The geology of Sarawak and Sabah caves G. E. Wilford
Material type:
TextPublisher: 1964Description: viii, 181 p. ill., maps, photos 26 cmSubject(s): Geology -- SarawakSummary: Limestone caves are the commonest and they occur in all the larger limestone hills. The limestones are of Permian, Jurassic, and Cretaceous age in west Sarawak and mainly of Tertiary age in East Sarawak dan Sabah; The 20 largest outcrops which contain caves cover about 200 square miles
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 550.59522 WIL (Browse shelf) | Available | 0000005799 |
Total holds: 0
Browsing JMG IBUPEJABAT shelves, Shelving location: Open Shelf, Collection: Open Shelf Close shelf browser
| 550.59522 RIC Major geological events since cretaceous in Sarawak, Malaysia | 550.59522 RIC Planktonic foraminferal biostratigraphy of northwest Sarawak, Malaysia | 550.59522 RIC The cretaceous of Sarawak, Malaysia | 550.59522 WIL The geology of Sarawak and Sabah caves | 550.5952211 DEN Geology of the Kuching area, west Malaysia | 550.5952211 YOG Geological considerations in the development of the Kuching area | 550.5952251 LAM The importance of geology in urban planning and development of the Sibu area, Sarawak |
Includes bibliographical references
Limestone caves are the commonest and they occur in all the larger limestone hills. The limestones are of Permian, Jurassic, and Cretaceous age in west Sarawak and mainly of Tertiary age in East Sarawak dan Sabah; The 20 largest outcrops which contain caves cover about 200 square miles
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