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Class 10 Social Science · Geography Chapter 5 of 7

Chapter 5 — Minerals And Energy Resources

Overview

Minerals and Energy Resources studies the material base of industry. A mineral is defined as a homogeneous, naturally occurring substance with a definable internal structure, and the chapter begins with where minerals are found: in veins and lodes within igneous and metamorphic rocks, in beds and layers within sedimentary rocks, as residual masses left by the decomposition of surface rocks, as alluvial or placer deposits in the sands of valley floors, and dissolved in ocean water. It then surveys India's minerals in the standard order. Ferrous minerals - iron ore, of which magnetite is the finest with about 70 per cent iron and haematite the most important industrially, distributed across four great belts from Odisha-Jharkhand to Maharashtra-Goa, and manganese, used in making steel and bleaching powder. Non-ferrous minerals - copper, malleable, ductile and a good conductor, and bauxite, the ore from which aluminium is obtained, itself a residual deposit. Non-metallic minerals - mica, with its excellent di-electric strength and low power loss factor, and limestone, the basic raw material for cement. The chapter is candid about the human cost, listing the hazards miners face, and about the fact that mineral resources are finite and non-renewable, so that conservation is not optional. Its second half turns to energy, dividing conventional sources - firewood, cattle dung cake, coal, petroleum, natural gas and electricity - from non-conventional ones - solar, wind, tidal, geothermal, biogas and atomic energy - and ends by insisting that a sustainable path requires using energy sparingly as well as developing new sources.

Learning Objectives

  • Define a mineral and describe the different modes in which minerals occur.
  • Distinguish between ferrous and non-ferrous minerals with examples.
  • Describe the types of iron ore and identify the four major iron ore belts of India.
  • Describe the occurrence and uses of manganese, copper and bauxite.
  • Describe the properties, uses and distribution of mica and limestone.
  • Explain the hazards faced by miners and the environmental effects of mining.
  • Explain why the conservation of minerals is necessary and state the measures for it.
  • Distinguish conventional from non-conventional sources of energy.
  • Describe the types of coal and the two main coal-bearing formations of India.
  • Describe the distribution of petroleum and natural gas in India.
  • Distinguish hydro from thermal electricity and describe the non-conventional sources being developed.
  • Suggest measures for the conservation of energy resources.

Topics in this chapter

6 topics · tap a topic title to jump straight to it.

🌍1

What is a Mineral and How Minerals Occur

The definition

Geologists define mineral as a homogenous, naturally occurring substance with a definable internal structure. Minerals are found in varied forms in nature, ranging from the hardest diamond to the softest talc.

Rocks are combinations of homogeneous substances called minerals. Some rocks, for instance limestone, consist of a single mineral only, but majority of the rock consist of several minerals in varying proportions. Although over 2000 minerals have been identified, only a few are abundantly found in most of the rocks.

Veins and lodes

Minerals generally occur in these forms. In igneous and metamorphic rocks minerals may occur in the cracks, crevices, faults or joints. The smaller occurrences are called veins and the larger are called lodes. In most cases, they are formed when minerals in liquid or molten and gaseous forms are forced upward through cavities towards the earth's surface. They cool and solidify as they rise. Major metallic minerals like tin, copper, zinc and lead etc. are obtained from veins and lodes.

Beds and layers

In sedimentary rocks a number of minerals occur in beds or layers. They have been formed as a result of deposition, accumulation and concentration in horizontal strata. Coal and some forms of iron ore have been concentrated as a result of long periods under great heat and pressure. Another group of sedimentary minerals include gypsum, potash salt and sodium salt. These are formed as a result of evaporation especially in arid regions.

Residual mass

Another mode of formation involves the decomposition of surface rocks, and the removal of soluble constituents, leaving a residual mass of weathered material containing ores. Bauxite is formed this way.

Placer deposits and ocean water

Certain minerals may occur as alluvial deposits in sands of valley floors and the base of hills. These deposits are called placer deposits and generally contain minerals, which are not corroded by water. Gold, silver, tin and platinum are most important among such minerals.

The ocean waters contain vast quantities of minerals, but most of these are too widely diffused to be of economic significance. However, common salt, magnesium and bromine are largely derived from ocean waters. The ocean beds, too, are rich in manganese nodules.

📌 Examples
  • Veins are the smaller occurrences in cracks and joints; lodes are the larger ones - the source of tin, copper, zinc and lead.
  • Placer deposits form in valley sands and contain minerals not corroded by water: gold, silver, tin, platinum.
  • Bauxite is a residual mass, left after soluble constituents are removed by the decomposition of surface rocks.
🌍2

Ferrous Minerals: Iron Ore and Manganese

Iron ore

Iron ore is the basic mineral and the backbone of industrial development. India is endowed with fairly abundant resources of iron ore. It has the largest reserve of iron ore in Asia.

The two important varieties are:

  • Magnetite is the finest iron ore with a very high content of iron up to 70 per cent. It has excellent magnetic qualities, especially valuable in the electrical industry.
  • Haematite ore is the most important industrial iron ore in terms of the quantity used, but has a slightly lower iron content than magnetite (50-60 per cent).

The four major belts

  1. Odisha-Jharkhand belt: In Odisha high grade haematite ore is found in Badampahar mines in the Mayurbhanj and Kendujhar districts. In the adjoining Singhbhum district of Jharkhand haematite iron ore is mined in Gua and Noamundi.
  2. Durg-Bastar-Chandrapur belt lies in Chhattisgarh and Maharashtra. Very high grade haematites are found in the famous Bailadila range of hills in the Bastar district of Chhattisgarh. The range of hills comprise of 14 deposits of super high grade haematite iron ore. It has the best physical properties needed for steel making. Iron ore from these mines is exported to Japan and South Korea via Vishakhapatnam port.
  3. Bellary-Chitradurga-Chikkamagaluru-Tumakuru belt in Karnataka has large reserves of iron ore. The Kudremukh mines located in the Western Ghats of Karnataka are a 100 per cent export unit. Kudremukh deposits are known to be one of the largest in the world. The ore is transported as slurry through a pipeline to a port near Mangaluru.
  4. Maharashtra-Goa belt includes the state of Goa and Ratnagiri district of Maharashtra. Though, the ores are not of very high quality, yet they are efficiently exploited. Iron ore is exported through Marmagao port.

Manganese

Manganese is mainly used in the manufacturing of steel and ferro-manganese alloy. Nearly 10 kg of manganese is required to manufacture one tonne of steel. It is also used in manufacturing bleaching powder, insecticides and paints.

📌 Examples
  • Magnetite: up to 70% iron, with excellent magnetic qualities valuable to the electrical industry.
  • Haematite: 50-60% iron, but the most important industrial ore by quantity used.
  • Nearly 10 kg of manganese is required to manufacture one tonne of steel.
📊 Visual ideas
Map - India's four major iron ore belts: Odisha-Jharkhand, Durg-Bastar-Chandrapur, Bellary-Chitradurga-Chikkamagaluru-Tumakuru, and Maharashtra-Goa, with the export ports of Vishakhapatnam, Mangaluru and Marmagao.
🌍3

Non-Ferrous and Non-Metallic Minerals

Copper

India is critically deficient in the reserve and production of copper. Being malleable, ductile and a good conductor, copper is mainly used in electrical cables, electronics and chemical industries.

The Balaghat mines in Madhya Pradesh produce 52 per cent of India's copper. The Khetri mines in Rajasthan and Singhbhum district of Jharkhand are also leading producers of copper.

Bauxite

Though, several ores contain aluminium, it is from bauxite, a clay-like substance that alumina and later aluminium is obtained. Bauxite deposits are formed by the decomposition of a wide variety of rocks rich in aluminium silicates.

Aluminium is an important metal because it combines the strength of metals such as iron, with extreme lightness and also with good conductivity and great malleability.

India's bauxite deposits are mainly found in the Amarkantak plateau, Maikal hills and the plateau region of Bilaspur-Katni. Odisha is the largest bauxite producing state in India. Panchpatmali deposits in Koraput district are the most important bauxite deposits in the state.

Mica

Mica is a mineral made up of a series of plates or leaves. It splits easily into thin sheets. These sheets can be so thin that a thousand can be layered into a mica sheet of a few centimetres high. Mica can be clear, black, green, red, yellow or brown.

Due to its excellent di-electric strength, low power loss factor, insulating properties and resistance to high voltage, mica is one of the most indispensable minerals used in electric and electronic industries.

Mica deposits are found in the northern edge of the Chota Nagpur plateau. Koderma-Gaya-Hazaribagh belt of Jharkhand is the leading producer. In Rajasthan the major mica producing area is around Ajmer. Nellore mica belt of Andhra Pradesh and Telangana is also an important producer in the country.

Limestone

Limestone is found in association with rocks composed of calcium carbonates or calcium and magnesium carbonates. It is found in sedimentary rocks of most geological formations.

Limestone is the basic raw material for the cement industry and essential for smelting iron ore in the blast furnace.

📌 Examples
  • Copper is malleable, ductile and a good conductor, used in electrical cables, electronics and chemical industries.
  • Aluminium combines the strength of iron with extreme lightness, good conductivity and great malleability.
  • Mica's excellent di-electric strength, low power loss factor and resistance to high voltage make it indispensable in electronics.
🌍4

Hazards of Mining and Conservation of Minerals

The human cost

Mining is a killer industry. The dust and noxious fumes inhaled by miners make them vulnerable to pulmonary diseases. The risk of collapsing mine roofs, inundation and fires in coalmines are a constant threat to miners.

The environmental cost

The water sources in the region get contaminated due to mining. Dumping of waste and slurry leads to degradation of land, soil, and increase in stream and river pollution.

Why conservation is necessary

The total volume of workable mineral deposits is an insignificant fraction i.e. one per cent of the earth's crust. We are rapidly consuming mineral resources that required millions of years to be created and concentrated.

The geological processes of mineral formation are so slow that the rates of replenishment are infinitely small in comparison to the present rates of consumption. Mineral resources are, therefore, finite and non-renewable.

Rich mineral deposits are our country's most valuable but short-lived possessions. Continued extraction of ores leads to increasing costs as mineral extraction comes from greater depths along with decrease in quality.

Measures of conservation

  • A concerted effort has to be made in order to use our mineral resources in a planned and sustainable manner.
  • Improved technologies need to be constantly evolved to allow use of low grade ores at low costs.
  • Recycling of metals, using scrap metals and other substitutes.
  • Technology should be evolved to use scrap metals and other substitutes.
📌 Examples
  • Workable mineral deposits are about one per cent of the earth's crust.
  • Miners face pulmonary disease from dust and fumes, and the constant threat of roof collapse, inundation and fire.
  • Conservation measures: planned use, technology for low-grade ores, recycling of metals and use of scrap and substitutes.
🌍5

Conventional Energy: Coal, Petroleum and Natural Gas

Coal and its stages

In India, coal is the most abundantly available fossil fuel. It provides a substantial part of the nation's energy needs. It is used for power generation, to supply energy to industry as well as for domestic needs.

Coal is formed due to the compression of plant material over millions of years. Coal, therefore, is found in a variety of forms depending on the degrees of compression and the depth and time of burial.

  • Peat - decaying plants in swamps produce peat, which has a low carbon and high moisture contents and low heating capacity.
  • Lignite is a low grade brown coal, which is soft with high moisture content. The principal lignite reserves are in Neyveli in Tamil Nadu and are used for generation of electricity.
  • Bituminous coal is buried deep and subjected to increased temperatures. It is the most popular coal in commercial use. Metallurgical coal is high grade bituminous coal which has a special value for smelting iron in blast furnaces.
  • Anthracite is the highest quality hard coal.

Where coal is found

In India coal occurs in rock series of two main geological ages, namely Gondwana, a little over 200 million years in age and in tertiary deposits which are only about 55 million years old.

The major resources of Gondwana coal, which are metallurgical coal, are located in Damodar valley (West Bengal-Jharkhand). Jharia, Raniganj, Bokaro are important coalfields. The Godavari, Mahanadi, Son and Wardha valleys also contain coal deposits. Tertiary coals occur in the north eastern states of Meghalaya, Assam, Arunachal Pradesh and Nagaland.

Petroleum

Petroleum is the next major energy source in India after coal. It provides fuel for heat and lighting, lubricants for machinery and raw materials for a number of manufacturing industries. Petroleum refineries act as a 'nodal industry' for synthetic textile, fertiliser and numerous chemical industries.

Most of the petroleum occurrences in India are associated with anticlines and fault traps in the rock formations of the tertiary age. In regions of folding, anticlines or domes, it occurs where oil is trapped in the crest of the upfold. The oil bearing layer is a porous limestone or sandstone through which oil may flow. The oil is prevented from rising or sinking by intervening non-porous layers. Petroleum is also found in fault traps between porous and non-porous rocks. Gas, being lighter usually occurs above the oil.

Mumbai High is the largest producer, followed by Gujarat and Assam. Ankaleshwar is the most important field of Gujarat. Assam is the oldest oil producing state of India. Digboi, Naharkatiya and Moran-Hugrijan are the important oil fields in the state.

Natural gas

Natural gas is an important clean energy resource found in association with or without petroleum. It is used as a source of energy as well as an industrial raw material in the petrochemical industry. Natural gas is considered an environment friendly fuel because of low carbon dioxide emissions and is therefore, the fuel for the present century.

Large reserves of natural gas have been discovered in the Krishna-Godavari basin. Along the west coast the reserves of the Mumbai High and allied fields are supplemented by finds in the Gulf of Cambay. Andaman and Nicobar islands are also important areas having large reserves of natural gas.

The 1700 km long Hazira-Vijaipur-Jagdishpur cross country gas pipeline links Mumbai High and Bassein with the fertiliser, power and industrial complexes in western and northern India.

📌 Examples
  • Coal stages: peat, lignite, bituminous, anthracite - in order of increasing carbon and heating capacity.
  • Gondwana coal, over 200 million years old, lies in the Damodar valley - Jharia, Raniganj, Bokaro.
  • Gas, being lighter, usually occurs above the oil in an anticline or fault trap.
🌍6

Electricity and Non-Conventional Sources

Two ways of generating electricity

Electricity has such a wide range of applications in today's world that, its per capita consumption is considered as an index of development. Electricity is generated mainly in two ways:

  • By running water which drives hydro turbines to generate hydro electricity.
  • By burning other fuels such as coal, petroleum and natural gas to drive turbines to produce thermal power.

Once generated the electricity is exactly the same. But the two sources differ completely in that hydro electricity uses a renewable resource that is not consumed, while thermal power uses exhaustible fossil fuels and emits carbon.

Nuclear or atomic energy

Nuclear energy is obtained by altering the structure of atoms. When such an alteration is made, much energy is released in the form of heat and this is used to generate electric power. Uranium and Thorium, which are available in Jharkhand and the Aravalli ranges of Rajasthan are used for generating atomic or nuclear power. The Monazite sands of Kerala is also rich in Thorium.

Solar energy

India is a tropical country. It has enormous possibilities of tapping solar energy. Photovoltaic technology converts sunlight directly into electricity. Solar energy is fast becoming popular in rural and remote areas.

The largest solar plant of India is located at Madhapur near Bhuj, where solar energy is used to sterilise milk cans. It is expected that use of solar energy will be able to minimise the dependence of rural households on firewood and dung cakes, which in turn will contribute to environmental conservation and adequate supply of manure in agriculture.

Wind power

India now ranks as a wind super power in the world. The largest wind farm cluster is located in Tamil Nadu from Nagarcoil to Madurai. Apart from these, Andhra Pradesh, Karnataka, Gujarat, Kerala, Maharashtra and Lakshadweep have important wind farms. Nagarcoil and Jaisalmer are well known for effective use of wind energy in the country.

Biogas, tidal and geothermal

  • Biogas: Shrubs, farm waste, animal and human waste are used to produce biogas for domestic consumption in rural areas. Biogas plants using cattle dung are known as 'Gobar gas plants'. These provide twin benefits to the farmer in the form of energy and improved quality of manure. Biogas is by far the most efficient use of cattle dung. It improves the quality of manure and also prevents the loss of trees and manure due to burning of fuel wood and cow dung cakes.
  • Tidal energy: Oceanic tides can be used to generate electricity. Floodgate dams are built across inlets. During high tide water flows into the inlet and gets trapped when the gate is closed. After the tide falls outside the flood gate, the water retained by the floodgate flows back to the sea via a pipe that carries it through a power-generating turbine. In India the Gulf of Khambhat, the Gulf of Kachchh in Gujarat on the western coast and Gangetic delta in Sunderban regions of West Bengal provide ideal conditions for utilising tidal energy.
  • Geothermal energy: Geothermal energy refers to the heat and electricity produced by using the heat from the interior of the Earth. Geothermal energy exists because, the Earth grows progressively hotter with increasing depth. Two experimental projects have been set up in India: one in the Parvati valley near Manikaran in Himachal Pradesh and the other in the Puga Valley, Ladakh.

Conservation of energy resources

Energy is a basic requirement for economic development. Every sector of the national economy needs inputs of energy. There is an urgent need to develop a sustainable path of energy development. Promotion of energy conservation and increased use of renewable energy sources are the twin planks of sustainable energy.

As a concerned citizen you can do your bit by using public transport systems instead of individual vehicles; switching off electricity when not in use; using power-saving devices and using non-conventional sources of energy.

📌 Examples
  • India's largest solar plant at Madhapur near Bhuj uses solar energy to sterilise milk cans.
  • The largest wind farm cluster runs in Tamil Nadu from Nagarcoil to Madurai; Jaisalmer is the other well-known site.
  • Geothermal projects at Parvati valley near Manikaran in Himachal Pradesh and in the Puga Valley, Ladakh.
📊 Visual ideas
Classification chart - Conventional energy (firewood, cattle dung cake, coal, petroleum, natural gas, electricity) against non-conventional energy (solar, wind, tidal, geothermal, biogas, atomic).

Key Concepts

Mineral
A homogeneous, naturally occurring substance with a definable internal structure, ranging from the hardest diamond to the softest talc.
Veins and lodes
Mineral occurrences in cracks, crevices, faults or joints of igneous and metamorphic rocks - veins are smaller, lodes larger.
Placer deposits
Alluvial deposits in valley sands and hill bases containing minerals not corroded by water - gold, silver, tin, platinum.
Magnetite
The finest iron ore, with iron content up to 70 per cent and excellent magnetic qualities.
Haematite
The most important industrial iron ore by quantity used, with 50-60 per cent iron content.
Ferrous minerals
Minerals containing iron, such as iron ore and manganese, which account for the bulk of metallic mineral production.
Non-ferrous minerals
Metallic minerals that do not contain iron, such as copper and bauxite.
Bauxite
A clay-like residual deposit from which alumina and then aluminium is obtained; Odisha is India's largest producer.
Mica
A mineral of plates or leaves that splits into thin sheets, with excellent di-electric strength, low power loss factor and resistance to high voltage.
Limestone
A rock of calcium or calcium-magnesium carbonates, the basic raw material for cement and essential for smelting iron ore.
Peat
The first stage of coal, formed from decaying plants in swamps, with low carbon, high moisture and low heating capacity.
Lignite
Low grade brown coal, soft and high in moisture; the principal reserves are at Neyveli in Tamil Nadu.
Bituminous coal
Deeply buried coal subjected to increased temperature, the most popular in commercial use; its high grade form is metallurgical coal.
Anthracite
The highest quality hard coal.
Gondwana coal
Metallurgical coal a little over 200 million years old, found chiefly in the Damodar valley at Jharia, Raniganj and Bokaro.
Anticline
An upfold in rock in whose crest petroleum is trapped, held by intervening non-porous layers.
Hazira-Vijaipur-Jagdishpur pipeline
The 1700 km cross-country gas pipeline linking Mumbai High and Bassein with fertiliser, power and industrial complexes in western and northern India.
Conventional sources of energy
Firewood, cattle dung cake, coal, petroleum, natural gas and electricity.
Non-conventional sources of energy
Solar, wind, tidal, geothermal, biogas and atomic energy.
Photovoltaic technology
Technology that converts sunlight directly into electricity.
Gobar gas plant
A biogas plant using cattle dung, giving the farmer both energy and improved manure - the most efficient use of cattle dung.
Geothermal energy
Heat and electricity produced using the heat of the earth's interior, which grows hotter with increasing depth.

End-of-Chapter Trial Paper & Test Questions

Topic-wise questions to test your understanding of every concept in this chapter.

  1. What is a mineral, and how do ferrous minerals differ from non-ferrous minerals? / खनिज क्या है, और लौह खनिज अलौह खनिजों से किस प्रकार भिन्न हैं?
    Show answer

    A mineral is a homogeneous, naturally occurring substance with a definable internal structure; ferrous minerals such as iron ore and manganese contain iron, while non-ferrous minerals such as copper and bauxite do not contain iron. / खनिज एक समांगी, प्राकृतिक रूप से पाया जाने वाला पदार्थ है जिसकी एक निश्चित आंतरिक संरचना होती है; लौह खनिजों जैसे लौह अयस्क और मैंगनीज में लोहा होता है, जबकि अलौह खनिजों जैसे ताँबा और बॉक्साइट में लोहा नहीं होता।

  2. Explain how minerals occur in igneous and sedimentary rocks with one example each. / आग्नेय और अवसादी चट्टानों में खनिजों की उपस्थिति को एक-एक उदाहरण सहित समझाइए।
    Show answer

    In igneous and metamorphic rocks minerals occur in cracks and faults as veins and lodes, e.g. tin and copper, whereas in sedimentary rocks they occur in beds formed by deposition and accumulation in horizontal strata, e.g. coal and limestone. / आग्नेय और कायांतरित चट्टानों में खनिज दरारों और भ्रंशों में शिराओं और निक्षेपों के रूप में पाए जाते हैं, जैसे टिन और ताँबा, जबकि अवसादी चट्टानों में वे क्षैतिज परतों में निक्षेपण द्वारा बनी संस्तरों में पाए जाते हैं, जैसे कोयला और चूना-पत्थर।

  3. Why is conservation of minerals essential, and suggest two ways to conserve them. / खनिजों का संरक्षण क्यों आवश्यक है, और इन्हें संरक्षित करने के दो उपाय सुझाइए।
    Show answer

    Minerals are non-renewable and take millions of years to form, but are being depleted rapidly; they can be conserved by using them economically and by recycling metals like iron, aluminium and copper. / खनिज अनवीकरणीय हैं और बनने में लाखों वर्ष लगते हैं, परंतु तेज़ी से समाप्त हो रहे हैं; इन्हें किफ़ायती उपयोग करके तथा लोहा, ऐलुमिनियम और ताँबा जैसी धातुओं के पुनर्चक्रण द्वारा संरक्षित किया जा सकता है।

  4. Distinguish between conventional and non-conventional sources of energy with examples. / ऊर्जा के परंपरागत और गैर-परंपरागत स्रोतों में उदाहरण सहित अंतर बताइए।
    Show answer

    Conventional sources are traditional and largely non-renewable, such as coal, petroleum and firewood, while non-conventional sources are renewable and eco-friendly, such as solar, wind, tidal and geothermal energy. / परंपरागत स्रोत पारंपरिक और मुख्यतः अनवीकरणीय होते हैं, जैसे कोयला, पेट्रोलियम और लकड़ी, जबकि गैर-परंपरागत स्रोत नवीकरणीय और पर्यावरण-अनुकूल होते हैं, जैसे सौर, पवन, ज्वारीय और भूतापीय ऊर्जा।

  5. Why is petroleum called 'liquid gold' and what are its major uses? / पेट्रोलियम को 'तरल सोना' क्यों कहा जाता है और इसके प्रमुख उपयोग क्या हैं?
    Show answer

    Petroleum is called liquid gold because of its high economic value and scarcity; it provides fuel for transport, heat and lighting, lubricants, and raw materials for many manufacturing industries such as plastics and fertilisers. / पेट्रोलियम को इसके उच्च आर्थिक मूल्य और दुर्लभता के कारण तरल सोना कहा जाता है; यह परिवहन के लिए ईंधन, ताप और प्रकाश, स्नेहक तथा प्लास्टिक और उर्वरक जैसी अनेक विनिर्माण इकाइयों के लिए कच्चा माल प्रदान करता है।

  6. Explain why solar energy has a bright future in India. / भारत में सौर ऊर्जा का भविष्य उज्ज्वल क्यों है, समझाइए।
    Show answer

    India lies in the tropical region and receives abundant sunlight throughout the year, so solar energy can be tapped through photovoltaic cells to meet rural and urban energy needs in a clean, renewable manner. / भारत उष्ण कटिबंधीय क्षेत्र में स्थित है और वर्ष भर प्रचुर धूप प्राप्त करता है, इसलिए सौर ऊर्जा को फोटोवोल्टिक सेलों द्वारा ग्रहण करके ग्रामीण और शहरी ऊर्जा आवश्यकताओं को स्वच्छ, नवीकरणीय रूप में पूरा किया जा सकता है।

  7. What is bauxite, and why is the aluminium produced from it important? / बॉक्साइट क्या है, और इससे प्राप्त ऐलुमिनियम क्यों महत्त्वपूर्ण है?
    Show answer

    Bauxite is the ore from which aluminium is obtained; aluminium is important because it combines the strength of metals like iron with light weight, good conductivity and malleability, making it useful in aircraft, utensils and wiring. / बॉक्साइट वह अयस्क है जिससे ऐलुमिनियम प्राप्त होता है; ऐलुमिनियम महत्त्वपूर्ण है क्योंकि यह लोहे जैसी धातुओं की मज़बूती के साथ हल्कापन, अच्छी चालकता और आघातवर्धनीयता रखता है, जिससे यह वायुयान, बर्तन और तारबंदी में उपयोगी है।

  8. How does mining create health and environmental hazards for miners and surrounding areas? / खनन कैसे खनिकों तथा आसपास के क्षेत्रों के लिए स्वास्थ्य और पर्यावरणीय खतरे उत्पन्न करता है?
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    Mining exposes workers to dust and toxic fumes causing pulmonary diseases, risks of mine collapse, flooding and fires, while it also degrades land, pollutes water sources and damages the surrounding environment. / खनन से श्रमिक धूल और विषैले धुएँ के संपर्क में आते हैं जिससे फेफड़ों के रोग होते हैं, खान धँसने, जलप्लावन और आग का खतरा रहता है, साथ ही यह भूमि को क्षरित करता है, जल स्रोतों को प्रदूषित करता है और आसपास के पर्यावरण को नुकसान पहुँचाता है।

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