000 | 01143nam a2200205 4500 | ||
---|---|---|---|
001 | 0000002820 | ||
008 | 111108s 1940 may d | ||
040 | _aJMGHQ | ||
090 | 0 | 0 |
_a553.4109595114 _bRIC |
100 | 1 | _aRichardson, J. A. | |
245 | 1 | 0 |
_aReport on Sungai Satak area, occurrence of gold Ulu Jelai _cJ. A. Richardson. |
260 | _c1940 | ||
300 |
_a1 v. (unnumbered) _c30cm |
||
520 | _aGold occurs in the alluvium of most of the valleys of rivers draining from the syenite. It is found in the Sungei Panau, on which the three areas, numbered 1, 2, and 3, are situated. Most of the gold occurs in coarse grained alluvial deposits, commonly boulder bads, cobble beds, and gravels, resting on bedrock either of sedimentary, pyroclastic or igneous rocks. The thickness of the alluvium generally does not exceed 15 feet or 20 feet; it may be less than 10 feet or but a few feet thick. | ||
650 | 0 |
_aGeology _zPerak _zUlu Jelai |
|
650 | 0 |
_aGold _xGeology _zPerak _zUlu Jelai |
|
650 | 0 |
_aGeology, Economic _zPerak _zUlu Jelai |
|
650 | 0 |
_aRiver sediments _zPerak _zUlu Jelai _zPanau, Sungei |
|
651 | 0 | _aPanau, Sungei (Ulu Jelai, Perak) | |
999 |
_c22568 _d22568 |