per-mine deep links.