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OVERVIEW OF THE IMPACT OF MINING ON THE ... - IIED pubs

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None available.<br />

3.166 Implications for water quality and quantity management<br />

There is some evidence to suggest that the mining operations at Kabwe have had adverse effects on the local<br />

environment. Large (but localized) areas are denuded of vegetation as a result of atmospheric pollution from<br />

the smelter and seepage from the waste dumps.<br />

3.17 The Luangwa sub-catchment<br />

3.17.1 General description<br />

3.17.1.1 Hydrology<br />

This area comprises one large sub-catchment containing the Luangwa River, with a series of smaller streams<br />

and rivers that drain into the Luangwa. The Luangwa River flows in a south-southwesterly direction, draining<br />

the Luangwa Rift Valley and also receiving flows from the Mulungushi sub-catchment before swinging<br />

southwards to join the Zambezi River at the town of Feira on the Mozambique border.<br />

The Luangwa River is perennial, though dry season flows are barely discernable. The Luangwa Rift Valley lies<br />

in a rain shadow that reduces rainfall from the southeasterly winds, and annual rainfalls average some 750 mm.<br />

The Luangwa River meanders across a broad floodplain, leaving many isolated oxbow lakes and lagoons. The<br />

central portion of the Luangwa Valley contains the Luangwa North and Luangwa South National parks.<br />

The smaller, perennial and non-perennial streams that drain the Muchinga Escarpment to the west and the<br />

Nyika and Viphya Plateaux to the east have steep gradients and have incised deeply into the country rock.<br />

3.17.1.2 Geology<br />

The plateaux on both sides of the Luangwa Rift Valley are composed of quartzites, sandstones, granites and<br />

gneisses, underlain by sedimentary rocks with coal measures to the east. These rock formations are intruded<br />

by numerous small pegmatites that are host to a variety of high-quality semi-precious stone deposits (amethyst,<br />

garnet, aquamarine).<br />

cxxxii

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