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

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

There is some evidence to suggest that the Moatize Coal Mine may have had a minor-medium impact on local<br />

water quality whilst other mining operations are likely to have had small, localized impacts at most. The artisan<br />

gold diggings have contributed to a considerable increase in the suspended sediment load of the Zambezi River<br />

during periods of low flow. The Matangua uranium and thorium deposit holds the risk of contaminating local<br />

water supplies.<br />

3.19 The Shire (Malawi) sub-catchment (including Tanzania)<br />

3.19.1 General description<br />

3.19.1.1 Hydrology<br />

This area comprises one large sub-catchment containing the Lake Malawi and its outflow, the Shire River, with<br />

a series of smaller streams and rivers that drain into Lake Malawi from the Malawi and Tanzanian portions of<br />

the rift valley.<br />

In the Tanzanian sector, the most import inflow is the Ruhuhu River, with smaller rivers draining the Livingstone<br />

Mountains and entering Lake Malawi at Songwe. All of these rivers are short, with steep gradients and carry<br />

large volumes of water since they drain areas that receive annual rainfalls in excess of 2,000 mm.<br />

Lake Malawi also receives inflows from several smaller perennial streams and rivers that drain the Rift Valley<br />

and flow into the lake. Outflows from Lake Malawi flow down the Shire River to the Zambezi River.<br />

The Shire River is perennial, though flows have declined in recent years due to a drop in the water level of Lake<br />

Malawi. The lower portion of the Lake Malawi Rift Valley lies in a partial rain shadow that reduces rainfall from<br />

the southeasterly winds, and annual rainfalls average some 850 mm. Slightly further south, the Mulanje Plateau<br />

receives over 2,500 mm of rainfall and provides strong inflows into the Shire River.<br />

All of the smaller, perennial and non-perennial streams that drain the Rift Valley into Lake Malawi have steep<br />

gradients and have incised deeply into the country rock.<br />

3.19.1.2 Geology<br />

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