| Deposit ID | 10233618 |
|---|---|
| MRDS ID | A000314 |
| MAS/MILS ID | 0020910021 |
| Record type | Site |
| Current site name | Kapon Creek |
| Alternate or previous names | Kapon Creek Discovery, Kapon Creek No. 2 Above Discovery |
| Point of reference | Claim |
|---|---|
| Geographic coordinates: | -160.24776, 60.1693 (WGS84) |
| Elevation | 549 |
| Location accuracy | 500(meters) |
Political divisions (FIPS codes)
Bethel(Census area)
Alaska(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Bethel A-4(quadrangle 1:63,360 scale)
Bethel SE(quadrangle 1:100,000 scale)
Bethel C(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Kuskokwim Delta(hydrologic unit)
Lower Kuskokwim River(hydrologic accounting unit)
Southwest(hydrologic subregion)
Alaska(hydrologic region)
Federal lands
Yukon Delta 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 |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Seward | 001 N | 063 W | 20 | C | Alaska |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Mercury | Tertiary |
| Claim (1) | -160.24776, 60.1693 |
|---|
| Operation type | Placer |
|---|---|
| Development status | Occurrence |
| Commodity type | Metallic |
| Significant | No |
| Type of mineral rights | Located Claim |
|---|
| Ownership category | Federal |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| U.S. Bureau of Mines | Minerals Availability System | MAS | 0020910021 | |
| USGS | Mineral Resources Data System | MRDS | A000314 | MAS references MRDS |
| Subject category | Comment text |
|---|---|
| Deposit | HEADWATER TRIBUTARY OF EEK RIVER. SLATE AND CONGLOMERATE BEDROCK CUT BY GRANITIC INTRUSIVES. A LITTLE MINING IN 1914-15. THE REPROT OF GRANITIC INTRUSIVES ROCKS ON KAPON CREEK IS PROBABLY BASED ON ERR0NEOUS HEARSAY BECAUSE MADDREN NEVER SAW THE CREEK AND I SAW NO GRANITIC ROCKS WHEN I MAPPED THE AREA. HOWEVER THERE ARE SOME RYOLITE AND DIABASE DIKES AND SILLS. THE ROCKS AND THE ASSOCIATION OF GOLD AND CINNABAR ON KAPON CREEK ARE SIMILAR TO ARSENIC CREEK. THE COURSE OF KAPON CREEK IS PROBABLY FAULT-CONTROLLED BECAUSE 1) THE STREAM IS UNUSUALLY STRAIGHT, 2) IT CUTS ACROSS THE BEDDING WHICH STRIKES NORTH-EAST AND DIP CONSISTENTLY SOUTHEAST, AND 3) IT IS ESSENTIALLY PARALLEL TO THE UPPER PART OF KWETHLUK VALLEY WHICH IS DEVELOPED ALONG THE TRAIL CREEK FAULT . (HOARE)0 |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 23-DEC-1996 | Sbh | U.S. Bureau of Mines |
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.