Geology of the Kamo Mine area

environmental effects of gol-e-gohar iron ore mine on groundwater of the area

gol-e-gohar iron ore mine of sirjan in southern part of iran is a large open pit that operates below the groundwater table and during mining operation, dewatering is required to prevent operation processes from flooding. current operation is going on by digging wells in or out of the pit and pumping to prevent flooding. as a result of the former dewatering operation a vast deep cone of depressi...

Surficial Geology of the Swan River Area

Geology of the Tagish Lake Area

ACCESS AND PHY SIOGRAPIHY Large lakes at elevations ranging from 656 to 844 re t res provide boat access to about 30 per cent of the map area. These lakes are most easily reached by floatplane or hslicopter, both stationed in Atlin some 40 kilometres to the east. During high water (earl) July through to late Septenber) Tagish Lake can also he reached from Atlin by powerbolt via the Atlin River....

Preliminary Geology and Mineral Potential of the Cascade Recreation Area

The C;~scade Rrcreation Area wi,\ created in 1YX7 to preserve wilderness and heritage recreation opportunities in I67 quxc kilomctres of the northern Cascade Mountain\. The area encompxses the headuatcrs of the Tulamecn. Snnss and Skaist rivers in the Ho~amccn Range\. 10 kilometres southeast of Hope and is hordcred by Manning Provincial Park on the southeast and Skagit Valley Recreation Arca on...

Geology and Mineral Occurrences of the Yalakom River Area*

(Glover et al . , 1988a, 1988b) and 1988 (Schiarizza et a l . , 1989d, 1989b). and extends the mapping eastward to include the eastem part of the Shulaps Range, the Yalakom and Bridge River valleys and the adjacent Camelsfoot Range. In addition, several weeks were spent re-examining critical areas in the Tyaughton Creek area and traversing the area south of Gun Creek in an effort to mesh our ...