Geography Set 28
π
π Physical Geography β’ Geology
Q.1) The Deccan Trap lava plateau consists of multiple basaltic lava flows interspersed with sedimentary beds. What is the average thickness of these individual lava flows?
Ans > 5 m to 29 m
- Geological Origins: The Deccan Traps represent one of the largest volcanic features on Earth. They formed between 60 and 68 million years ago during the late Cretaceous period. Massive, fissure-based volcanic eruptions deposited immense volumes of basaltic lava over roughly 30,000 years.
- Step-Like Topography: The term “trap” is derived from the Swedish word ‘trappa’, which means stairs. This perfectly describes the unique, terraced landscape created by these overlapping lava flows, which average 5 to 29 metres in thickness.
- Agricultural Significance: Over millions of years, the weathering of this basaltic rock has produced deep, highly fertile black soils (known as regur). This soil retains moisture exceptionally well, making the Deccan Plateau India’s premier region for cotton cultivation.
π Indian Geography β’ Evolution
Q.2) Two great geological events occurred during the Tertiary Period: the final breaking-up of the old Gondwana continent and the uplift of which ancient geosyncline into the Himalayas?
Ans > Tethys
- The Ancient Tethys Sea: Before the formation of the Himalayas, a vast, shallow marine basin known as the Tethys Sea (or Tethys geosyncline) existed between the ancient supercontinents of Laurasia to the north and Gondwanaland to the south.
- Tectonic Collision: During the Tertiary period, the Indian plate broke away from Gondwanaland and drifted rapidly northward. As it collided with the immense Eurasian plate, the tremendous compressive forces caused the tectonic boundary to buckle.
- Himalayan Uplift: The massive layers of marine sediments that had accumulated on the floor of the Tethys Sea over millions of years were squeezed, folded, and thrust upward. This dramatic geological event birthed the mighty Himalayan mountain range, which continues to rise slowly today due to ongoing tectonic pressure.
π Stratigraphy β’ Time Scale
Q.3) In the Indian Geological Time Scale advocated by T.S. Holland, the Pre-Cambrian Era (which includes the Cuddapah and Vindhyan systems) is recognized by which collective name?
Ans > The Purana Group
- Hollandβs Classification: Sir Thomas Henry Holland, a prominent British geologist who worked extensively in India, proposed a unique geological time scale specifically tailored for the Indian subcontinent. He categorized Indian rock systems into four broad divisions: Archaean, Purana, Dravidian, and Aryan.
- The Purana Group defined: The term “Purana” translates to ‘ancient’ in Sanskrit. In geological terms, the Purana Group corresponds to the Proterozoic eon (late Pre-Cambrian era). It encompasses sedimentary rock formations that are younger than the primary Archaean rocks but older than the fossil-bearing rocks of the Cambrian period.
- Economic Importance: The Purana rock system includes the famous Cuddapah and Vindhyan formations. These ancient structural beds are incredibly significant for India’s economy, as they are major sources of valuable building stones, limestones used for cement, and notably, the diamond-bearing conglomerates found in regions like Panna.
π Topography β’ Plateaus
Q.4) The Malwa Plateau is bordered by the Aravallis in the north and the Bundelkhand Plateau in the east. Which prominent mountain range bounds it in the south?
Ans > Vindhyan Range
- Geographical Boundaries: The Malwa Plateau occupies a central position in India, acting as a transitional zone between the northern plains and the peninsular south. Its natural borders are distinctly defined by the Aravalli Range to the northwest and the Vindhyan Range stretching across its southern edge.
- Drainage Patterns: The topography of the plateau dictates the flow of its major rivers. Because the Vindhyan Range forms an elevated southern wall, the plateau slopes gently toward the north and northeast. Consequently, important rivers like the Chambal, Betwa, and Ken flow northward to join the Yamuna river system.
- Historical and Cultural Hub: Historically, the Malwa region has been a melting pot of cultures and a crucial transit route connecting northern India to the western coast. The fertile volcanic soils found here have supported rich agricultural communities and prosperous ancient kingdoms, such as those ruled from Ujjain and Mandu.
π Mountains β’ Northeast India
Q.5) The highest point of the Meghalaya Plateau reaches an elevation of approximately 1965 metres. What is the name of this peak?
Ans > Shillong Peak
- Topographical Dominance: Shillong Peak stands as the highest point in the entire state of Meghalaya, reaching an altitude of roughly 1965 metres (often cited as 1961m in recent surveys). It offers a commanding, panoramic view of the city of Shillong and the surrounding lush, rolling hills.
- Geological Context: The Meghalaya Plateau, despite being located in the northeast, is geologically an eastward extension of the ancient Indian Peninsular Plateau, separated from it by the Malda fault gap. It is distinctly different in its rock composition from the younger, folded Himalayas to its north.
- Cultural and Strategic Importance: Local Khasi traditions hold the peak in high reverence, believing it to be the abode of the patron deity of Shillong, ‘U Shulong’. Today, due to its immense strategic altitude and location, the area around the peak is heavily administered by the Indian Air Force and hosts a crucial radar station.
π Indian Geography β’ Basins
Q.6) The Mahanadi Basin, sprawling over the districts of Raipur, Bilaspur, and Durg, is widely known by which alternative regional name?
Ans > Chhattisgarh Plain
- Structural Basin: The Chhattisgarh Plain is a prominent geographical feature in central India. It forms a large, saucer-shaped structural basin that is entirely drained by the upper Mahanadi River and its numerous tributaries. This depression is surrounded by higher elevations, including the Maikal Range and the Chota Nagpur Plateau.
- The “Rice Bowl” of Central India: The plain is characterized by relatively flat terrain and deep, fertile soils composed largely of red and yellow earth. Combined with adequate monsoon rainfall and extensive canal irrigation, this region is a massive producer of paddy, earning it the nickname “the rice bowl of Central India.”
- Industrial Heartland: Beneath the agricultural surface, the margins of the Chhattisgarh Plain are incredibly rich in mineral resources, particularly coal and iron ore. This geological wealth has spurred intense industrialization in districts like Durg (home to the Bhilai Steel Plant), transforming the agrarian basin into a major manufacturing hub.
π Topography β’ Peaks
Q.7) The Karnataka Plateau features an average elevation of 600-900 metres. What is the name of its highest peak, which reaches 1930 metres in the Baba-Budan Hills?
Ans > Mullayanagiri (Mulangiri)
- The Highest Point: Mullayanagiri, standing at an elevation of 1930 metres, is not only the highest peak in the Baba-Budan Hills but the highest peak in the entire state of Karnataka. It forms a crucial part of the towering Western Ghats mountain ecosystem in the Chikkamagaluru district.
- Historical Coffee Connection: The Baba-Budan Hills hold a legendary place in Indian agricultural history. According to tradition, the 17th-century Sufi saint Baba Budan smuggled seven raw coffee beans from Mocha (Yemen) and planted them in these very hills, giving birth to India’s vast coffee industry, which still dominates the region’s slopes today.
- Ecological Hotspot: The high-altitude terrain surrounding Mullayanagiri consists of unique shola grassland ecosystems interspersed with thick, stunted tropical montane forests. This environment supports endemic flora and fauna and acts as a vital catchment area for major rivers that sustain the southern Indian peninsula.
π Transport β’ Mountain Passes
Q.8) Which of the following passes in the Western Ghats joins Mumbai with Pune and sits at an elevation of about 1000 metres above sea level?
Ans > Bhor Ghat
- Crucial Transport Artery: Bhor Ghat is a steep mountain pass located in the Sahyadri range (Western Ghats) of Maharashtra. Historically and currently, it serves as the most critical land route connecting the coastal metropolis of Mumbai with the inland city of Pune and the broader Deccan Plateau.
- Engineering Marvels: Overcoming the steep gradient of Bhor Ghat was a major challenge during the British colonial era. The construction of the Great Indian Peninsula Railway line through this pass in the 1860s involved drilling multiple tunnels and building immense viaducts, making it one of the most ambitious engineering projects of its time.
- Economic Lifeline: Today, both the Mumbai-Pune Expressway and the central railway line traverse this ghat. It facilitates the massive daily movement of freight and passengers, effectively integrating the booming IT and manufacturing hubs of Pune with the financial capital of Mumbai, thus driving the regional economy.
π Topography β’ Western Ghats
Q.9) The Western Ghats (Sahyadris) form a massive watershed running parallel to the western coast. They stretch for about 1600 km from Kanyakumari up to the mouth of which river in the north?
Ans > Tapi
- Geographical Extent: The Western Ghats are a formidable continuous mountain chain that forms the western edge of the Deccan Plateau. They begin their 1600 km southward journey precisely at the valley of the Tapi River in Gujarat/Maharashtra, running parallel to the Arabian Sea until they terminate at Kanyakumari, the southern tip of India.
- The Great Escarpment: Geologically, the Western Ghats are not true fold mountains but rather a prominent fault scarp. They were formed by the tectonic uplift and subsequent tilting of the Indian peninsula during the breakup of Gondwanaland, which explains their steep, cliff-like faces on the western coastal side.
- Major Hydrological Divide: Acting as one of India’s most critical watersheds, the Western Ghats intercept the moisture-laden southwest monsoon winds, resulting in heavy rainfall. This immense runoff gives birth to almost all the major east-flowing peninsular rivers, including the Godavari, Krishna, and Kaveri, which sustain millions across southern India.
π Topography β’ Eastern Ghats
Q.10) The Eastern Ghats consists of a series of detached hills. Which of the following peaks is NOT a part of the Eastern Ghats?
Ans > Kalsubai
- Identifying Kalsubai: Kalsubai, standing proudly at 1646 metres, is famously known as the “Everest of Maharashtra.” It is located in the Sahyadri ranges, making it a prominent peak of the Western Ghats, not the Eastern Ghats. It represents the highest point in Maharashtra.
- Nature of the Eastern Ghats: Unlike the continuous, towering Western Ghats, the Eastern Ghats are a highly fragmented and discontinuous range of lower hills. Over millions of years, mighty east-flowing rivers like the Mahanadi, Godavari, and Krishna have aggressively eroded and cut through these mountains to reach the Bay of Bengal.
- Prominent Eastern Peaks: The hills that do remain in the Eastern Ghats form distinct, localized ranges such as the Javadi, Shevaroy, and Nallamala hills. Peaks like Mahendragiri (1501 m) in Odisha and Singaraju represent some of the highest surviving elevations within this heavily weathered and ancient geological formation.
π Geography β’ Himalayan Faults
Q.11) Which major tectonic fault line physically separates the rugged Lesser Himalayas from the younger Shiwaliks (Outer Himalayas)?
Ans > Main Boundary Thrust (MBT)
- Himalayan Fault Systems: The Himalayas are heavily fractured by a series of massive, parallel thrust faults created by the relentless northward push of the Indian tectonic plate. The Main Boundary Thrust (MBT) is one of the most significant of these fault lines, running almost the entire length of the mountain range.
- Geological Division: The MBT serves as the distinct structural boundary that sharply divides two very different geological zones: the older, more highly metamorphosed rocks of the Lesser Himalayas to the north, and the much younger, softer, unconsolidated sedimentary rocks of the Shiwalik range (Outer Himalayas) to the south.
- Seismic Danger Zone: Because the Indian plate is still actively moving under the Eurasian plate, the MBT remains a highly active tectonic feature. Stress accumulates along this fault line over time, making the regions located immediately along the MBT highly susceptible to catastrophic, high-magnitude earthquakes.
π Topography β’ Trans-Himalayas
Q.12) The Trans-Himalayas contain the Tethys marine sediments and constitute the core of the Himalayan axis. Which of the following ranges belongs to the Trans-Himalayas?
Ans > Zaskar and Ladakh
- Defining the Trans-Himalayas: The Trans-Himalayas, also known as the Tibetan Himalayas, are a distinct mountain system situated immediately north of the Great Himalayan range. This zone was actually the first to be uplifted from the ancient Tethys Sea, making its rock formations generally older than the main Himalayas.
- The Zaskar and Ladakh Ranges: The rugged Zaskar (or Zanskar) Range and the barren, high-altitude Ladakh Range are the most prominent parallel mountain chains within the Trans-Himalayan region in India. The Indus River famously cuts a deep gorge right between these two massive ranges as it flows toward Pakistan.
- Harsh Alpine Desert: Because the towering Great Himalayas to the south block the moisture-laden monsoon winds, the Trans-Himalayan region (including Ladakh and Zaskar) receives almost no rainfall. This results in a stark, high-altitude cold desert environment characterized by extreme temperatures and sparse vegetation.
π Geology β’ Valleys
Q.13) The Kashmir Valley is described as a structural longitudinal ‘Doon’ filled with lacustrine deposits. It is structurally surrounded by the Greater Himalayas and which other mountain range?
Ans > Pir-Panjal Range
- The Valley’s Enclosure: The breathtaking Kashmir Valley is an oval-shaped, structurally depressed basin nestled deep within the Himalayan system. It is securely walled in by two massive mountain barriers: the towering Great Himalayas to its northeast and the imposing Pir-Panjal range running along its southwest.
- Geological Origins: Geologists describe the Kashmir Valley as a massive synclinal basin (a structural trough) that was once occupied by a vast Pleistocene-era lake. As the Pir-Panjal range actively uplifted, it temporarily blocked the drainage of the region, creating a massive water body.
- Lacustrine Deposits: Over millennia, the ancient lake slowly drained away through a gorge cut by the Jhelum river near Baramulla. What remained were incredibly thick beds of fine clays, sands, and lacustrine (lake-based) sediments. These fertile remnants form the famous ‘Karewa’ terraces that define the valley’s modern landscape.
π Transport β’ Mountain Passes
Q.14) Which high-altitude mountain pass, located in the Greater Himalayas of Arunachal Pradesh, connects the state with Lhasa, the capital of Tibet?
Ans > Bomdi La
- Strategic Location: Bomdi La is a crucial, high-altitude mountain pass (sitting at an elevation of roughly 2600 metres) situated in the Greater Himalayas. Located in the West Kameng district of Arunachal Pradesh, it serves as the vital gateway connecting the Indian plains to the mountainous Tawang region.
- Historical Trade Route: For centuries, Bomdi La functioned as an integral part of the ancient, rugged trade networks traversing the Himalayas. It provided a direct, albeit treacherous, overland route for merchants, monks, and travelers moving between northeastern India and Lhasa, the traditional capital of Tibet.
- Military Significance: The pass gained immense strategic and historical importance during the 1962 Sino-Indian War. The heavy fighting that occurred in and around Bomdi La highlighted its critical role as a military chokepoint. Today, it remains heavily fortified and maintained by the Indian Army’s Border Roads Organisation to ensure year-round connectivity.
π Agriculture β’ Soil Types
Q.15) The Karewas of the Kashmir Valley are well known for the cultivation of various high-value agricultural products. Which of the following is NOT typically cultivated on these lacustrine deposits?
Ans > Tea
- Understanding Karewas: Karewas are highly unique geological formations found exclusively in the Kashmir Valley. They are thick, elevated tablelands composed of ancient lacustrine (lake-deposited) sediments, clays, and sands left behind when the Pleistocene lake that once filled the valley finally drained.
- High-Value Crops: The soil composition of the Karewas, combined with Kashmir’s temperate climate, creates ideal conditions for cultivating specialized, high-value horticulture. The plateau regions of Pampore and Pulwama are globally renowned for producing premium saffron, alongside vast orchards of almonds, walnuts, and apples.
- Why Not Tea?: Tea cultivation strictly requires a warm, humid, tropical or subtropical climate with abundant, evenly distributed rainfall throughout the year, typically found in regions like Assam, Darjeeling, or the Nilgiris. The harsh winters, heavy snowfall, and distinct temperate climate of the Kashmir Valley make it completely unsuited for commercial tea production.
π Physical Geography β’ Glaciers
Q.16) Measuring approximately 15 km in length, what is the name of the longest glacier of the Pir-Panjal range, located in the Chandra Valley of the Lahul and Spiti region?
Ans > Sonapani glacier
- Glacial Giant of Pir-Panjal: The Sonapani glacier holds the distinction of being the longest glacier in the entire Pir-Panjal mountain range. Stretching for roughly 15 kilometres, it is a massive river of ice located at a staggering altitude of about 4000 metres.
- Location in Lahaul and Spiti: This massive glacier is situated within the harsh, high-altitude terrain of the Chandra Valley in the Lahaul and Spiti district of Himachal Pradesh. It can be viewed prominently from the Rohtang Pass, serving as a popular spectacle for trekkers and researchers.
- Hydrological Importance: Like many Himalayan glaciers, the Sonapani glacier plays a critical role in the region’s hydrology. The meltwater from this glacier feeds directly into the upper tributaries of the Chenab River system, providing an essential, year-round water supply for agriculture and hydroelectric projects downstream in the plains.
π Geography β’ Rivers & Islands
Q.17) The Brahmaputra River has a low gradient in the Assam valley, causing it to become highly braided with numerous islands. Which of the following is the most prominent riverine island formed by the Brahmaputra?
Ans > Majuli
- The Braided River: As the mighty Brahmaputra river descends from the steep Himalayas and enters the relatively flat Assam Valley, its gradient drops sharply. This sudden loss of velocity causes the river to drop its massive silt load, forming a complex, highly braided channel network choked with sandbars.
- Majuli’s Formation: In the heart of this braided network lies Majuli, widely recognized as the largest riverine island in the world. Formed over centuries by the constant shifting and deposition of massive amounts of alluvium by the Brahmaputra and its tributaries, the island’s exact shape and size change with every annual flood season.
- Cultural Hub: Beyond its geographic uniqueness, Majuli is the epicenter of Assamese neo-Vaishnavite culture. It is home to numerous ancient ‘Sattras’ (monasteries) that preserve centuries-old traditions of classical dance, music, and art, making it a proposed UNESCO World Heritage site despite the ongoing threat of severe riverbank erosion.
π Drainage System β’ Rivers
Q.18) The Yamuna River is the longest and the western-most tributary of the Ganga. What is the total length of the Yamuna River?
Ans > 1380 km
- Glacial Origins: The Yamuna River originates from the pristine Yamunotri Glacier, located at a massive elevation of 6,387 metres on the southwestern slopes of the Banderpoonch peaks in the Lower Himalayas of Uttarakhand.
- A Massive Tributary: Journeying a total distance of approximately 1,380 kilometres, the Yamuna holds the title of the longest and largest tributary of the Ganga in India. It flows parallel to the Ganga for hundreds of kilometres, creating the highly fertile Doab region, before finally merging with it at the Triveni Sangam in Prayagraj (Allahabad).
- Pollution Challenges: Despite its sacred status and its critical role in supplying water to major cities like Delhi, Agra, and Mathura, the Yamuna is currently one of the most heavily polluted rivers in the world. Industrial runoff, untreated sewage, and agricultural chemicals have severely degraded its water quality, especially in the stretches downstream of the national capital.
π Drainage System β’ Confluence
Q.19) Which easterly flowing river of the Peninsular Region is formed by the confluence of the South Koel and Sankh rivers near Rourkela?
Ans > Brahmani
- The Point of Confluence: The Brahmani River is a major seasonal river in eastern India. It does not have a single source but is instead formed by the dramatic confluence of two distinct riversβthe South Koel and the Sankh. These rivers join near Vedvyas in the industrial city of Rourkela, Odisha.
- Course and Basin: After its formation, the Brahmani carves its way southward through the rugged Garhjat Hills and the mineral-rich Chota Nagpur Plateau. It flows for nearly 480 kilometres before merging with the Baitarani River to form a massive estuarine delta that empties into the Bay of Bengal.
- Industrial Lifeline: The Brahmani basin is of immense economic importance. Because it flows directly through India’s premier coal and iron ore belts, the river serves as the primary water lifeline for heavy industries, including the massive Rourkela Steel Plant, and supports agricultural irrigation in the coastal plains of Odisha.
π Climatology β’ Monsoons
Q.20) The classical “Thermal Concept” explaining the Indian Monsoons as large-scale land and sea breezes produced by differential heating and cooling was proposed by:
Ans > Halley
- The Scientist Behind the Theory: In 1686, the famous English astronomer and meteorologist Sir Edmond Halley (best known for calculating the orbit of Halley’s Comet) published a seminal paper. He proposed what is now known as the “Classical Theory” or “Thermal Concept” of the Indian monsoon.
- Differential Heating Explained: Halley theorized that monsoons are essentially gigantic land and sea breezes operating on a continental scale. He argued that during the summer, the vast Asian landmass heats up much faster than the surrounding Indian Ocean, creating a massive low-pressure area that aggressively pulls in moisture-laden winds from the sea.
- Modern Revisions: While Halley’s thermal concept provided the foundational understanding of monsoons for centuries, modern meteorology has proven it to be overly simplistic. Today, we know the monsoon is a vastly more complex system influenced by the shifting of the Intertropical Convergence Zone (ITCZ), the Tibetan plateau’s high-altitude heating, and global jet streams.
π Climatology β’ Weather Systems
Q.21) According to the modern concepts of the Indian monsoon, the summer-time heating of the Tibetan Plateau produces a thermal anticyclone (high pressure) in the middle part of the troposphere. At what specific atmospheric pressure level does this form?
Ans > 500 mb level
- The Tibetan Heating Engine: During the intense summer months, the massive, elevated Tibetan Plateauβoften called the “Roof of the World”βabsorbs vast amounts of solar radiation. Because it sits at an average altitude of 4,500 metres, it acts as a giant radiator, heating the middle of the atmosphere directly.
- Anti-Cyclogenesis at 500 mb: This intense, localized heating causes the air above the plateau to expand and rise. As this air ascends into the middle troposphere (specifically around the 500 millibar atmospheric pressure level), it spreads outward, forming a strong, warm-core thermal anticyclone (a high-pressure system).
- Driving the Monsoon: This 500 mb anticyclone is critical for the Indian monsoon. The outward flow of air at this high altitude pushes southward toward the equator, where it descends over the Indian Ocean. This descending air strengthens the surface high-pressure system over the ocean, forcefully pushing the moisture-laden southwest monsoon winds directly toward the Indian subcontinent.
π Climatology β’ Monsoons
Q.22) During a “break” in the monsoon, rainfall practically ceases over the plains of India. This occurs because the broad-scale surface pressure, known as the monsoon trough, shifts towards which region?
Ans > The Himalayas
- The Monsoon Trough: The monsoon trough is a massive, elongated belt of low atmospheric pressure that typically stretches across the plains of northern India from Rajasthan to the Bay of Bengal. It acts as a magnet, drawing in and steering the moisture-laden monsoon winds across the subcontinent.
- The Shift Northward: The position of this trough is not static. Periodically, the axis of the trough migrates drastically northward, settling right along the foothills of the Himalayas. When this shift occurs, it triggers what meteorologists call a “break” in the monsoon.
- Impact on Rainfall: During a break phase, rainfall practically dries up over the vast agricultural plains of central and northern India. Conversely, because the low-pressure trough is now parked against the mountains, the Himalayan foothills and northeastern states experience devastatingly heavy rainfall, frequently resulting in massive floods in rivers like the Brahmaputra.
π Geography β’ Soil Types
Q.23) Which soil type covers about 15 million hectares in India, contains varying percentages of calcium carbonate, and is deposited mainly by wind action?
Ans > Desert Soils
- Extent and Location: Desert soils, also known as arid soils, cover approximately 15 million hectares of the Indian landmass. They are predominantly found in the arid and semi-arid regions of northwestern India, encompassing large tracts of western Rajasthan, southern Haryana, and northern Gujarat.
- Aeolian Deposits: Unlike alluvial or black soils formed by rivers or volcanic activity, desert soils are largely ‘aeolian’ in natureβmeaning they are deposited and heavily influenced by wind action. Over millennia, strong winds have blown vast amounts of sand and dust into these regions, creating deep, sandy profiles.
- Chemical Composition: These soils are generally sandy in texture, poor in organic matter (humus), and highly deficient in nitrogen. However, they frequently contain high and varying percentages of soluble salts and calcium carbonate (forming ‘kankar’ nodules in the lower layers), which heavily restricts the downward infiltration of water.
π Economic Geography β’ Minerals
Q.24) Which Indian state is the leading producer of iron ore, accounting for over half of the country’s total iron ore production today?
Ans > Odisha (Orissa)
- The Iron Ore Giant: According to the most recent data from the Ministry of Mines, Odisha is the undisputed leader in iron ore production in India. The state consistently accounts for over 50% of the country’s total iron ore output, far surpassing historical leaders like Karnataka or Jharkhand.
- Prime Mining Districts: Odisha’s dominance is driven by the incredibly rich, high-grade hematite deposits found in its northern districts. The sprawling mining complexes in Keonjhar, Sundargarh, and Mayurbhanj boast some of the largest and most easily accessible iron ore reserves in all of Asia.
- Economic Impact: This massive extraction scale is the backbone of eastern India’s heavy industry. The abundant, high-quality ore directly feeds a massive network of domestic steel plants, both within the state (like Rourkela Steel Plant) and across the nation, while also serving as a major export commodity for the Indian economy.
π Economic Geography β’ Industries
Q.25) The integrated copper mining-cum-ore refining plant known as the Khetri Copper Complex is located in the Jhunjhunu District of which state?
Ans > Rajasthan
- Historical Copper Hub: The Khetri region in the Jhunjhunu district of Rajasthan boasts a remarkably long history of copper extraction. Archaeological evidence suggests that copper mining and crude smelting have occurred in the Aravalli hills surrounding Khetri since the ancient Indus Valley Civilization.
- The Modern Complex: To tap into these historic reserves on an industrial scale, the Government of India established the Khetri Copper Complex (KCC) in 1967 under the public sector enterprise Hindustan Copper Limited. It was designed as a massive, fully integrated facility capable of both mining the raw ore and refining it into usable copper.
- Industrial Decline and Heritage: While the KCC was once a bustling pillar of India’s non-ferrous metal industry, producing thousands of tonnes of copper annually, mining operations have severely dwindled in recent years due to the depletion of high-grade ore and high operational costs. However, it remains a site of immense geological and industrial heritage.
π Economic Geography β’ Minerals
Q.26) Panna is the main diamond-producing district in India. From which geological system’s formations does this district extract diamonds?
Ans > Vindhyan System
- The Vindhyan Rock System: The Vindhyan geological system is an ancient sedimentary rock formation that stretches widely across central India. Formed during the Proterozoic eon, it is largely composed of un-fossiliferous, horizontally bedded sandstones, shales, and limestones that accumulated in shallow marine basins.
- The Panna Diamond Belt: Located in Madhya Pradesh, the Panna district is practically synonymous with Indian diamond mining. The diamonds here are not found in deep, volcanic kimberlite pipes (as in South Africa) but are instead embedded within the ancient, conglomeratic sedimentary beds of the Vindhyan system.
- Mining Operations: The National Mineral Development Corporation (NMDC) operates the primary mechanized diamond mine at Majhgawan in Panna. Alongside this large-scale operation, the region is famous for thousands of small, shallow, artisanal lease-mines where local workers meticulously sift through the Vindhyan gravel hoping to uncover gem-quality stones.
π Economic Geography β’ Minerals
Q.27) Chromite is an oxide of iron and chromium widely used in metallurgy. Which state is the absolute largest producer of chromite in India, accounting for about 99 per cent of the total production?
Ans > Orissa
- A Strategic Mineral: Chromite is a critically important industrial mineral. It is the only commercially viable ore of chromium, an element that is absolutely essential for the production of stainless steel, nichrome alloys, and various heat-resistant refractory materials used in high-temperature industrial furnaces.
- Odisha’s Total Monopoly: When it comes to chromite, Odisha (formerly Orissa) holds a virtual monopoly in India. The state possesses over 95% of the country’s total chromite reserves and consistently accounts for a staggering 99% of India’s annual chromite production.
- The Sukinda Valley: This immense wealth is not spread out but is heavily concentrated in a very small geographical area. The Sukinda Valley in the Jajpur district is one of the most prolific chromite mining belts in the world. The open-cast mining here is so intensive that it has frequently drawn severe environmental scrutiny due to hexavalent chromium contamination in local water bodies.
π Economic Geography β’ Energy Resources
Q.28) The Jharia coalfield sprawls over an area of about 460 sq km and is the largest and most important coal-producing mine in India. It produces nearly 90 per cent of the country’s:
Ans > Coking coal
- The Importance of Coking Coal: Not all coal is created equal. Coking coal (also known as metallurgical coal) is a highly specific, premium grade of bituminous coal. When heated in the absence of oxygen, it forms “coke”βa pure carbon material that is absolutely vital for smelting iron ore into steel in blast furnaces.
- Jhariaβs Dominance: Located in the Damodar River Valley of Jharkhand, the Jharia coalfield is the beating heart of India’s heavy industry. It is the only major repository of prime coking coal in the entire country, single-handedly producing nearly 90% of India’s domestic supply to feed the massive steel plants of the eastern sector.
- The Underground Fires: Despite its immense economic value, Jharia is globally notorious for an ongoing ecological disaster. Subsurface coal fires have been burning relentlessly beneath the Jharia coalfield for over a century (since 1916). These unquenchable fires devour millions of tonnes of premium coal, cause catastrophic land subsidence, and blanket the region in toxic fumes.
π Transport Geography β’ Pipelines
Q.29) The Lakwa-Rudrasagar-Barauni Pipeline was completed in 1968 to transport crude oil to the Barauni Oil Refinery in Bihar. From which state does this pipeline originate?
Ans > Assam
- India’s Oldest Oil Basin: Assam is the cradle of India’s petroleum industry. The upper Assam basin, encompassing regions like Digboi, Naharkatiya, Lakwa, and Rudrasagar, contains some of the oldest and most historically significant onshore crude oil reserves in the subcontinent.
- Logistical Challenges: Extracting oil in Assam presented a major geographical hurdle: the petroleum had to be transported safely and efficiently from the remote northeastern corner of the country to major refining centers situated deep within the mainland Indian plains.
- Pipeline Engineering: To solve this, the Lakwa-Rudrasagar-Barauni Pipeline was constructed and commissioned in 1968. Stretching for hundreds of kilometers, this critical piece of infrastructure pumped crude oil directly from the prolific oil fields of the Sibsagar district in Assam all the way to the massive public sector Barauni Refinery in Bihar for processing and national distribution.
π Economic Geography β’ Industries
Q.30) The true foundation of the modern cotton textile industry in India was laid in 1854 when Cowasji Nanabhoy Davar successfully set up a Spinning and Weaving Company. In which city was this historic mill established?
Ans > Mumbai (Bombay)
- A Shift to Modernization: Prior to the 1850s, Indiaβs textile industry was entirely decentralized, relying on millions of highly skilled village artisans using traditional handlooms. The establishment of the Bombay Spinning and Weaving Company in 1854 marked the dramatic beginning of India’s transition to large-scale, steam-powered, factory-based manufacturing.
- Why Mumbai?: Mumbai (then Bombay) provided the perfect storm of geographical and economic advantages for this nascent industry. It had a highly humid coastal climate (ideal for spinning cotton thread without breaking), an excellent natural harbor for importing heavy British machinery and exporting finished goods, and access to immense capital from wealthy Parsi and Gujarati merchants.
- The Cotton Boom: Davar’s massive success triggered an industrial explosion. Dozens of massive textile mills rapidly sprouted across Mumbai, transforming the city into the “Manchester of India.” This boom was further accelerated by the American Civil War in the 1860s, which severely disrupted global cotton supplies and caused a massive surge in demand for Indian textiles.
π Quick Summary β Geography Set 28
- Geology: Deccan Trap lava flows average 5-29 m in thickness.
- Evolution: Tethys geosyncline uplifted into the Himalayas during the Tertiary Period.
- Time Scale: Pre-Cambrian Era (Cuddapah/Vindhyan systems) is known as the Purana Group.
- Plateaus: The Vindhyan Range bounds the Malwa Plateau in the south.
- Peaks: Shillong Peak is the highest point of the Meghalaya Plateau.
- Basins: The Mahanadi Basin is also known as the Chhattisgarh Plain.
- Peaks: Mullayanagiri is the highest peak of the Karnataka Plateau.
- Passes: Bhor Ghat in the Western Ghats joins Mumbai with Pune.
- Western Ghats: They stretch from Kanyakumari up to the Tapi river mouth.
- Eastern Ghats: Kalsubai is a peak of the Western Ghats, NOT the Eastern Ghats.
- Faults: The Main Boundary Thrust (MBT) separates Lesser Himalayas from Shiwaliks.
- Himalayas: Zaskar and Ladakh ranges belong to the Trans-Himalayas.
- Valleys: The Kashmir Valley is surrounded by the Greater Himalayas and the Pir-Panjal Range.
- Passes: Bomdi La pass connects Arunachal Pradesh with Lhasa, Tibet.
- Soil: Tea is NOT typically cultivated on the lacustrine Karewas of Kashmir.
- Glaciers: Sonapani is the longest glacier of the Pir-Panjal range.
- Islands: Majuli is the most prominent riverine island formed by the Brahmaputra.
- Rivers: The total length of the Yamuna River is 1380 km.
- Confluence: Brahmani river is formed by the confluence of South Koel and Sankh rivers.
- Monsoons: Halley proposed the classical “Thermal Concept” of Indian Monsoons.
- Weather Systems: The Tibetan Plateau anticyclone forms at the 500 mb level.
- Monsoons: During a “break,” the monsoon trough shifts towards the Himalayas.
- Soil: Desert Soils are deposited mainly by wind action and cover ~15 million hectares.
- Minerals: Odisha (Orissa) is the leading producer of iron ore in India.
- Industries: The Khetri Copper Complex is located in Rajasthan.
- Minerals: Panna diamonds are extracted from the Vindhyan System formations.
- Minerals: Orissa is the absolute largest producer of chromite in India.
- Energy: The Jharia coalfield produces nearly 90 per cent of India’s coking coal.
- Pipelines: The Lakwa-Rudrasagar-Barauni Pipeline originates in Assam.
- Industries: The first modern cotton textile mill was established in Mumbai (1854).
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