Mining Economy | CUET PG Geography | Notes

TOPIC INFOCUET PG (Geography)

SUB-TOPIC INFO  Economic Geography

CONTENT TYPE Detailed Notes

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1. Factors Governing the Exploitation of Mineral Resources

1.1. Geological Factors

1.2. Economic Factors

1.3. Technological Factors

1.4. Locational and Infrastructural Factors

1.5. Political, Legal, and Institutional Factors

1.6. Environmental Factors and Constraints

2. World Reserves and Production of Iron Ore, Manganese, Bauxite, and Copper

2.1. Iron Ore

2.2. Manganese

2.3. Bauxite (and Alumina)

2.4. Copper

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DETAILED NOTES CUET PG (GEOGRAPHY)

Mining Economy

CUET PG GEOGRAPHY

Economic Geography

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Factors Governing the Exploitation of Mineral Resources

  • The exploitation of mineral resources — the decision as to whether, when, and how a mineral deposit is actually extracted — depends on far more than the mere geological presence of the mineral in the ground. Mineral exploitation is governed by an interacting set of geological, economic, technological, locational, political, and environmental factors, and it is a central principle of resource geography that the mere existence of a mineral deposit does not automatically make it a usable, exploitable “resource” — a deposit only becomes an economically workable resource when a combination of favourable factors converts geological potential (reserve) into an actually extractable and marketable commodity.

Geological Factors

  • Grade (ore concentration/richness) of the deposit is the single most fundamental geological determinant of exploitability. Ores with a high mineral concentration require less rock to be processed per unit of extracted mineral, making extraction more economical, whereas low-grade ores, though sometimes present in vastly greater total quantity, require the processing of enormous volumes of rock to yield the same quantity of usable mineral, making extraction economically unviable unless prices are high or extraction technology has significantly improved (as has historically occurred with copper, where the average grade of ore considered economically workable has fallen dramatically over the twentieth century due to technological advances). Size and extent of the deposit (reserve size) matters because large deposits justify the substantial fixed capital investment required for mining infrastructure (shafts, processing plants, transport links) by allowing costs to be spread over a longer productive life and greater output volume, whereas small, isolated deposits often cannot justify this investment even if the ore grade is favourable.
  • The depth of occurrence of the deposit is critical, since minerals occurring near the surface can be extracted through comparatively cheap open-cast (surface) mining, while deeply buried deposits require expensive, technically demanding, and more hazardous underground (shaft) mining, substantially raising extraction costs and depth-related safety and ventilation challenges. The geological structure and associated impurities of a deposit also matter — a deposit that is structurally complex (faulted, folded, or intermixed with unwanted rock/gangue material) is costlier to mine and process than a simple, continuous, relatively pure seam or vein, and the presence of harmful associated impurities (such as sulfur in coal, which increases pollution control costs) can reduce a deposit’s commercial attractiveness even where the primary mineral content is substantial.

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