Notes of Ch 2 Structure and Physiography| Class 11th Geography


• The earth is approximately 460 million years old.

• Over these long years, it has undergone many changes brought about primarily by the endogenic and exogenic forces.

• These forces have played a significant role in giving shape to various surface and subsurface features of the earth.

• The Indian plate which was to the south of the equator millions of years ago was much larger in size and the Australian plate was a part of it.

• Over millions of years, this plate broke into many parts and the Australian plate moved towards the south eastern direction and the Indian plate to the north.

• This northward movement of the Indian plate is still continuing and it has significant consequences on the physical environment of the Indian subcontinent.

• It is primarily through the interplay of these endogenic and exogenic forces and lateral movements of the plates that the present geological structure and geomorphologic processes active in the Indian subcontinent came into existence.

• Based on the variations in its geological structure and formations, India can be divided into three geological divisions. These geological regions broadly follow the physical features:
(i) The Penisular Block
(ii) The Himalayas and other Peninuslar Mountains
(iii) Indo-Ganga-Brahmaputra Plain. 

The Peninsular Block

• The northern boundary of the Peninsular Block - line running from Kachchh along the western flank of the Aravali Range near Delhi and then roughly parallel to the Yamuna and the Ganga as far as the Rajmahal Hills and the Ganga delta.

• Karbi Anglong and the Meghalaya Plateau in the northeast and Rajasthan in the west are also extensions of this block.

• The northeastern parts are separated by the Malda fault in West Bengal from the Chotanagpur plateau.

• In Rajasthan, the desert and other desert—like features overlay this block.

• The Peninsula is formed by a great complex of very ancient gneisses and granites, which constitutes a major part of it.

• As a part of the Indo-Australian Plate, it has been subjected to various vertical movements and block faulting.

• The rift valleys of the Narmada, the Tapi and the Mahanadi and the Satpura block mountains are some examples of it.

• The Peninsula mostly consists of relict and residual mountains like the Aravali hills, the Nallamala hills, the Javadi hills, the Veliconda hills, the Palkonda range and the Mahendragiri hills, etc.

• The river valleys here are shallow with low gradients.

• Most of the east flowing rivers form deltas before entering into the Bay of Bengal.

• The deltas formed by the Mahanadi, the Krishna, the Kaveri and the Godavari are important examples.

The Himalayas And Other Peninsular Mountains

• The Himalayas along with other Peninsular mountains are young, weak and flexible in their geological structure unlike the rigid and stable Peninsular Block.

• These mountains are tectonic in origin, dissected by fast-flowing rivers which are in their youthful stage.

• Various landforms like gorges, V-shaped valleys, rapids, waterfalls, etc. are indicative of this stage.

Indo-ganga-brahmaputra Plain

• The third geological division of India comprises the plains formed by the river Indus, the Ganga and the Brahmaputra.

• Originally, it was a geo-synclinal depression which attained its maximum development during the third phase of the Himalayan mountain formation approximately about 64 million years ago.

• Since then, it has been gradually filled by the sediments brought by the Himalayan and Peninsular rivers.

• Average depth of alluvial deposits in these plains ranges from 1,000­2,000 m.

• The relief and physiography ofIndia has been greatly influenced by the geological and geomorphological processes active in the Indian subcontinent.


• ‘Physiography’ of an area is the outcome ofstructure, process and the stage of development.

• The north has a vast expanse of rugged topography consisting of a series of mountain ranges with varied peaks, beautiful valleys and deep gorges.

• The south consists of stable table land with highly dissected plateaus, denuded rocks and developed series of scarps.

• In between these two lies the vast north Indian plain.

Based on these macro variations, India can be divided into the following physiographic divisions:
(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 consist of the Himalayas and the Northeastern hills.

• The Himalayas consist of a series of parallel mountain ranges.

• Some of the important ranges are the Greater Himalayan range, which includes the Great Himalayas and the Trans-Himalayan range, the Middle Himalayas and the Shiwalik.

• The general orientation of these ranges is from northwest to the southeast direction in the northwestern part of India.

• Himalayas in the Darjiling and Sikkim regions lie in an eastwest direction, while in Arunachal Pradesh they are from southwest to the northwest direction.

• In Nagaland, Manipur and Mizoram, they are in the north south direction.

• The approxiate length of the Great Himalayan range, also known as the central axial range, is 2,500 km from east to west, and their width varies between 160-400 km from north to south.

• The Himalayas stand almost like a strong and long wall between the Indian subcontinent and the Central and East Asian countries.

• Himalayas are not only the physical barrier, they are also a climatic, drainage and cultural divide.

• Himalayas can be divided into the following sub-divisions:
(i) Kashmir or Northwestern Himalayas
(ii) Himachal and Uttaranchal Himalayas
(iii) Darjiling and Sikkim Himalayas
(iv) Arunachal Himalayas
(v) Eastern Hills and Mountains

Kashmir or Northwestern Himalayas

• It comprise a series of ranges such as the Karakoram, Ladakh, Zaskar and Pir Panjal.

• The northeastern part of the Kashmir Himalayas is a cold desert, which lies between the Greater Himalayas and the Karakoram ranges.

• Between the Great Himalayas and the Pir Panjal range, lies the world famous valley of Kashmir and the famous Dal Lake.

• Important glaciers of South Asia such as the Baltoro and Siachen are also found in this region.

• The Kashmir Himalayas are also famous for Karewa formations, which are useful for the cultivation of Zafran, a local variety of saffron.

• Some of the important passes of the region are Zoji La on the Great Himalayas, Banihal on the Pir Panjal, Photu La on the Zaskar and Khardung La on the Ladakh range.

• Some of the important fresh lakes such as Dal and Wular and salt water lakes such as Pangong Tso and Tso Moriri are also in this region.

• This region is drained by the river Indus, and its tributaries such as the Jhelum and the Chenab.

• Jhelum in the valley of Kashmir is still in its youth stage and yet forms meanders - a typical feature associated with the mature stage in the evolution of fluvial land form.

The Himachal and Uttarakhand Himalayas

• The northernmost part of the Himachal Himalayas is an extension of the Ladakh cold desert, in which all the three ranges of Himalayas are prominent.

• These are the Great Himalayan range, the Lesser Himalayas (which is locally known as Dhaoladhar in Himachal Pradesh and Nagtibha in Uttarakhand) and the Shiwalik range from the North
to the South.

• In this section of Lesser Himalayas, the altitude between 1,000-2,000 m.

• The important hill stations such as Dharamshala, Mussoorie, Shimla, Kaosani and the cantonment towns and health resorts such as Shimla, Mussoorie, Kasauli, Almora, Lansdowne and Ranikhet, etc.

• The two distinguishing features of this region from the point of view of physiography are the ‘Shiwalik’ and ‘Dun formations’. Some important duns located in this region are the the places of pilgrimage such as the Gangotri, Yamunotri, Kedarnath, Badrinathand Hemkund Sahib are also situated in this part.

• The region is also known to have five famous Prayags (river confluences).

The Darjiling and Sikkim Himalayas

• They are bordered by Nepal Himalayas in the west and Bhutan Himalayas in the east.

• It is relatively small but is a most significant part of the Himalayas.

• Known for its fast-flowing rivers such as Tista.

• It is a region of high mountain peaks like Kanchenjunga (Kanchengiri), and deep valleys.

• The higher reaches of this region are inhabited by Lepcha tribes.

The Arunachal Himalayas

• These extend from the east of the Bhutan Himalayas up to the Diphu pass in the east.

• The general direction of the mountain range is from southwest to northeast.

• Some of the important mountain peaks of the region are Kangtu and Namcha Barwa.

• These ranges are dissected by fast-flowing rivers from the north to the south, forming deep gorges.
the Bhramaputa flows through a deep gorge after crossing Namcha Barwa.

• Some of the important rivers are the Kameng the Subansiri, the Dihang, the Dibang and the Lohit.

• These are perennial with the high rate offall, thus, having the highest hydro-electric power potential in the country.

• An important aspect of the Arunachal Himalayas is the numerous ethnic tribal community inhabiting in these areas.

• Some of the prominent ones from west to east are the Monpa, Daffla, Abor, Mishmi, Nishi and the Nagas. Most of these communities practise Jhumming.

• It is also known as shifting or slash and burn cultivation.

• This region is rich in biodiversity which has been preserved by the indigenous communities.

• Due to rugged topography, the inter-valley transportation linkages are nominal.

• Hence, most of the interactions are carried through the duar region along the Arunachal-Assam border.

The Eastern Hills and Mountains

• These are part of the Himalayan mountain system having their general alignment from the north to the south direction.

• They are known by different local names. In the north, they are known as Patkai Bum, Naga hills, the Manipur hills and in the south as Mizo or Lushai hills.

• These are low hills, inhabited by numerous tribal groups practicing Jhum cultivation.

• Most of these ranges are separated from each other by numerous small rivers.

• The Barak is an important river in Manipur and Mizoram.

• The physiography of Manipur is unique by the presence of a large lake known as ‘Loktak’ lake at the centre, surrounded by mountains from all sides.

• Mizoram which is also known as the ‘Molassis basin’ which is made up of soft unconsolidated rocks.

The Northern Plains

• The northern plains are formed by the alluvial deposits brought by the rivers - the Indus, the Ganga and the Brahmaputra.

• These plains extend approximately 3,200 km from the east to the west.

• The average width of these plains varies between 150-300 km.

• The maximum depth of alluvium deposits varies between 1,000-2,000 m. From the north to the south.

• These can be divided into three major zones: the Bhabar, the Tarai and the alluvial plains.

• The alluvial plains can be further divided into the Khadar and the Bhangar.

• Bhabar is a narrow belt ranging between 8-10 km parallel to the Shiwalik foothills at the break-up of the slope.

• The streams and rivers coming from the mountains deposit heavy materials of rocks and boulders, and at times, disappear in this zone.

• South of the Bhabar is the Tarai belt, with an approximate width of 10-20 km where most of the streams and rivers re-emerge without having any properly demarcated channel,

• Marshy and swampy conditions known as the Tarai.

• This has a luxurious growth of natural vegetation and houses a varied wild life.

• The south of Tarai is a belt consisting of old and new alluvial deposits known as the Bhangar and Khadar respectively.

The Peninsular Plateau

• Irregular triangle in shape.

• Rising from the height of 150 m above the river plains up to an elevation of 600-900 m.

• Delhi ridge in the northwest, (extension of Aravalis), the Rajmahal hills in the east, Gir range in the west and the Cardamom hills in the south constitute the outer extent of the Peninsular plateau. northeast, Shillong and Karbi-Anglong plateau.

• The Peninsular India is made up of a series of patland plateaus such as the Hazaribagh plateau, the Palamu plateau, the Ranchi plateau, the Malwa plateau, the Coimbatore plateau and the Karnataka plateau, etc.

• This is one of the oldest and the most stable landmass of India.

• The general elevation of the plateau is from the west to the east.

• Narmada, tapti, Mahanadi, Godavari, Krishna, and cauvery are some of the important rivers.

• Some of the important physiographic features of this region are tors, block mountains, rift valleys, spurs, bare rocky structures, series of hummocky hills and wall-like quartzite dykes offering natural sites for water storage.

• The western and northwestern part of the plateau has an emphatic presence of black soil.

• The northwestern part of the plateau has a complex relief of ravines and gorges. The ravines of Chambal, Bhind and Morena are some of the well-known examples. On the basis of the prominent relief features, the Peninsular plateau can be divided into three broad groups:
(i) The Deccan Plateau
(ii) The Central Highlands
(iii) The Northeastern Plateau.

The Deccan Plateau

• This is bordered by the Western Ghats in the west, Eastern Ghats in the east and the Satpura, Maikal range and Mahadeo hills in the north.

• Western Ghats are locally known by different names such as Sahyadri in Maharashtra, Nilgiri hills in Karnataka and Tamil Nadu and Anaimalai hills and Cardamom hills in Kerala.

• Western Ghats are comparatively higher in elevation and more continuous than the Eastern Ghats. Their average elevation is about 1,500 m with the height increasing from north to south.

• ‘Anaimudi’ (2,695 m), the highest peak of Peninsular plateau is located on the Anaimalai hills of the Western Ghats followed by Dodabetta(2,637 m) on the Nilgiri hills.

• Most of the Peninsular rivers have their origin in the Western Ghats. Eastern Ghats comprising the discontinuous and low hills are highly eroded by the rivers such as the Mahanadi, the Godavari, the Krishna, the Kaveri, etc.

• Some of the important ranges include the Javadi hills, the Palkonda range, the Nallamala hills, the Mahendragiri hills, etc.

• The Eastern and the Western Ghats meet each other at the Nilgiri hills.

The Central Highlands

• They are bounded to the west by the Aravali range.

• The Satpura range is formed by a series of scarped plateaus on the south, generally at an elevation varying between 600-900 m above the mean sea level.

• This forms the northernmost boundary of the Deccan plateau.

• It is a classic example of the relict mountains which are highly denuded and form discontinuous ranges.

• This region has undergone metamorphic processes in its geological history, which can be corroborated by the presence of metamorphic rocks such as marble, slate, gneiss, etc.

• The general elevation of the Central Highlands ranges between 700-1,000 m.

• Banas is the only significant tributary of the river Chambal that originates from the Aravalli in the west.

• An eastern extension of the Central Highland is formed by the Rajmahal hills, to the south of which lies a large reserve of mineral resources in the Chotanagpur plateau.

The Northeastern Plateau

• It is an extension of the main Peninsular plateau.

• It is believed that due to the force exerted by the northeastward movement of the Indian plate at the time of the Himalayan origin, a huge fault was created between the Rajmahal hills and the Meghalaya plateau. Later, this depression got filled up by the deposition activity of the numerous rivers.

• The Meghalaya and Karbi Anglong plateau stand detached from the main Peninsular Block.

• The Meghalaya plateau is further sub-divided into three:
(i) The Garo Hills;
(ii) The Khasi Hills;
(iii) The Jaintia Hills,

• These are named after the tribal groups inhabiting this region.

• An extension of this is also seen in the Karbi Anglong hills of Assam.

• Rich in mineral resources like coal, iron ore, sillimanite, limestone and uranium.

• The Meghalaya plateau has a highly eroded surface.

• Cherrapunji displays a bare rocky surface devoid of any permanent vegetation cover.

The Indian Desert

• To the northwest of the Aravali hills lies the Great Indian desert.

• It is a land of undulating topography dotted with longitudinal dunes and barchans.

• This region receives low rainfall below 150 mm per year; hence, it has arid climate with low vegetation cover.

• It is because of these characteristic features that this is also known as Marusthali.

• The Luni river flowing in the southern part of the desert is of some significance.

• Low precipitation and high evaporation makes it a water deficit region.

• There are some streams which disappear after flowing for some distance and present a typical case of inland drainage by joining a lake or playa.

• The lakes and the playas have brackish water which is the main source of obtaining salt.

The Coastal Plains

• On the basis of the location and active geomorphological processes, it can be broadly divided into two:
(i) the western coastal plains;
(ii) the eastern coastal plains.

The Western coastal plains

• These are an example of submerged coastal plain.

• It is believed that the city of Dwaraka which was once a part of the Indian mainland situated along the west coast is submerged under water.

• Because of this submergence it is a narrow belt and provides natural conditions for the development of ports and harbours. Kandla, Mazagaon, JLN port Navha Sheva, Marmagao, Mangalore, Cochin, etc. are some of the important natural ports located along the west coast.

• Western coast may be divided into following divisions:
(i) the Kachchh and Kathiawar coast in Gujarat,
(ii) Konkan coast in Maharashtra,
(iii) Goan coast and Malabar coast in Karnataka and Kerala respectively.

• The rivers flowing through this coastal plain do not form any delta.

• The Malabar coast has got certain distinguishing features in the form of ‘Kayals’ (backwaters), which are used for fishing, inland navigation and also due to its special attraction for tourists. Every year the famous Nehru Trophy Vallamkali (boat race) is held in Punnamada Kayal in Kerala.

The Eastern coastal plain

• These are broader and is an example of an emergent coast.

• There are well- developed deltas here, formed by the rivers flowing eastward in to the Bay of Bengal.

• These include the deltas of the Mahanadi, the Godavari, the Krishna and the Kaveri.

• Because of its emergent nature, it has less number of ports and harbours.

• The continental shelf extends up to 500 km into the sea, which makes it difficult for the development of good ports and harbours.

The Islands

• There are two major island groups in India:
→ one in the Bay of Bengal
→ other in the Arabian Sea

The islands of the Bay of Bengal

• The Bay of Bengal island groups consist of about 572 islands/islets.

• These are situated roughly between 6°N-14°N and 92°E -94°E.

• The two principal groups of islets include the Ritchie’s archipelago and the Labrynth island. The entire group of island is divided into two broad categories — the Andaman in the north and the Nicobar in the south.

• They are separated by a water body which is called the Ten degree channel. These islands are an elevated portion of submarine mountains. However, some smaller islands are volcanic in origin.

• Barren island, the only active volcano in India is also situated in the Nicobar islands.

• The coastal line has some coral deposits, and beautiful beaches. These islands receive convectional rainfall and have an equatorial type of vegetation.

The islands of the Arabian sea

• These include Lakshadweep and Minicoy.

• These are scattered between 8°N-12°N and 71°E -74°E longitude.

• These islands are located at a distance of280 km-480 km off the Kerala coast is built of coral deposits.

• There are approximately 36 islands of which 11 are inhabited.

• Minicoy is the largest island with an area of 453 sq. km.

• The entire group of islands is broadly divided by the Eleventh degree channel, north of which is the Amini Island and to the south of the Canannore Island.

• The Islands of this archipelago have storm beaches consisting of unconsolidated pebbles, shingles, cobbles and boulders on the eastern seaboar.
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