Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
  Environmental and Engineering Geoscience   Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Environmental and Engineering Geoscience; August 1999; v. 5; no. 3; p. 271-313
This Article
Right arrow Submit a response
Right arrow Alert me when this article is cited
Right arrow Alert me when eLetters are posted
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 Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Right arrow Order Hardcopy of Full Text via AGI/GeoRef
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Bell, F. G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The Lesotho Highlands Water Project; a geotechnical and engineering geological review of the initial phase

F. G. Bell

University of Natal, Department of Geology and Applied, Durban, South Africa

The purpose of Lesotho Highlands Water Project is primarily to supply water from Lesotho to Gauteng Province, the industrial region of South Africa. In addition, the hydroelectric scheme at Muela will supply enough electrical power to meet the needs of Lesotho. The project consists of a number of dams, reservoirs and tunnels, and a hydroelectric scheme which will be constructed in four phases. Construction operations, if the project runs to completion, will last until around 2020. Phase IA commenced in 1987 and consists of Katse Dam, a Transfer Tunnel from the impounded reservoir to the Muela Hydroelectric Power Station, the Muela Dam, and a Delivery Tunnel from the latter dam to the outfall on the Ash River, which is part of the Vaal River system. The tunnels total some 81 km in length. Except for the adits which were drilled and blasted, the tunnels were constructed by five tunnel boring machines. The Katse Dam and Transfer Tunnel were constructed in the basalts of the Drakensberg Formation. Many of these basalts have been subjected to deuteric alteration and consequently contain expansive clay minerals. Their presence can mean that the basalts disintegrate rapidly on exposure, which led to increased excavation at the dam site, and slabbing and spalling from the perimeter of the tunnel. The Muela Hydroelectric Power Station and Delivery Tunnel South were constructed primarily in sandstones of the Clarens Formation. These sandstones presented few problems during excavation and this tunnel was bored 20 months ahead of schedule. It was anticipated that the Delivery Tunnel North would be the most difficult to excavate as it runs through a succession of mudstones and sandstones. Hence, this tunnel was excavated by a double-shielded tunnel boring machine which could bore through varied ground and provide protection against rock fall, while simultaneously installing precast lining segments.

This record provided courtesy of AGI/GeoRef.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Association of Engineering Geologists