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A mineral is a naturally occurring homogeneous substance with a definable internal structure.
Rocks are combinations of minerals.
Minerals vary because they form through different geological processes and under different conditions.
A mineral becomes an ore when its concentration is sufficient for commercial extraction and processing.
Economically viable percentage = (50/80) × 100 = 62.5%.
Veins and lodes occur in cracks, crevices, faults and joints of igneous and metamorphic rocks.
Coal and some forms of iron ore occur in layers or beds in sedimentary rocks.
Bauxite forms through the decomposition of rocks and removal of soluble constituents.
Placer deposits commonly contain valuable minerals such as gold, silver, tin and platinum.
Ocean waters provide common salt, magnesium and bromine, while ocean beds contain manganese nodules.
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