| 000 | 01174nam a2200217 4500 | ||
|---|---|---|---|
| 001 | 0000002833 | ||
| 003 | OSt | ||
| 005 | 20231219160918.0 | ||
| 008 | 111110 1995 eng d | ||
| 040 |
_aJMGHQ _cJabatan Penyiasatan Kajibumi Malaysia |
||
| 090 | 0 | 0 |
_a551.44709595114 _bCHO |
| 100 | 1 | _aChow, Weng Sum | |
| 245 | 1 | 0 |
_aSinkholes and rockfalls in the Kinta Valley : RAK (F6) _cChow Weng Sum. |
| 260 | _c1995 | ||
| 300 |
_av, 23p. _bcol., ill, maps _c30cm |
||
| 520 | _aAbout 80 percent of the Kinta Valley is underlain by limestone bedrock with some cropping out as hills. Natural erosional processess acting on the limestone bedrock generally give rise to cavities which subsequently could lead to formation of sinkholes. Similar erosional processess acting on the steep cliff faces of the limestone hills could lead to rockfalls. Records show that sinkholes in the Kinta Valley form within a north-northeast- trending zone along the western flank of the valley and within a north-northwest-trending zone along east. | ||
| 650 | 0 |
_aRockfalls _zPahang _zLembah Kinta |
|
| 650 | 0 |
_aSink holes _zPerak |
|
| 651 | 0 | _aLembah Kinta (Pahang) | |
| 942 |
_2ddc _cRPT |
||
| 999 |
_c25160 _d25160 |
||