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Minerals and Energy Resources

What minerals are and where they occur

Explain what minerals are and how they occur.

Minerals are everywhere. From a tiny pin to a tall building or a big ship, almost everything we use is made from minerals: railway lines, roads, machines, cars, buses and aeroplanes. Your toothpaste is full of them: silica and limestone scrub the teeth, fluoride (from the mineral fluorite) fights cavities, titanium oxide makes it white, and mica makes it sparkle. Even our food has minerals: only about 0.3 per cent of what we eat, but without them our body could not use the other 99.7 per cent.

Haban's question. Haban comes from a remote village to Guwahati and sees 'houses' moving on the road. His father explains: these are buses and trains, made of metals like iron and aluminium, and they move because an engine uses energy. Metals and energy both come from the earth.

What is a mineral? Geologists call it a 'homogenous, naturally occurring substance with a definable internal structure'. Homogenous means it is the same all through, like a roti, not like a pizza with different toppings in different places. Some are very hard, like diamond; some are very soft, like talc. Rocks are made of minerals: limestone has just one, most rocks have several. Over 2000 minerals are known.

What is an ore? An ore is a mass of a mineral mixed with other things, with enough of the mineral to make digging it out profitable. Simple test: can you take the metal out and still make money? Then it is an ore. Whether a deposit becomes a mine depends on how rich the ore is, how easy it is to dig, and how close it is to the market.

Five places minerals are found.

  • Veins and lodes (cracks in igneous and metamorphic rocks): hot liquid and gas rise, cool and harden. Small ones are veins, big ones lodes. Tin, copper, zinc, lead.
  • Beds or layers in sedimentary rocks: coal, some iron ore; and gypsum, potash salt, sodium salt left behind when water evaporates in dry areas.
  • Left-over (residual) mass: surface rocks break down, the parts that dissolve are washed away, and the ore stays behind. Bauxite forms this way.
  • Placer deposits: in the sands of valley floors and at the foot of hills. These minerals do not corrode in water: gold, silver, tin, platinum.
  • Oceans: common salt, magnesium, bromine from sea water, and manganese nodules on the sea bed.

Rat-hole mining. Most minerals in India belong to the nation and need government permission to mine. But in many tribal areas of the north-east, minerals belong to individuals or communities. In Meghalaya (Jowai and Cherrapunjee), families dug coal through long, narrow tunnels: 'rat-hole' mining, which is dangerous (roofs fall, water floods in). The National Green Tribunal has declared it illegal.

A mineral is natural and the same all through; an ore has enough of it to be worth mining.

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