OR/15/033 Summary: Difference between revisions
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The underground geological mapping undertaken in Carrock Mine have confirmed the results of previous work published by Moore (1977) and extended the coverage into the levels that were driven after this work was published. The analysis of the samples collected during this study has highlighted that all the waters sampled have arsenic levels above WHO guideline values. | The underground geological mapping undertaken in Carrock Mine have confirmed the results of previous work published by Moore (1977)<ref name="Moore">MOORE, J McM. 1977. Carrock Fell Tungsten Mine, Cumbria; ''Royal School of Mines Journal'' 1977; pp 7–14. </ref> and extended the coverage into the levels that were driven after this work was published. The analysis of the samples collected during this study has highlighted that all the waters sampled have arsenic levels above WHO guideline values. | ||
Samples of host rocks, the later lead veins and the tailings collected during the field work are stored at the British Geological Survey and remain available for detailed study. | Samples of host rocks, the later lead veins and the tailings collected during the field work are stored at the British Geological Survey and remain available for detailed study. | ||
==Reference== | |||
[[category:OR/15/033 The Underground Geology of part of the Carrock Tungsten Mine, Caldbeck Fells | 07]] | [[category:OR/15/033 The Underground Geology of part of the Carrock Tungsten Mine, Caldbeck Fells | 07]] |
Latest revision as of 14:24, 28 July 2015
Shaw, R P. 2015. The Underground Geology of part of the Carrock Tungsten Mine, Caldbeck Fells. British Geological Survey Internal Report, OR/15/033. |
The underground geological mapping undertaken in Carrock Mine have confirmed the results of previous work published by Moore (1977)[1] and extended the coverage into the levels that were driven after this work was published. The analysis of the samples collected during this study has highlighted that all the waters sampled have arsenic levels above WHO guideline values.
Samples of host rocks, the later lead veins and the tailings collected during the field work are stored at the British Geological Survey and remain available for detailed study.
Reference
- ↑ MOORE, J McM. 1977. Carrock Fell Tungsten Mine, Cumbria; Royal School of Mines Journal 1977; pp 7–14.