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

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Table 4.6: Mining operations in the Shashe (Botswana) sub-catchment. Code Number Name of Mine Commodity (ies) Mined ccxxviii Status Relative Size Probable Impact Bots-7 Matsitama Copper Operating Small Very low Bots-8 Tati Gold Operating Small Low–Medium (As) Bots-9 Selkirk Copper, Nickel Operating Small Low Table 4.7: Mining operations in the Shashe (Zimbabwe) Sub-catchment. Name Commodity Status Total produced /t Champion Arsenic Closed 1924 1022.7 High Hydra Arsenic Closed 1946 553.3 High Vubachikwe Arsenic Closed 1949 110.1 High Antelope Gold Closed 9.2 Medium Potential Impact Blanket Gold In operation 27.0 High: Arsenic possible Freda Gold In operation 10.5 High: Arsenic possible Horn Gold Dump retreatment 5.0 High: Arsenic & bismuth possible Vubachikwe Black Jack Gold In operation 25.1 High: Size & Arsenic possible Noel Nickel Closed 1963 4651.9 High: Arsenic possible Hampden Iron Pyrite Closed 1942 1492.0 High See ZGS (1988a) and ZGS (1988b) for locations. A copper smelter was operated at Valley, west of West Nicholson, during the first half of the twentieth century (Tyndale-Biscoe, 1940). In Zimbabwe, there is exploration for diamond, arsenic, nickel, gold, copper and lead (ZGS, 2001). 4.5.3 Alluvial mining Alluvial mining of gold takes place in the Thuli River in Zimbabwe (Figure 3.14; Chiyanike, 1997). There appears to be no alluvial mining taking place in the Botswana sector of the sub-catchment. 4.5.4 Monitoring systems ZINWA is currently setting one up and the Botswana Department of Water plans to expand its current monitoring programme.
4.5.5 Water quality data None available. 4.5.6 Implications for water quality and quantity management In Zimbabwe, the major impacts to be expected are from arseniferous gold and nickel mines and arsenic mines in the western Gwanda and the Lower Gwanda Greenstone Belt: acid mine drainage and release of toxic metals, such as arsenic and bismuth are possible. There are minor impacts from alluvial gold mining in the Thuli River. In Botswana, minor impacts are anticipated from arseniferous gold, nickel and copper mines, with minor acid mine drainage. 4.6 The Pazhi sub-catchment 4.6.1 General description 4.6.1.1 Hydrology This is Zone L1 of Area B (ZSG, 1984). The area consists of the catchments of several small rivers, which flow directly into the Limpopo. The two largest are the Pazhi and the Mutshilashokwe. 4.6.1.2 Geology Karoo basalts underlie most of the sub-catchment, whilst Limpopo Belt gneisses underlie the east (Figure 3.6; ZGS, 1999). 4.6.1.3 Pedology, agriculture and land use Soils in the sub-catchment can be divided into two groups: • Very shallow to moderately shallow sandy loams, formed from gneisses; and • Very shallow sands, derived from the basalts (DRSS, 1979). The sub-catchment is entirely in Natural Region V, with poor soils rainfall under 600mm and in places under 450mm (ZSG, 1997). Land use is mainly Communal Lands, with subsistence agriculture: mainly livestock production. The southeast corner is commercial farming land with livestock production. ccxxix
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AN OVERVIEW OF THE IMPACT OF MINING
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AN OVERVIEW OF THE IMPACT OF MINING
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exploited, the size of the facility
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2.3.6 Stockpiling and transport of
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4.1.6 Mining and mineral processing
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LIST OF FIGURES Figure 1.1: Compari
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Table 1.6: Minimum annual productio
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Table 3.26: Mining operations in th
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ACKNOWLEDGEMENTS Several enthusiast
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1. INTRODUCTION AND BACKGROUND INFO
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Box 1.2). Each research team is req
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The MRC cannot be held responsible
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of amenity or deterioration in wate
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Typically, river flows in the count
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In simple terms, all of the propone
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shared by more than one country, es
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most appropriate technical or inves
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CAMEROUN GABON CENTRAL AFRICAN REPU
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1.6.1 Data on the location, nature,
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1997). In future studies, more atte
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Section 5 briefly reviews the water
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Mining methods vary widely and depe
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Removal and storage of ores and was
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These effects are usually ameliorat
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Water quality changes are widely co
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these substances are often mobilize
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The acidification of the water has
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and kinetic stability of the comple
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This process is carefully balanced
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neutralize each other - this situat
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(Chenje, 2000). Despite the recent
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Swaziland Water Environment Tanzani
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Draft Environmental Management Bill
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siting of works plan for approval t
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The draft policy encourages develop
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provides a definition but one which
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2.9.3.9 Zimbabwe Environmental Impa
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Sector Activity Industry °Chemical
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Cyanides and related compounds (CN)
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of Natural Resources and the South
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3.1.1 Geology, topography and soils
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Air temperatures across the Zambezi
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or fuelwood production. Similar pat
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Zambia. Clearly, some water quality
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3.2.1.6 Human impacts on water reso
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The Botswana segment of this area f
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3.4.1.4 Surface water users The onl
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3.5.1.2 Geology The Upper Karoo Bat
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3.5.6 Implications for water qualit
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3.6.4 Monitoring systems None. 3.6.
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3.7.2 Mining and mineral processing
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3.8.1.5 Water management systems Th
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3.9.1.2 Geology This sub-catchment
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3.9.5 Water quality data None avail
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Z-87 Mulobezi Amethyst Operating Ve
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3.11.1.6 Human impacts on water res
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3.12.1.2 Geology This sub-catchment
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• Increased quantities of suspend
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Determinant Fischer’s Farm Raglan
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3.13.1.4 Surface water users There
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The Nampundwe pyrite mine poses a r
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Z-90 Chisuki Mica, Tin, Tantalite O
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along the major roads between Chiru
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3.16.1 General description 3.16.1.1
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Z-17 Jessie Gold Starting Very Smal
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Small intrusions of Greenstone form
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Several stretches of streams and ri
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3.18.1.5 Water management systems T
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3.18.6 Implications for water quali
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3.20 The Mazowe (Mozambique) sub-ca
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3.20.4 Monitoring systems This area
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The only settlements of any size ar
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3.23.1 General description 3.23.1.1
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3.23.4 Monitoring systems None. 3.2
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• Non-point impact from minefield
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This is Zones G1-G6, B1-B3, S1-S6,
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The catchment falls mainly under th
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The two lone water quality data poi
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• Non-point domestic effluent, ru
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Land use comprises the Siabuwa, Oma
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3.28 The Ume sub-catchment 3.28.1 G
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3.28.4 Monitoring systems None. 3.2
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3.29.1.4 Surface water users The Ci
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Thristle Etna Gold 6.7 Medium Tiger
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Sanyati, all may well contribute or
Page 177 and 178: 3.30.1.5 Water management systems T
Page 179 and 180: This is Zone Z1 of Area C (ZSG, 198
Page 181 and 182: 3.31.5 Water quality data Only one
Page 183 and 184: 3.32.2 Mining and mineral processin
Page 185 and 186: Land use above the Zambezi Escarpme
Page 187 and 188: Extensive alluvial mining of gold t
Page 189 and 190: The major settlements are the metro
Page 191 and 192: 3.34.6 Implications for water quali
Page 193 and 194: • Urban run off, urban areas of C
Page 195 and 196: 3.36.1.4 Surface water users The to
Page 197 and 198: 3.37.1.1 Hydrology This is Zones M1
Page 199 and 200: The catchment falls under the Harar
Page 201 and 202: 3.37.3 Alluvial mining Alluvial min
Page 203 and 204: widely intruded by Mashonaland Dole
Page 205 and 206: 3.38.4 Monitoring systems ZINWA is
Page 209 and 210: 4. THE LIMPOPO BASIN In order to pr
Page 211 and 212: Mountains. Most of the basin consis
Page 213 and 214: the City of Pretoria and the northe
Page 215 and 216: continues to flow in the deeper all
Page 217 and 218: Each basin state maintains its own
Page 219 and 220: Land use in the upper parts of the
Page 221 and 222: the Limpopo River some 100 kilometr
Page 223 and 224: None obtainable in time for this re
Page 225 and 226: 4.4.2 Mining and mineral processing
Page 227: In the Botswana sector of the sub-c
Page 231 and 232: 4.6.5 Water quality data None avail
Page 233 and 234: Table 4.9: Mining operations in the
Page 235 and 236: 4.7.4 Monitoring systems ZINWA is c
Page 237 and 238: There is exploration for diamonds (
Page 239 and 240: There is exploration, mainly for di
Page 243 and 244: Hwange National Park (ZSG, 1998). A
Page 245 and 246: 4.12.1.3 Pedology, agriculture and
Page 247 and 248: 4.13 The Marico sub-catchment 4.13.
Page 249 and 250: • Major non-point impact of agric
Page 251 and 252: Several thermal springs are located
Page 253 and 254: • Disposal of large volumes of li
Page 255 and 256: D7-13 Premier Diamond - kimberlite
Page 257 and 258: 4.15.1 General description 4.15.1.1
Page 261 and 262: Most of the clayey loam soils in th
Page 263 and 264: 4.17 The Theuniskloof sub-catchment
Page 265 and 266: 4.17.4 Monitoring systems The Depar
Page 267 and 268: 4.18.1.4 Surface water users All of
Page 269 and 270: Water quality data for three sites
Page 271 and 272: supplies in the sub-catchment, the
Page 273 and 274: 4.20.1.2 Geology Like the Mogalakwe
Page 275 and 276: • Minor non-point impact from non
Page 277 and 278: 4.21 The Nzhelele sub-catchment 4.2
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4.22.1.3 Pedology, agriculture and
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Code Number Name of Mine Commodity
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5. THE OLIFANTS CATCHMENT In order
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Soil formations across the Olifants
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indices of per capita agricultural
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professional capacity within the me
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• Dark grey to blackish, mottled
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5.2.5 Water quality data No specifi
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Several towns (e.g. Witbank and Mid
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The following mining operations are
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5.3.6 Implications for water qualit
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5.4.1.3 Pedology, agriculture and l
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K 5.5 5 4.5 Cl 380 350 200 F 1.0 1.
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local geological formations. High c
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The South African Department of Wat
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pH 8.5 8.3 8.8 8.7 8.8 8.9 TDS 439
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Soils in the sub-catchment can be d
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No information is available on the
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In its upper reaches, the sub-catch
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The Phalaborwa Water Board has been
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m 3 /day) water abstractions, and m
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In the south-west of the sub-catchm
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• Minor non-point impact of agric
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(Figure 4.2). The tributaries of th
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5.9.1.6 Human impacts on water reso
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y the upper Klaserie River. Recent
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5.10.6 Implications for water quali
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In Mozambique, the Mozambican Depar
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Acid mine drainage (AMD) represents
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• Antimony, cadmium and tin conta
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• Decreased light penetration to
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6.1.8 “Peripheral” or indirect
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Worldwide, the general public has e
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2. That copies of this report shoul
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Banks, D., P.L. Younger, R.T. Arnes
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CSIR (1993). An Environmental Impac
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Fuggle, R.F. & M.A. Rabie (1996). E
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Love, D. & D.K. Hallbauer (2000). M
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Pettersson, U.T. & J. Ingri (2000b)
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Turton, A.R. (1999b). Water scarcit
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World Bank (1998). World Developmen
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