Kalimashi 1 mine
| Location | |
|---|---|
  Kalimashi 1 mine Location in Albania | |
| Location | Kukës |
| Kukës District | Kukës County |
| Country | Albania |
| Coordinates | 42°14′N 20°06′E / 42.24°N 20.1°ECoordinates: 42°14′N 20°06′E / 42.24°N 20.1°E |
| Production | |
| Products | Chromium |
| History | |
| Opened | 1978 |
| Closed | 2000 |
| Owner | |
The Kalimashi 1 mine is a large mine located in northern Albania in Kukës County, 80 kilometres (50 mi) north-east of the capital, Tirana. Kalimashi 1 represents the fourth largest chromium reserve in Albania and one of the largest in Europe having estimated reserves of 1.9 million tonnes of ore grading 20% chromium metal.[1] The mine is part of the Kukës Massif, a 108 square kilometres (42 sq mi) area which has a rock thickness between 4 kilometres (2.5 mi) and 6 kilometres (3.7 mi) and contains 54 verified chromium deposits and occurrences.[1] The deposit has been explored to depths of up to 300 metres (980 ft) and the geological reserves amount to 6.8 million tonnes grading 21.4% chromium metal.[1]
The Kalimashi 1 mine began operating in 1978. The total combined chromium ore production from the mine between 1986 and 1998 amounted to 860,000 tonnes.[1] The deepest level of the mine is the + 600 Level which reaches a depth of 300 metres (980 ft). The chromium ore reserves of the mine are split into two categories above and below + 600 Level. The proven ore reserves located above the + 600 Level amount to 1,900,000 tonnes of ore grading 20% chromium metal.[1] The proven ore reserves located below the + 600 Level are currently not estimated or calculated but are expected to be grading over 30% chromium metal.[1] The mine's total reserves amount to 1.9 million tonnes of ore grading 20% chromium metal.[1] The chromium ore exploitation complex is located completlely underground and has been shut down since 2000 due to financial difficulties. The Kalimashi 1 mine is one of the eight Albanian chromium mines to have reserves of over 1 million tonnes of chromium ore.[1]
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