Structure & Physiography Class 11 Geography

Introduction

• The Earth has a long history, about 4.6 billion years old.
• Its landforms have changed over time due to two main forces: endogenic (inside) and exogenic (outside).
• Millions of years ago, the Indian plate was south of the equator and larger, including the Australian plate.
• Over time, the Indian plate moved north while the Australian plate went southeast.
• The Indian plate is still moving north, affecting the environment of the Indian subcontinent.
• The northward movement of the Indian plate has several important consequences for the region.

• The current geological structure and geomorphological processes in the Indian subcontinent have resulted from the interaction of endogenic and exogenic forces and lateral plate movements.

• India can be classified into three main geological divisions based on its geological structure and formations:
  (i) The Peninsular Block
  (ii) The Himalayas and other Peninsular Mountains
  (iii) The Indo-Ganga-Brahmaputra Plain

The Peninsular Block

The Himalayas And Other Peninsular Mountains

•  The Himalayas and other Peninsular mountains are young, weak, and flexible in their geological structure, contrasting with the rigid and stable Peninsular Block.
• These mountains continue to be influenced by both exogenic (external) and endogenic (internal) forces, leading to the formation of geological features such as faults, folds, and thrust plains.
•  The mountains are of tectonic origin and are characterized by fast-flowing rivers that are still in their youthful stage.
• Common landforms associated with this stage include:
  (i) Gorges
  (ii) V-shaped valleys
  (iii) Rapids
  (iv) Waterfalls

Indo-Ganga-Brahmaputra Plain

• The third geological division of India consists of the plains formed by the Indus, Ganga, and Brahmaputra rivers.
• This region was originally a geo-synclinal depression that reached its maximum development during the third phase of the Himalayan mountain formation, approximately 64 million years ago.
• Since that time, the depression has been gradually filled with sediments carried by both Himalayan and Peninsular rivers. The average depth of alluvial deposits in these plains ranges from 1,000 to 2,000 meters.
•  The relief and physiography of India have been profoundly shaped by the geological and geomorphological processes active within the subcontinent.

Physiography

The physiography of an area results from its structure, process, and stage of development.

• Diversity of Physical Features:
  India exhibits great diversity in its physical landscape:
  (i) North India: Characterized by rugged topography, including a series of mountain ranges with varied peaks, beautiful valleys, and deep gorges.
  (ii) South India: Features stable tablelands with highly dissected plateaus, denuded rocks, and developed scarps.
  (iii) Central Region: Contains the vast North Indian Plain, situated between the northern mountains and southern plateaus.
• Physiographic Divisions of India:
  (i) The Northern and North-eastern Mountains
  (ii) The Northern Plain
  (iii) The Peninsular Plateau
  (iv) The Indian Desert
  (v) The Coastal Plains
  (vi) The Islands

The North and Northeastern Mountains

• The North and Northeastern Mountains are comprised of the Himalayas and the Northeastern hills.
• The Himalayas feature a series of parallel mountain ranges.
  (i) Greater Himalayan Range (also known as the Great Himalayas)
  (ii) Shiwalik Range
• The general orientation of these ranges in northwestern India is from northwest to southeast.
• In the Darjeeling and Sikkim regions, the Himalayas run in an east-west direction.
• In Arunachal Pradesh, they extend from southwest to northwest.

  In Nagaland, Manipur, and Mizoram, the ranges run in a north-south direction.

• The Great Himalayan Range (central axial range) is approximately 2,500 km long (east to west) and 160-400 km wide (north to south).

• The Himalayas act as a barrier, separating the Indian subcontinent from Central and East Asian countries.

• Beyond being a physical barrier, the Himalayas also serve as a climatic, drainage, and cultural divide.

The Northern Plains

• The northern plains are created by alluvial deposits from the Indus, Ganga, and Brahmaputra rivers.
•  They stretch about 3,200 km from east to west, with an average width of 150-300 km.
• Alluvial deposits can reach depths of 1,000-2,000 m.
•  Zoning of the Plains
  (a) Bhabar
  (i)  A narrow belt (8-10 km) parallel to the Shiwalik foothills.
  (ii) Streams from the mountains deposit rocks and boulders; rivers may disappear here.
  (b) Tarai
  (i) Located south of Bhabar, approximately 10-20 km wide.
  (ii) Streams re-emerge, creating marshy areas with rich natural vegetation and diverse wildlife.
  (c) Alluvial Plains
  (i)  Bhangar - Older alluvial deposits.
  (ii) Khadar -  Newer alluvial deposits.
• The plains exhibit features like sand bars, meanders, oxbow lakes, and braided channels.
• The Brahmaputra plains are noted for riverine islands and sand bars, often subject to flooding and shifting courses.
• The river mouths form significant deltas, such as the Sunderbans delta.
•  The plains are generally flat, with an elevation of 50-150 m above sea level.
• Haryana and Delhi serve as a water divide between the Indus and Ganga river systems.
• The Brahmaputra flows from northeast to southwest, turning sharply southward at Dhubri before entering Bangladesh.
•  The fertile alluvial soil supports crops like wheat, rice, sugarcane, and jute, sustaining a large population.

The Peninsular Plateau

The Structure and Physiology of the Peninsular Plateau

The Deccan Plateau

The Deccan Plateau

The Central Highlands

• The region is bounded to the west by the Aravali Range.
• The SATPURA Range consists of scarped plateaus at elevations ranging from 600-900 m above sea level, marking the northern boundary of the Deccan Plateau.
• This range is a classic example of relict mountains, characterized by significant erosion and discontinuous formations.
• The Peninsular Plateau extends to Jaisalmer in the west, where it features longitudinal sand ridges and crescent-shaped sand dunes known as barchans.
• The area has experienced metamorphic processes, indicated by the presence of metamorphic rocks such as marble, slate, and gneiss.
• The Central Highlands have an elevation between 700-1,000 m above sea level and slope towards the north and northeast.
• Most tributaries of the Yamuna River originate in the Vindhyan and Kaimur Ranges.
• The Banas River is the only significant tributary of the Chambal River that starts from the Aravali in the west.
• The Rajmahal Hills form an eastern extension of the Central Highlands, with a significant reserve of minerals located in the Chotanagpur Plateau.

The Northeastern Plateau

• The Meghalaya Plateau is an extension of the main Peninsular Plateau.
• A significant fault was created between the Rajmahal Hills and the Meghalaya Plateau due to the northeastward movement of the Indian plate during the Himalayan formation.
• This fault later filled with sediment from various rivers.
• Currently, the Meghalaya and Karbi Anglong Plateaus are separated from the main Peninsular Block.
• The Meghalaya Plateau is subdivided into three regions, Garo Hills, Khasi Hills, Jaintia Hills.
• These hills are named after the tribal groups that inhabit the area.
• An extension of the Meghalaya Plateau is found in the Karbi Anglong Hills of Assam.
• Similar to the Chotanagpur Plateau, the Meghalaya Plateau is rich in minerals, including coal, iron ore, sillimanite, limestone, and uranium.
• This region receives heavy rainfall from the southwest monsoon, leading to a highly eroded surface.
• Cherrapunji features a rocky terrain with little to no permanent vegetation cover.

The Indian Desert

• The Great Indian Desert is located northwest of the Aravali Hills.
• Characterized by undulating terrain, it features longitudinal dunes and barchans.
• Receives low annual rainfall, below 150 mm, resulting in an arid climate and minimal vegetation cover.
• Due to these characteristics, it is also referred to as Marusthali.
• Geological evidence indicates that this region was underwater during the Mesozoic era, supported by findings at the Aakal Fossil Park and marine deposits near Brahmsar (wood fossils are approximately 180 million years old).
• While the desert's underlying rock structure is an extension of the Peninsular Plateau, extreme aridity has shaped its surface through physical weathering and wind action.

The Indian Dessert

• Notable desert features include mushroom rocks, shifting dunes, and oases (mainly in the southern region).
• The desert can be divided based on orientation: the northern part slopes towards Sindh and the southern part towards the Rann of Kachchh.
• Most rivers in this area are ephemeral, with the Luni River being significant in the southern desert.
• The region experiences low precipitation and high evaporation, leading to water scarcity.
• Some streams disappear after a short distance, creating typical cases of inland drainage as they flow into lakes or playas.
• The lakes and playas contain brackish water, which serves as the main source for salt extraction.

The Coastal Plains

India has an extensive coastline, which can be divided into two main types based on location and geomorphological processes:

• Western Coastal Plains
• Eastern Coastal Plains

(i) Western Coastal Plains

• This area is an example of a submerged coast.
• The city of Dwaraka, once part of the mainland, is now underwater.
• The western coast is narrow and ideal for ports and harbors.

• Important Ports:
  1. Kandla
  2. Mazagaon
  3. JLN Port Navha Sheva
  4. Marmagao
  5. Mangalore
  6. Cochin

• Geographical Divisions:
  1. Kachchh and Kathiawar coast (Gujarat)
  2. Konkan coast (Maharashtra)
  3. Goan coast (Goa)
  4. Malabar coast (Karnataka and Kerala)

• The plains are narrow in the middle and wider towards the north and south.

•  Rivers here do not create deltas.

• Known for 'Kayals' (backwaters) used for fishing, navigation, and tourism. The famous Nehru Trophy Vallamkali (boat race) occurs in Punnamada Kayal, Kerala.

(ii) Eastern Coastal Plains

• Broader than the western coastal plains; classified as an emergent coast. Well-developed deltas formed by eastward-flowing rivers into the Bay of Bengal.
• Major Deltas are the Mahanadi, the Godavari, the Krishna and the Kaveri.
• Due to its emergent nature, fewer ports and harbors compared to the west. Continental shelf extends up to 500 km, complicating port development.
• Notable ports along the eastern coast includes Chennai, Visakhapatnam, Kolkata and Paradip.
  Chennai
  Visakhapatnam
  Kolkata
  Paradip

The Islands

India has two significant island groups:

• Bay of Bengal Islands
• Arabian Sea Islands