Geography Set 9 | MROY Class

Geography Set 9

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πŸ“Œ Indian Geography β€’ Flood Control

Q.1) The National Flood Control Programme consists of three distinct phases. Which phase lasts for five years and emphasizes the improvement of surface drainage and the establishment of effective flood warning systems?

Ans > The Short-Term Phase
  • Explanation: The Short-Term Phase lasts for the next five years following the Immediate Phase. In this phase, there is an emphasis on the improvement of surface drainage, establishment of effective flood warning systems, shifting or raising of villages above flood level, and the construction of diversion channels and embankments.
  • Genesis of the 1954 Flood Policy: The National Flood Control Programme was launched in 1954 after disastrous floods devastated several parts of the country. This marked a watershed moment where the Government shifted from ad-hoc relief measures to a comprehensive, phased strategy involving immediate relief, medium-term infrastructure, and long-term ecological balance.
πŸ“Œ Indian Geography β€’ Flood Control

Q.2) Under the National Flood Control Programme, the construction of dams, storage reservoirs, and soil conservation in the catchment areas of main rivers are activities designated to which phase?

Ans > The Long-Term Phase
  • Explanation: The Long-Term Phase includes the construction of dams and storage reservoirs, digging large diversion channels, taking suitable steps for land-use improvement, and soil conservation in the catchment area of the main river and its tributaries.
  • Strategic Shift to Catchment Management: This long-term vision aims to treat the source of rivers through extensive soil conservation and afforestation to reduce sediment load and slow surface runoff before it reaches the plains.
πŸ“Œ Indian Geography β€’ Policies

Q.3) To overcome the problem of floods through a holistic view across the country, the Government of India established which of the following commissions?

Ans > National Flood Commission (Rashtriya Barh Ayog)
  • Explanation: In order to overcome the problem of floods in the country, the Government of India set up the National Flood Commission (Rashtriya Barh Ayog). This Commission took a holistic view of the flood problem.
  • Establishment and Mandate: Established by the Ministry of Agriculture and Irrigation in 1976. Its primary mandate was to conduct a comprehensive evaluation of the flood control measures undertaken since 1954 and evolve an integrated approach to the flood problem.
πŸ“Œ Indian Geography β€’ Vegetation

Q.4) According to the spatial distribution of vegetation in India, the floristic region of the Indus Plain is characterized by which of the following main tree species that can bear severe drought conditions?

Ans > Acacias, cacti, wild-palms, and khejra
  • Explanation: The Indus Plain floristic region’s vegetation can bear arid and severe drought conditions. Acacias, cacti, wild-palms, khejra, and palas, etc. are the main trees of this region.
  • Ecological Importance of Khejri: The Khejri tree (Prosopis cineraria) is the defining keystone species of this arid landscape, honored as the state tree of Rajasthan, providing essential fodder and binding the loose sandy soil.
πŸ“Œ Indian Geography β€’ Vegetation

Q.5) Stretching all along the western coast from the Gulf of Khambat (Cambay) to Cape Comorin (Kanyakumari), the Malabar Region features which types of natural vegetation?

Ans > Moist tropical evergreen to broad-leafed mixed and monsoon deciduous type
  • Explanation: In the Malabar Region, the vegetation type ranges from moist tropical evergreen to broad-leafed mixed and monsoon deciduous type.
  • Influence of the Monsoon: The Malabar coast, backed by the Western Ghats, receives heavy orographic rainfall (often >250 cm annually) sustaining incredibly dense, multi-tiered evergreen forests and high biodiversity.
πŸ“Œ Indian Geography β€’ General

Q.6) What is the stated total geographical area of India according to the provided text?

Ans > 32,87,263 sq km
  • Explanation: The total geographical area of India is exactly 32,87,263 sq km, of which about 6,75,500 sq km is under forests.
  • Global Standing: India is the seventh-largest country in the world by land area, accounting for roughly 2.4% of the earth’s total surface area, while supporting over 17% of the global human population.
πŸ“Œ Indian Geography β€’ Forestry

Q.7) When comparing the per capita forest area, India stands at a significant deficit compared to the global average. What is the per head forest area in India versus the world average?

Ans > 0.07 hectare against 1.10 hectares
  • Explanation: The per head forest area in India is only 0.07 hectare as against the world average of 1.10 hectares.
  • The Demographic Pressure: This extraordinarily low per capita forest area is primarily a mathematical consequence of the country’s massive population of over 1.4 billion people, exacerbated by historical deforestation.
πŸ“Œ Indian Geography β€’ Forests

Q.8) Which specific type of Indian forest typically consists of tall teak trees mixed with sal, bamboos, and shrubs growing closely together to form thickets?

Ans > Tropical Moist Deciduous Forests
  • Explanation: The typical landscape of Tropical Moist Deciduous Forests consists of tall teak trees with sal, bamboos, and shrubs growing fairly close together to form thickets.
  • Commercial Timber Hub: Thriving in moderate to high annual rainfall (100 to 200 cm), these forests are the backbone of India’s timber economy, housing prized hardwood species like Teak and Sal.
πŸ“Œ Indian Geography β€’ Forests

Q.9) Tropical Thorny Forests are generally found in arid and semi-arid regions where the average annual rainfall is less than 70 cm and the average annual temperature varies between:

Ans > 25Β°C and 30Β°C
  • Explanation: Tropical Thorny Forests occur in regions characterized by low rainfall and high heat, with the average annual temperature typically ranging between 25Β°C and 30Β°C.
  • Flora Adaptations: Plants like Neem, Babul, and succulents form stunted, scattered bushes with deeply modified thorny or tiny leaves to survive the massive evaporation rates of regions like western Rajasthan and Gujarat.
πŸ“Œ Indian Geography β€’ Forestry

Q.10) Which of the following is the dominant tree species in the Subtropical Montane Forests of the north-western Himalayas (excluding Ladakh and Kashmir)?

Ans > Chir (pine)
  • Explanation: In the Subtropical Montane Forests, Chir (pine) is the main tree, although broad-leaved trees like oak, jamun, and rhododendron are also found in these areas.
  • Socio-Economic Importance: The robust, fast-growing Chir Pine thrives at mid-elevations (1000–2000m) and is heavily tapped by local communities to extract oleoresin, refined into turpentine oil and rosin.
πŸ“Œ Indian Geography β€’ Forests

Q.11) Characterized by closed and uneven canopies that permit enough light for grasses and climbers to grow on the ground level, which forest type is typically found in areas with 70–100 cm annual rainfall?

Ans > Dry Deciduous Forests
  • Explanation: Dry Deciduous Forests represent a transition between moist deciduous and thorn forests, characterized by closed/uneven canopies permitting light for grasses, found in 70–100 cm rainfall zones.
  • Vulnerability to Fire: The structural openness creates a dense undergrowth of sun-dried grasses, making these forests highly susceptible to devastating forest fires during the long dry spells.
πŸ“Œ Indian Geography β€’ Montane Ecology

Q.12) In the Himalayan mountain system, the Himalayan Moist Forests (wet temperate type) typically occupy a specific altitudinal belt that varies between:

Ans > 1000 and 2000 metres
  • Explanation: The wet temperate type of the Himalayan Moist Forests is generally found in a belt where the altitude varies between 1000 and 2000 metres.
  • Moisture Dynamics: This specific altitudinal belt frequently intercepts monsoon clouds, resulting in high humidity, mists, and heavy rainfall, nurturing rich evergreen broad-leaved trees and epiphytes.
πŸ“Œ Indian Geography β€’ Rainfall

Q.13) The Montane Wet Temperate Forests of the Himalayas, which contain species like oak, fir, and spruce, are located in areas where the mean annual rainfall is between:

Ans > 100 to 250 cm
  • Explanation: The Montane Wet Temperate Forests are found in areas where the mean annual rainfall is between 100 to 250 cm.
  • Ecological Significance: The dense mix of coniferous and broad-leaved species in these wet forests acts as a massive sponge, heavily regulating the water flow for major Himalayan rivers entering the northern plains.
πŸ“Œ Indian Geography β€’ Tree Species

Q.14) Which Himalayan tree, growing between 900 m and 1800 m, yields light and reddish-brown wood used for making tea-boxes, as well as providing resins, gums, and turpentine oils?

Ans > Chir (Pinus Longifolia)
  • Explanation: Chir (Pinus Longifolia) occurs between 900 m and 1800 m. Its light, reddish-brown wood is used for tea-boxes, and it yields valuable commercial resins.
  • Fire Ecology: Adapted to rocky Himalayan slopes, its thick bark withstands low-intensity ground fires, which help clear competing undergrowth and promote seed germination.
πŸ“Œ Indian Geography β€’ Flora

Q.15) Along the Himalayas from Chumbi Valley to Sikkim, which tree produces a moderately hard, pink-colored wood that is useful for doors and furniture, while also yielding resins?

Ans > Blue-Pine (Pinus Excelsa)
  • Explanation: Blue-Pine (Pinus Excelsa) wood is pink, moderately hard, and of good quality, widely used for doors, windows, and furniture, while also yielding resins.
  • Ecology: Growing slightly higher (1800m-3000m) than the Chir pine, it is an aggressive colonizer of disturbed or landslide-cleared soils, heavily stabilizing steep mountain slopes.
πŸ“Œ Indian Geography β€’ Timber

Q.16) The wood of Silver-fir (Abies), found in the north-western and north-eastern Himalayas, is soft but not very durable. What is it predominantly used for?

Ans > Planking, packing boxes, wood-pulp, and match sticks
  • Explanation: Silver-fir (Abies) is soft but not very durable; it is mostly used for planking, packing boxes, wood-pulp, paper, and match sticks.
  • High Altitude Adaptation: It grows at 2,200–3,300 meters near the tree line. While structurally weak and unsuitable for heavy construction, its soft, long-fibered structure is highly valuable to the paper and matchstick industries.
πŸ“Œ Indian Geography β€’ Hardwoods

Q.17) Which fine and attractive wood, predominantly found in Kashmir and Himachal Pradesh, does not shrink or swell once dried and is highly prized for making musical instruments and gun-butts?

Ans > Walnut (Juglans Regia)
  • Explanation: Walnut (Juglans Regia) is fine and attractive. Once dried it does not shrink, swell, or split, making it ideal for musical instruments, gun-butts, and cabinet works.
  • Exceptional Wood Stability: Its incredible dimensional stability, resisting changes in humidity, combined with an attractive grain, makes it the cornerstone of the famous Kashmiri wood-carving industry.
πŸ“Œ Indian Geography β€’ Flora uses

Q.18) The White Willow (Salix Alba) tree provides materials for multiple uses. While its twigs are used for making baskets, what is its wood primarily famous for?

Ans > Making cricket bats and sports goods
  • Explanation: The twigs of the White Willow (Salix Alba) are used for baskets, while the highly valued wood is famously used for making cricket bats and sports goods.
  • The Cricket Bat Industry: Heavily cultivated in the cold, riverine climates of Kashmir, the “Kashmir Willow” possesses extreme toughness and shock absorption without splintering, making it ideal for professional-grade cricket bats.
πŸ“Œ Indian Geography β€’ River Links

Q.19) The Chambal Link Canal Project aims to construct a 500 km canal to provide water to the central parts of Rajasthan. It proposes to connect the Chambal River with which other major canal system?

Ans > Indira Gandhi Canal
  • Explanation: A proposed ~500 km canal connecting the Chambal River with the Indira Gandhi Canal aims to provide desperately needed water to the central arid parts of Rajasthan.
  • The River Interlinking Vision: Part of the National Perspective Plan, the project transfers surplus seasonal floodwaters from the Chambal basin in the east directly into the parched desert core of western Rajasthan via the existing Indira Gandhi network.
πŸ“Œ Indian Geography β€’ River Projects

Q.20) The Narmada Link Canal project proposes to build a terminal storage dam across the Narmada River near Navagam. Which drought-prone regions will this canal directly benefit?

Ans > Kachchh (Gujarat) and western Rajasthan
  • Explanation: The Narmada Link Canal proposes a diversion canal from the terminal dam near Navagam to supply the severely drought-prone regions of Kachchh (Gujarat) and western Rajasthan.
  • Lifeline for Arid Regions: Driven by the Sardar Sarovar Dam, this colossal concrete-lined canal transports Narmada water hundreds of kilometers to historically parched areas, drastically reducing drought-induced distress migration.
πŸ“Œ Indian Geography β€’ Climate

Q.21) In stark contrast to Mawsynram’s extreme rainfall, what is the reported average annual rainfall in the desert region of Ganganagar?

Ans > 20 cm
  • Explanation: While Mawsynram receives over 1000 cm of rainfall annually, the average annual rainfall in Ganganagar is a meager 20 cm.
  • Agricultural Paradox: Despite experiencing some of India’s highest summer temperatures and lowest rainfall, Ganganagar is transformed into the “food basket of Rajasthan” entirely through intense canal irrigation systems like the Indira Gandhi Canal.
πŸ“Œ Indian Geography β€’ Hydrology

Q.22) To alleviate the water needs of drought-prone areas in Tamil Nadu, the Periyar Diversion Scheme redirects surplus water through a tunnel across which mountain range?

Ans > Sahyadri (Western Ghats)
  • Explanation: The Periyar Diversion Scheme collects the surplus water of the west-flowing Periyar river and diverts it through a tunnel across the Sahyadri (Western Ghats) to Tamil Nadu in the east.
  • Trans-Basin Water Transfer: Built in the late 19th century around the Mullaperiyar Dam, this historic engineering feat artificially forces a west-flowing river to cross the massive topographic barrier of the rain-drenched Western Ghats to supply the arid eastern rain shadow.
πŸ“Œ Geomorphology β€’ Rivers

Q.23) Which tributary of the Brahmaputra River presents a classic example of river capturing by taking over the waters of the Meghna river of Bangladesh?

Ans > Kapili
  • Explanation: Kapili, a tributary of the Brahmaputra, captured the waters of the Meghna river of Bangladesh, demonstrating the geomorphic process of river capturing.
  • Tectonic Influences: Facilitated by the tectonic uplift of the Shillong Plateau, the Kapili River aggressively eroded backwards (headward erosion), breaching the drainage divide and stealing the upper reaches of the Meghna.
πŸ“Œ Geomorphology β€’ Landforms

Q.24) Which geographical feature serves as physical evidence of the abandoned valley created after the Kapili River captured the waters of the Meghna River?

Ans > Lumding-Halflong Pass
  • Explanation: The Lumding-Halflong Pass serves as geological evidence of the abandoned valley left behind after the Kapili river captured the headwaters of the Meghna.
  • Understanding Abandoned Valleys: A wide, U-shaped “wind gap” without a corresponding stream proves a massive volume of water once flowed there. British engineers later utilized this naturally flat, eroded corridor to build a critical railway line.
πŸ“Œ Geomorphology β€’ Himalayas

Q.25) According to geologists, the Tsangpo river over Tibet historically took an easterly course and joined which major river system before headward erosion altered its path?

Ans > Irrawaddy River (Myanmar)
  • Explanation: During early days, the Tsangpo over Tibet took an easterly course and used to join the Irrawaddy River (Myanmar) through the Chindwin.
  • The Great Bend: This ancient route was violently severed by the tectonic uplift of the eastern Himalayas (Namcha Barwa), forcing the river into a 180-degree hairpin bend southward into India to form the modern Brahmaputra system.
πŸ“Œ Hydrology β€’ Punjab Rivers

Q.26) Traces of abandoned river channels between Montgomery and Multan demonstrate that which river drastically changed its old course about 250 years ago to join the Satluj near Sultanpur?

Ans > Beas
  • Explanation: About 250 years ago the Beas river changed its old courseβ€”traces of which remain between Montgomery and Multanβ€”and joined the Satluj river near Sultanpur.
  • Dynamic Plains: The incredibly low gradient of the Indo-Gangetic plains makes rivers highly unstable. Around 1790, heavy flooding and sedimentation blocked the Beas’s original path to the Chenab, forcing it to merge with the Sutlej instead.
πŸ“Œ Hydrology β€’ Brahmaputra

Q.27) Historical hydrological records indicate that about 250 years ago, the Brahmaputra river flowing through Mymensingh naturally discharged its waters into which river?

Ans > Meghna River
  • Explanation: About 250 years ago, the Brahmaputra flowing through Mymensingh was discharging its massive waters directly into the Meghna River.
  • The 1787 Tipping Point: A catastrophic flood and earthquake caused the Teesta River to dump its massive sediment load into the Brahmaputra, choking the old channel through Mymensingh and forcing the river to carve a new path south.
πŸ“Œ Hydrology β€’ Delta

Q.28) Following tectonic and depositional shifts, the Brahmaputra river straightened its course and joined the Ganga (Padma) River to form a massive new stream known as:

Ans > Jamuna
  • Explanation: In due course, the Brahmaputra straightened its course southward and joined the Ganga (Padma) River, forming a colossal new stream called the Jamuna.
  • Braided River Characteristics: Carrying a gargantuan load of Himalayan sediment, the relatively young Jamuna is a highly unstable braided river, creating temporary sand islands (chars) in a channel up to 15km wide during monsoons.
πŸ“Œ Tectonics β€’ Northern Plains

Q.29) The shifting of river courses in the northern plains of India is attributed to several geomorphic phenomena. Which of the following tectonic uplifts is noted as a primary cause for these river shifts?

Ans > Upliftment of the Potwar Plateau (Delhi-Sirhind Plateau)
  • Explanation: The shifting of river courses is prominently caused by the upliftment of the Potwar Plateau (Delhi-Sirhind Plateau), along with the downwarping of the Malda Gap.
  • The Great Drainage Divide: Acting as the master drainage divide, the slow tectonic tilting of the Delhi Ridge over millennia separated the Indus (west) and Ganga (east) basins, and is believed to have caused the drying of the legendary Saraswati river.
πŸ“Œ Geology β€’ Plateaus

Q.30) The Chotanagpur Plateau is a complex geological formation sprawling over parts of West Bengal, Jharkhand, and Chhattisgarh. It is predominantly composed of which basal rock types?

Ans > Archaean granite and gneiss with patches of Dharwar rocks
  • Explanation: The Chotanagpur Plateau is fundamentally composed of ancient Archaean granite and gneiss rocks with patches of highly metalliferous Dharwar (mica-schists) rocks, as well as Gondwana coal basins.
  • The Mineral Heartland: As one of the oldest, most stable landmasses (the Peninsular Shield), the inclusion of Dharwar rocks makes this plateau the “Ruhr of India,” holding the nation’s richest reserves of iron ore, copper, and mica.

πŸ“Œ Quick Summary β€” Geography Set 9

  • Flood Control Phase: The Short-Term Phase lasts 5 years, focusing on surface drainage and warning systems.
  • Catchment Management: The Long-Term Phase focuses on dams and soil conservation.
  • Rashtriya Barh Ayog: The National Flood Commission set up to take a holistic view of floods.
  • Indus Plain Flora: Acacias, cacti, and the vital Khejri tree endure extreme droughts.
  • Malabar Region: Experiences heavy orographic rain, resulting in moist tropical evergreen forests.
  • Area of India: The stated geographical area is exactly 32,87,263 sq km.
  • Forest Area Deficit: India’s per capita forest area is only 0.07 hectare compared to the global 1.10.
  • Valuable Hardwoods: Teak and Sal are prominently found in Tropical Moist Deciduous Forests.
  • Thorny Forests: Found in arid regions (<70 cm rain) with intense 25Β°C-30Β°C average heat.
  • NW Himalayan Flora: Chir (pine) dominates the Subtropical Montane Forests (1000-2000m).
  • Dry Deciduous Vulnerability: Uneven canopies allow grass undergrowth, making them highly prone to fire.
  • Wet Temperate Belt: Himalayan Moist Forests typically grow between altitudes of 1000m and 2000m.
  • Montane Wet Temperate: Thrive in specific high-altitude belts receiving 100-250 cm rainfall.
  • Resin & Packaging: The Chir Pine is famous for light wood (tea boxes) and turpentine.
  • Blue-Pine: High altitude pine yielding pink-colored wood favored for furniture.
  • Silver-Fir: Very soft wood; critical for match sticks and paper pulp industries.
  • Kashmiri Walnut: Highly dimensionally stable wood prized for gun-butts and instruments.
  • White Willow: Moisture-loving tree in Kashmir explicitly used for high-grade cricket bats.
  • Canal Interlinking: The Chambal Link project aims to feed central Rajasthan via the Indira Gandhi Canal.
  • Narmada Distribution: Navagam Dam canals aim to resolve Kachchh and western Rajasthan droughts.
  • Arid Extremes: Ganganagar desert receives only 20 cm rainfall annually despite being a food bowl.
  • Periyar Tunnel: Routes surplus Kerala water through the Sahyadri mountains into arid Tamil Nadu.
  • River Capturing: The Kapili river successfully captured the headwaters of the Meghna.
  • Wind Gaps: Lumding-Halflong Pass is physical evidence of an abandoned river valley.
  • Tsangpo History: Ancient Tibetan Tsangpo once flowed east into Myanmar’s Irrawaddy before tectonic shifts.
  • Dynamic Plains: The Beas shifted course 250 years ago, abandoning channels near Multan.
  • Brahmaputra Shift: In 1787, floods forced it out of its Mymensingh channel (joining Meghna).
  • The Jamuna Creation: The straight, new massive channel of the Brahmaputra merging with the Ganga.
  • Drainage Divide: The tectonic uplift of the Potwar (Delhi-Sirhind) Plateau permanently separated Indus and Ganga.
  • Peninsular Shield: Chotanagpur Plateau holds India’s mineral wealth in Archaean granite and Dharwar rocks.
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