Hostname: page-component-586b7cd67f-t7czq Total loading time: 0 Render date: 2024-11-25T23:31:45.775Z Has data issue: false hasContentIssue false
  • English
  • Français

The Limestone Hills of the Kinta Valley Tinfield, Federated Malay States: their Geology and Physiographic Origin

Published online by Cambridge University Press:  01 May 2009

W. E. Cameron
Get access Rights & Permissions [Opens in a new window]

Extract

The limestone hills of the Kinta Valley, standing up with white cliff faces from an almost level plain, form a prominent and picturesque feature of this prolific tinfield, and attract attention and present a varying scene as viewed from different points in the valley of the Kinta River. Their mode of origin has been the subject of marked divergence of opinion amongst geologists acquainted with them, as has also their age in relation to the series of metamorphic sediments found in the same valley.

Type
Original Articles
Information
Geological Magazine , Volume 62 , Issue 1 , January 1925 , pp. 21 - 27
Copyright
Copyright © Cambridge University Press 1925

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

1 “Secondary Stanniferous Deposits of the Kinta District”: Q.J.G.S., vol. lxxii, pt. 3, 23rd 11, 1917Google Scholar; ‘Dredge Prospecting in the Kinta Valley Mining Journal, London, 30th 09, 1923.Google Scholar

2 “Structural Geology of British Malaya”: Journal of Geology, vol. xxxi, No. 17, 1923.Google Scholar