Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
South African Journal of Geology Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

South African Journal of Geology; March 2005; v. 108; no. 1; p. 3-4; DOI: 10.2113/108.1.3
© 2005 Geological Society of South Africa
This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by McMillan, M. D.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

Exploration history of Rosh Pinah and Aggeneys

The discovery of Rosh Pinah

Michael D. McMillan

18 Derry Road, Newlands, Cape Town, South Africa

The first 20% of the full text of this article appears below.

The writer was assigned the onerous task of mapping the Witputs - Sendelingsdrif area in Namibia in 1963. This coincided with the start of the Precambrian Research Unit at the University of Cape Town.

Field work commenced in May, and in August of that year a move north was made away from the geology along the Orange River, leap frogging across the wide open valley of Namuskluft, to the mountainous area at Gergarub 25kms to the north. A temporary overnight campsite was established on the talus scree of a minor tributary valley cutting its way down the mountain slope. A quick traverse in the late afternoon resulted in the collection of a few pieces of scree - one was struck by the weight of sample that on closer examination turned out to be barite. Traversing upslope of the tributary on the side of the huge anticline, ones attention was drawn by the occasional green copper oxide staining. Closer examination revealed sulphides of lead and zinc. The containing rock was a quartzite-grit sequence.

The writer returned to Gergarub during the university year end vacation in December 1964 to sample and map the outcropping mineralisation that resembled a kind of dolomite rock weathering to a light to dark brown . . . [Full Text of this Article]







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Geological Society of South Africa