| Deposit ID | 10048671 |
|---|---|
| MRDS ID | MP00286 |
| Record type | Site |
| Current site name | King's Clay |
| Alternate or previous names | Locality No. 11, Sublimity Locality |
| Geographic coordinates: | -122.73035, 44.86953 (WGS84) |
|---|---|
| Relative position | ABOUT 6 MI NORTHEAST OF STAYTON |
Political divisions (FIPS codes)
Marion(county)
Oregon(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Stout Mountain(quadrangle 1:24,000 scale)
North Santiam River(quadrangle 1:100,000 scale)
Salem(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Molalla-Pudding(hydrologic unit)
Willamette(hydrologic accounting unit)
Willamette(hydrologic subregion)
Pacific Northwest(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Oregon | Marion |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Willamette | 008S | 001E | 18 | SW4 OF SE4 | Oregon |
| Commodity | Importance |
|---|---|
| Clay | Primary |
| Materials | Type of material |
|---|---|
| Kaolinite | Ore |
| Limonite | Gangue |
| Quartz | Gangue |
| Result | SEVERAL SAMPLES YIELDED FUSION AT CONE 27 TO CONE 33 |
|---|
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Mafic Volcanic Rock > Basalt | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff |
| (1) | -122.73035, 44.86953 |
|---|
| General form | MASSIVE |
|---|---|
| Thickness | 4.57M |
| Length | 243.84M |
| Width | 121.92M |
| Development status | Occurrence |
|---|---|
| Commodity type | Non-metallic |
| Deposit size | Small |
| Significant | No |
| Type | Operator |
|---|---|
| Owner | Willamina Clay Products Co. |
| First year | 1937 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | MP00286 | |
| U.S. Bureau of Mines | Minerals Availability System | MAS | 0410470027 |
WILSON AND TREASHER, 1938
WILSON, HEWITT, AND TREASHER, R.C., 1938, PRELIMINARY REPORT OF SOME OF THE REFRACTORY CLAYS OF WESTERN OREGON: OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES BULLETIN 5, P. 49-54
| Subject category | Comment text |
|---|---|
| Deposit | DESCRIPTION OF CLAY SUGGESTS IT IS A HYDROTHERMAL ALTERATION PRODUCT OF A PUMICEOUS TUFF. "BROWN VEINS" DO NOT SEEM TO HAVE DEVELOPED, AS IRON OXIDE MATERIAL IS CITED AS HAVING PERCOLATED DOWN FROM OVERLYING TUFF BASED ON GREATER ABUNDANCE NEAR UPPER CONTACT OF CLAY WITH TUFF. A MODEL HAS NOT YET BEEN PUBLISHED FOR THIS TYPE OF DEPOSIT. DIMENSIONS GIVEN WERE PRESUMED BASED UPON DRILL HOLE DATA AND WERE USED TO CALCULATE POSSIBLE RESOURCES. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-AUG-1994 | Peterson, Jocelyn A. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.