| Deposit ID | 10023527 |
|---|---|
| MRDS ID | I000621 |
| Record type | Site |
| Current site name | Bi'R Hayzan Diatomite Deposit |
| Geographic coordinates: | 39.17437, 27.59369 (WGS84) |
|---|---|
| Relative position | DEPOSIT IS FOUND IN THE SOUTHWESTERN ARM OF THE NAFUD SAND SEA, ABOUT 67 KM EAST OF TAYMA IN NORTHWESTERN SAUDI ARABIA. |
Political divisions (FIPS codes)
Saudi Arabia(country)
| Country |
|---|
| Saudi Arabia |
| Commodity | Importance |
|---|---|
| Diatomite | Primary |
| Materials | Type of material |
|---|---|
| Diatomite | Ore |
| Result | BASED ON 4 SAMPLES: 85% SIO2 |
|---|---|
| Result | 2.34% FE2O3 |
| Result | 1.4% AL2O3 |
| Result | AND 8.27% LOI (THESE SAMPLES WERE NOT OVEN-DRIED FIRST, THEREFORE THE SILICA CONTENT IS PROBABLY IN EXCESS OF 89%). THE DIATOMITE HAS LOW BULK DENSITY (0.64 G/CUB. CM) AND AN AVERAGE POROSITY OF 63%. |
| Model code | 222 |
|---|---|
| USGS model code | 31s |
| Deposit model name | Lacustrine diatomite |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Unconsolidated Deposit > Sand and Gravel | ||
| |||
| (1) | 39.17437, 27.59369 |
|---|
| Dip | 5 TO 9 DEG NE |
|---|---|
| Thickness | 2.2M |
| Development status | Prospect |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000621 |
WHITNEY, J.W., 1982, PRELIMINARY GEOLOGICAL INVESTIGATION OF THE BI'R HAYZAN DIATOMITE DEPOSIT, KINGDOM OF SAUDI ARABIA, WITH A SECTION ON SELECTED PHYSICAL PROPERTIES AND IMPLICATIONS FOR FUTURE GEOPHYSICAL EXPLORATION BY MARK E. GETTINGS: U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 82-1046, 25 P
| Subject category | Comment text |
|---|---|
| Deposit | THE LACUSTRINE DIATOMITE BEDS LIE STRATIGRAPHICALLY ABOVE EOLIAN SAND AND BELOW A LARGE BARCHANOID DUNE, INDICATING DEPOSITION DURING AN EXCEPTIONAL PERIOD OF PLUVIAL CLIMATE IN AN OTHERWISE ARID SAND DESERT, PROBABLY DURING THE LAST INTERGLACIAL CLIMATE OF THE PLEISTOCENE. DIATOMITE RELATED TO THE SAME PLUVIAL EPISODE HAS ALSO BEEN FOUND IN THE AFAR REGION OF ETHIOPIA. THE BI'R HAYZAN DEPOSIT IS EXPOSED ON THE WINDWARD SIDE OF THE LARGE TRANSVERSE DUNE. THE EXPOSED SECTION OF DIATOMITE IS 450 M LONG. THE DIATOMITE IS 1.6 TO 2.2 M (AVE. 1.85 M) THICK IN THE OUTCROP AND HAS PARALLEL LAMINAE. THERE ARE MINOR IRON OXIDE STAINS ON THE SURFACE OF THE OUTCROP AND NEAR THE TOP OF THE DEPOSIT. THERE ARE NO INTERBEDS OF SAND, SILT, OR CLAY IN HTE DEPOSIT. WHITNEY ESTIMATED THAT DIATOMITE SEDIMENTATION LASTED AT LEAST 880 YEARS. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1990 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.