- (a). coal
- (b). bauxite
- (c). gold
- (d). zinc
Bauxite forms through surface weathering and decomposition that removes soluble material and leaves an aluminium-rich residue.
(b) bauxite
- (a). bauxite
- (b). mica
- (c). iron ore
- (d). copper
The Koderma-Gaya-Hazaribagh belt is a major mica-producing region.
(b) mica
- (a). sedimentary rocks
- (b). metamorphic rocks
- (c). igneous rocks
- (d). none of the above
Coal, some iron ore, gypsum, potash and salt occur in beds or layers of sedimentary rocks.
(a) sedimentary rocks
- (a). oil
- (b). uranium
- (c). thorium
- (d). coal
Monazite sands in Kerala contain thorium used for atomic energy.
(c) thorium
Uses the chapter’s classification of minerals and energy sources.
(a) Ferrous minerals contain iron, such as iron ore and manganese; non-ferrous minerals do not, such as copper, bauxite and lead. (b) Conventional sources such as coal, petroleum and firewood have long been widely used; non-conventional sources such as solar, wind, tidal and biogas are newer, generally renewable alternatives.
Definition follows geographers’ description in the opening section.
A mineral is a homogeneous, naturally occurring substance with a definite internal structure. It has a characteristic chemical composition and physical properties formed through geological processes.
Grounded in the description of veins and lodes.
Minerals occur in cracks, faults and joints. Molten or gaseous mineral material is forced upward through cavities, cools and solidifies, forming small veins or larger lodes.
Grounded in the mineral-conservation section.
Minerals are finite and take millions of years to form, while extraction and consumption are rapid. Conservation reduces depletion, environmental damage and future scarcity through efficient use, recycling and substitutes.
Grounded in the coal distribution subsection.
India’s coal occurs mainly in two geological ages. Gondwana coal, about 200 million years old, supplies most production and lies chiefly in peninsular river valleys. Major fields include Jharia, Raniganj and Bokaro in the Damodar valley; deposits also occur in the Godavari, Mahanadi, Son and Wardha valleys. Tertiary coal, about 55 million years old, occurs in the north-eastern states of Meghalaya, Assam, Arunachal Pradesh and Nagaland. Lignite, a low-grade brown coal, is found at Neyveli in Tamil Nadu and in parts of Rajasthan and Gujarat. The location of these deposits strongly influences thermal power and heavy industry.
Grounded in the solar-energy passage and its rural-development benefits.
India is tropical and receives abundant sunshine over most of the year, giving solar power a large geographical base. Solar photovoltaic systems can serve dispersed villages and remote areas without expensive grid extension, reducing dependence on firewood and dung cakes and improving rural life. The resource is renewable and produces electricity without the air pollution and greenhouse emissions of fossil fuels. Falling technology costs and uses ranging from lighting and pumps to cooking and industry increase its practicality. Solar development also reduces imported fuel dependence and conserves coal and petroleum. Storage, grid integration and initial cost remain challenges, but the scale and regularity of sunlight make the long-term potential strong.