India's Physiographic Divisions
India's physical landscape is remarkably diverse, shaped by tectonic forces, weathering, and fluvial processes over millions of years. The country can be divided into six major physiographic divisions.
Overview of Physiographic Divisions
| Division | Approximate Area | Key Feature | Geological Age |
|---|---|---|---|
| The Himalayan Mountains | ~5 lakh sq km | Young fold mountains; highest peaks | Tertiary (Cenozoic) |
| The Northern Plains | ~7 lakh sq km | Alluvial deposits of Indus-Ganga-Brahmaputra | Quaternary |
| The Peninsular Plateau | ~16 lakh sq km | Oldest landmass; igneous & metamorphic rocks | Precambrian (Archaean) |
| The Indian Desert | ~2 lakh sq km | Arid landscape; sand dunes (Thar) | Quaternary |
| The Coastal Plains | Narrow strips along coasts | Marine deposits; lagoons and deltas | Recent |
| The Islands | ~8,249 sq km | Andaman & Nicobar (tectonic); Lakshadweep (coral) | Tertiary to Recent |
The Himalayan Mountains
The Himalayas stretch in a west-east arc from the Indus to the Brahmaputra, spanning approximately 2,400 km in length and 150-400 km in width.
Longitudinal Divisions of the Himalayas
| Range | Local Name | Average Height | Width | Key Features |
|---|---|---|---|---|
| Greater Himalayas | Himadri | ~6,100 m | 25 km | Perpetual snow; peaks above 8,000 m; Kangchenjunga (8,598 m) |
| Lesser Himalayas | Himachal | 3,500-5,000 m | 60-80 km | Pir Panjal, Dhauladhar, Mussoorie Range; hill stations |
| Outer Himalayas | Shivaliks | 600-1,500 m | 10-50 km | Youngest range; composed of unconsolidated sediments; Duns |
Major Himalayan Peaks in India
| Peak | Height (m) | State/Region |
|---|---|---|
| K2 (Godwin-Austen) | 8,611 | Karakoram Range (PoK) |
| Kangchenjunga | 8,598 | Sikkim |
| Nanda Devi | 7,816 | Uttarakhand |
| Kamet | 7,756 | Uttarakhand |
| Saltoro Kangri | 7,742 | Karakoram (Ladakh) |
Regional Divisions of the Himalayas
| Region | Between | States Covered |
|---|---|---|
| Punjab/Kashmir Himalayas | Indus to Sutlej | J&K, Ladakh, Himachal Pradesh |
| Kumaon Himalayas | Sutlej to Kali | Himachal Pradesh, Uttarakhand |
| Nepal Himalayas | Kali to Tista | Nepal (international) |
| Assam Himalayas | Tista to Dihang | Sikkim, Arunachal Pradesh |
Key Himalayan Passes
| Pass | Elevation (m) | State/UT | Connects / Significance |
|---|---|---|---|
| Karakoram Pass | 5,540 | Ladakh | Highest pass in the Karakoram Range; ancient route between Leh and Yarkand |
| Zoji La | 3,528 | J&K–Ladakh | On Srinagar–Leh Highway; gateway to Ladakh |
| Rohtang Pass | 3,978 | Himachal Pradesh | Links Kullu Valley with Lahaul-Spiti; open May–November |
| Shipki La | 4,500 | Himachal Pradesh | India–Tibet trade route; one of three open trading border passes with China |
| Nathu La | 4,310 | Sikkim | India–China trading pass; reopened for border trade in 2006 |
| Bomdi La | 2,530 | Arunachal Pradesh | Strategic pass near China–Bhutan border; route to Tawang |
The Northern Plains
The Indo-Gangetic plain is formed by the alluvial deposits of the Indus, Ganga, and Brahmaputra river systems. It stretches about 2,400 km in length and 150-300 km in width.
Zones of the Northern Plains
| Zone | Description | Location |
|---|---|---|
| Bhabar | Narrow belt of pebble-studded rocks (8-16 km wide); streams disappear | Along Shivalik foothills |
| Terai | Marshy, swampy zone; dense forests; re-emergence of streams | South of Bhabar |
| Bhangar | Older alluvium; above flood level; contains kankar (calcareous nodules) | Higher terraces of river valleys |
| Khadar | Newer alluvium; renewed by annual floods; highly fertile | Flood plains of rivers |
Mnemonic: Remember the Northern Plains zones from north to south as "B-T-B-K" (Bhabar, Terai, Bhangar, Khadar). Think: "Big Tigers Bring Khaos." Also remember: Bhabar = streams disappear (porous pebbles), Terai = streams re-emerge (marshy), Bhangar = old alluvium with kankar, Khadar = new alluvium (fertile flood plains).
The Northern Plains can be regionally divided into: the Punjab Plains (Indus tributaries), the Ganga Plains (extending from Haryana to West Bengal, the most extensive section), and the Brahmaputra Plains (Assam valley). The Ganga Plains are further subdivided into the Upper Ganga Plain (Uttarakhand-UP), Middle Ganga Plain (eastern UP-Bihar), and Lower Ganga Plain (West Bengal-Bangladesh).
The Indian Desert (Thar)
The Thar Desert covers approximately 2 lakh sq km in western Rajasthan and parts of Gujarat, extending into Pakistan. It is bounded by the Aravalli Range on the east and southeast. Key features include longitudinal sand dunes (barchans), seasonal salt lakes (such as Sambhar Lake — India's largest inland salt lake), and the Luni River, the only significant river in the region. The desert receives less than 25 cm of annual rainfall. The Indira Gandhi Canal (Rajasthan Canal), originating from the Harike Barrage on the Sutlej-Beas confluence, has transformed parts of the Thar into cultivable land.
The Peninsular Plateau
The Peninsular Plateau is India's oldest and most stable landmass, composed primarily of igneous and metamorphic rocks. It is bounded by the Aravalli Range in the northwest, the Vindhya and Satpura ranges in the north, and flanked by the Western and Eastern Ghats. A significant geological feature is the Deccan Traps — layers of solidified flood basalt from massive volcanic eruptions approximately 66 million years ago (Cretaceous-Paleogene boundary). The Deccan Traps currently cover about 5 lakh sq km across west-central India and are responsible for the formation of the regur (black cotton) soil.
Sub-divisions of the Peninsular Plateau
| Sub-division | Key Features |
|---|---|
| Central Highlands | North of Narmada; includes Malwa Plateau, Bundelkhand, Baghelkhand; slope towards north |
| Deccan Plateau | South of Narmada; triangular; higher on western side; slopes eastward |
| Western Ghats | Average height 900-1600 m; continuous range; higher than Eastern Ghats |
| Eastern Ghats | Discontinuous; average 600 m; cut by Godavari, Krishna, Kaveri rivers |
Common Mistake: The Western Ghats are NOT fold mountains — they are a faulted edge (escarpment) of the Deccan Plateau, formed by down-faulting of the western coast. The Himalayas are fold mountains. UPSC frequently tests the distinction between young fold mountains, block mountains, and residual mountains. Similarly, the Aravalli Range is a residual mountain (oldest fold mountains, now heavily eroded), not a young fold mountain.
Important Peaks of Western and Eastern Ghats
| Peak | Height (m) | Range |
|---|---|---|
| Anamudi | 2,695 | Western Ghats (Kerala) |
| Dodda Betta | 2,637 | Western Ghats (Nilgiris, Tamil Nadu) |
| Mahendragiri | 1,501 | Eastern Ghats (Odisha) |
Major Rivers of India
India's rivers are classified into two major groups based on their origin: Himalayan rivers (perennial, snow-fed) and Peninsular rivers (seasonal, rain-fed). The three major Himalayan river systems — Indus, Ganga, and Brahmaputra — together drain about 60% of India's total geographical area. The Indus system (Indus + five tributaries: Jhelum, Chenab, Ravi, Beas, Sutlej) is governed by the Indus Waters Treaty (1960) between India and Pakistan, which allocates the three eastern rivers (Beas, Ravi, Sutlej) to India and the three western rivers (Indus, Jhelum, Chenab) to Pakistan. The Ganga basin is the largest river basin in India, while the Godavari is the longest peninsular river, often called the "Dakshin Ganga."
Major Rivers: Origin, Length, and Tributaries
| River | Origin | Length (km) | Drains Into | Major Tributaries |
|---|---|---|---|---|
| Ganga | Gangotri Glacier, Uttarakhand | 2,525 | Bay of Bengal | Yamuna, Ramganga, Ghaghra, Gandak, Kosi, Son, Mahananda |
| Brahmaputra | Kailash Range (Tibet) at ~5,150 m | 2,900 (total) | Bay of Bengal | Dibang, Lohit, Subansiri, Manas, Tista, Dhansiri |
| Indus | Near Mansarovar Lake, Tibet | 2,880 (709 in India) | Arabian Sea | Jhelum, Chenab, Ravi, Beas, Sutlej |
| Godavari | Trimbakeshwar, Nashik (Maharashtra) at 1,067 m | 1,465 | Bay of Bengal | Pranhita, Indravathi, Sabari, Manjira, Purna, Pravara |
| Krishna | Mahabaleshwar, Maharashtra | 1,400 | Bay of Bengal | Bhima, Tungabhadra, Koyna, Musi |
| Yamuna | Yamunotri Glacier, Uttarakhand | 1,376 | Merges with Ganga at Prayagraj | Chambal, Betwa, Ken, Sindh |
| Narmada | Amarkantak, Madhya Pradesh | 1,312 | Arabian Sea | Tawa, Hiran, Barna, Kolar |
| Kaveri | Talakaveri, Kodagu (Karnataka) | ~800 | Bay of Bengal | Hemavati, Kabini, Shimsha, Arkavati |
Drainage Patterns
| Pattern | Description | Indian Example |
|---|---|---|
| Dendritic | Tree-like branching; develops on uniform slopes | Northern Plains rivers |
| Trellis | Main stream joined by tributaries at right angles | Subarnarekha basin |
| Radial | Rivers flow outward from a central high point | Rivers originating from Amarkantak |
| Rectangular | Right-angle bends due to jointed rocks | Chambal drainage in parts |
| Centripetal | Rivers converge into a depression | Loktak Lake drainage |
Key distinction: Narmada and Tapi are the only two major peninsular rivers that flow westward into the Arabian Sea. Both flow through rift valleys (linear, fault-formed troughs), NOT ordinary valleys. This is why they do NOT form deltas — they form estuaries instead. All other major peninsular rivers (Godavari, Krishna, Kaveri, Mahanadi) flow eastward and form deltas. UPSC has directly tested this in Prelims 2013.
Interlinking of Rivers (ILR) Programme
The National Perspective Plan for interlinking of rivers envisages transferring water from surplus to deficit basins. The Ken-Betwa Link Project (KBLP) is the first project under this programme to receive government approval (December 2021) at an estimated cost of Rs 44,605 crore. The project involves transferring water from the Ken River to the Betwa River through the construction of the Daudhan Dam and a linking canal, benefiting parts of Madhya Pradesh and Uttar Pradesh. The project is planned for completion by March 2030 and is being implemented through a Special Purpose Vehicle — the Ken Betwa Link Project Authority (KBLPA).
Himalayan vs. Peninsular Rivers
| Feature | Himalayan Rivers | Peninsular Rivers |
|---|---|---|
| Source | Glaciers and snowmelt | Rainfall and springs |
| Flow | Perennial | Seasonal (except west-flowing) |
| Catchment | Large | Relatively smaller |
| Gradient | Steep in upper; gentle in plains | Gentle; mature stage |
| Meanders | Extensive in plains | Less pronounced |
| Delta | Large deltas (Sundarbans) | Deltas (Godavari, Krishna, Kaveri) |
| Drainage | Antecedent and consequent | Superimposed |
Soil Types of India
Indian soils are classified into several major types based on genesis, composition, and distribution.
Major Soil Types and Distribution
| Soil Type | Region/Distribution | Key Properties | Suitable Crops |
|---|---|---|---|
| Alluvial Soil | Indo-Gangetic Plains, river valleys, coastal areas | Rich in potash; deficient in phosphorus and nitrogen; light to dark | Rice, wheat, sugarcane, pulses |
| Black Soil (Regur) | Deccan Plateau (Maharashtra, Gujarat, MP, Karnataka) | Rich in calcium, potassium, magnesium; poor in nitrogen; self-ploughing | Cotton, tobacco, oilseeds, jowar |
| Red Soil | Eastern Deccan, Odisha, Chhattisgarh, Tamil Nadu | High iron content; acidic; poor in nitrogen, phosphorus, humus | Groundnut, red gram, Bengal gram, castor |
| Laterite Soil | Western Ghats, parts of Odisha, Jharkhand, Kerala | Rich in iron and aluminium; acidite; poor in fertility | Tea, coffee, cashew, rubber |
| Arid/Desert Soil | Western Rajasthan, parts of Gujarat, Haryana | Sandy; low humus; high salinity; poor water retention | Bajra, pulses (with irrigation) |
| Forest/Mountain Soil | Himalayan slopes, Western & Eastern Ghats | Rich in humus; acidic; varies with altitude | Tea, coffee, spices, fruits |
| Peaty/Marshy Soil | Kerala, coastal Odisha, Sundarbans, Uttarakhand | High organic content; acidic; waterlogged | Rice (in some areas) |
| Saline/Alkaline Soil | Punjab, Haryana, Rajasthan, coastal Gujarat (Rann of Kutch) | High sodium, potassium, magnesium salts; Usar/Reh | Poor for crops; requires reclamation |
Coastal Plains and Islands
India's total coastline, traditionally measured at 7,516.6 km, was re-assessed to 11,098.81 km by the National Hydrographic Office (NHO) in coordination with the Survey of India using modern GIS software and high-resolution High-Water Line data. The revised figure was officially promulgated by the Ministry of Ports, Shipping and Waterways in April 2025. The increase reflects better measurement technology, not a physical change in the landmass.
Coastal Plains
| Coast | Name | Length | Features |
|---|---|---|---|
| Western Coast | Konkan, Kanara, Malabar | ~1,500 km | Narrow; rocky; lagoons and backwaters (Kerala); fewer deltas |
| Eastern Coast | Northern Circars, Coromandel | ~2,000 km | Broader; alluvial; lagoon (Chilika Lake); large deltas (Godavari, Krishna, Kaveri) |
Islands
| Island Group | Location | Number | Origin | Key Features |
|---|---|---|---|---|
| Andaman & Nicobar | Bay of Bengal | 572 | Tectonic (submerged mountain chain) | Barren Island — only active volcano in India (last erupted 2017); part of a submerged extension of the Arakan Yoma range; 31 islands inhabited; home to Particularly Vulnerable Tribal Groups (PVTGs) |
| Lakshadweep | Arabian Sea | 36 | Coral origin (atolls) | 12 atolls, 3 reefs, 5 submerged banks; 10 islands inhabited; total area ~32 sq km; Kavaratti is capital; important for India's maritime security in the Arabian Sea |
The Andaman & Nicobar Islands extend India's Exclusive Economic Zone (EEZ) significantly into the Bay of Bengal and are strategically located near the Strait of Malacca, one of the world's busiest shipping lanes. The Lakshadweep islands, being coral atolls, are highly vulnerable to sea-level rise and coral bleaching from climate change.
Important for UPSC
Prelims Focus
- Exact heights of major peaks and lengths of rivers
- Matching rivers with their origin points and tributaries
- Soil types and their crop suitability
- Physiographic divisions and their geological age
- Drainage patterns and their characteristics
- Island groups and their geological origin
- Key mountain passes — location, connecting regions, and strategic significance
- India's coastline length and the 2025 revision from 7,516.6 km to 11,098.81 km
Mains Dimensions
- Role of Himalayas in shaping India's climate, rivers, and biodiversity (GS1)
- River interlinking and its geographical, environmental, and social implications (GS1/GS3)
- Soil degradation, conservation strategies, and their link to food security (GS3)
- Peninsular Plateau's mineral wealth and its economic significance (GS1/GS3)
- Coastal zone management and vulnerability to climate change (GS3)
- Strategic significance of Himalayan passes for border security and trade connectivity (GS1/GS2)
- Indus Waters Treaty — geopolitical dimensions and climate change impact on transboundary water sharing (GS2)
Interview Angles
- Why does India have such diverse physiography in a relatively compact area?
- Should the Himalayas be treated as an ecological entity rather than a political boundary?
- How does the geology of the Peninsular Plateau make it mineral-rich but water-scarce?
- Discuss the strategic significance of the Andaman & Nicobar and Lakshadweep islands
- Ken-Betwa interlinking — evaluate trade-offs between water security, submergence of Panna Tiger Reserve habitat, and displacement
Vocabulary
Physiography
- Pronunciation: /ˌfɪziˈɒɡrəfi/
- Definition: The branch of physical geography that studies the Earth's natural physical features, including landforms, climate, vegetation, and hydrology.
- Origin: From French physiographie, combining Greek phusis ("nature") and grapho ("to write"); earliest recorded use in English dates to 1799 in Immanuel Kant's Essays & Treatises.
Alluvial
- Pronunciation: /əˈluːviəl/
- Definition: Relating to or composed of sediment (clay, silt, sand, gravel) deposited by flowing water, especially in river valleys and floodplains.
- Origin: From Medieval Latin alluvius ("washed against"), derived from Latin alluere ("to wash against"), combining ad ("to, against") and lavere ("to wash"); first attested in English in 1771.
Peninsular
- Pronunciation: /pəˈnɪnsjʊlə(r)/
- Definition: Of or relating to a peninsula — a landmass almost entirely surrounded by water but connected to the mainland by a narrow strip of land.
- Origin: A learned borrowing from Latin paenīnsulāris, derived from paene ("almost") and insula ("island"), literally meaning "almost an island."
Key Terms
Deccan Plateau
- Pronunciation: /ˈdɛkən pləˈtəʊ/
- Definition: A large triangular plateau in southern India extending over approximately 422,000 sq km (163,000 sq mi), bounded by the Western Ghats to the west, Eastern Ghats to the east, and the Vindhya-Satpura ranges to the north, with an average elevation of about 600 metres that rises to over 1,000 m in the south. Its most remarkable geological feature is the Deccan Traps — massive layers of basaltic lava up to 2,000 metres thick that erupted approximately 66 million years ago at the Cretaceous-Paleogene boundary, producing the fertile regur (black cotton) soil that supports India's cotton-growing belt.
- Context: The word "Deccan" is an anglicised form of the Prakrit word dakkhaṇa, derived from Sanskrit dakṣiṇa meaning "south." The plateau is composed primarily of Precambrian gneiss, granite-gneiss, and schists overlain by Cretaceous basalt flows. It covers most of Maharashtra, Karnataka, Telangana, and Andhra Pradesh (excluding coastal regions), with minor portions of Kerala and Tamil Nadu. The plateau slopes gently from west to east, explaining why most peninsular rivers (Godavari, Krishna, Kaveri) flow eastward into the Bay of Bengal.
- UPSC Relevance: GS1 Geography. Prelims tests physiographic divisions, geological age (Precambrian basement, Cretaceous Deccan Traps), and the distinction between Western Ghats (faulted escarpment) and Himalayas (fold mountains). Mains asks about the Deccan Trap's natural resource potential (asked 2022), mineral wealth (iron ore, manganese, bauxite), and the plateau's role in shaping India's drainage and soil patterns. For Mains, focus on the relationship between basaltic lava flows and regur soil formation, and the plateau's eastward slope determining river direction.
Interlinking of Rivers
- Pronunciation: /ˌɪntəˈlɪŋkɪŋ ɒv ˈrɪvəz/
- Definition: A large-scale Indian civil engineering programme under the National Perspective Plan (1980) that aims to transfer water from surplus river basins to deficit basins through a network of reservoirs and canals, comprising 30 link projects — 14 under the Himalayan Rivers Component and 16 under the Peninsular Rivers Component — with the National Water Development Agency (NWDA) as the implementing body. Pre-Feasibility Reports have been completed for all 30 projects, Feasibility Reports for 26, and Detailed Project Reports for 11 as of 2025.
- Context: The concept traces back to 19th-century British engineer Arthur Cotton's proposals; it was formally revived by Dr K.L. Rao's "National Water Grid" idea in the 1970s, and the National Perspective Plan was published by the Ministry of Water Resources in 1980, with NWDA established in 1982. The Ken-Betwa Link Project (KBLP) is the first project to enter the implementation stage — its foundation stone was laid by PM Modi on 25 December 2024 at Khajuraho, MP, at an estimated cost of Rs 44,605 crore, with completion targeted by 2030. It will provide irrigation for 6.3 lakh hectares and drinking water for 62 lakh people.
- UPSC Relevance: GS1 Geography and GS3 Environment. Directly asked in Mains 2020: "Critically examine interlinking of rivers as solution to droughts, floods, and interrupted navigation." Prelims tests Ken-Betwa Link Project details — first project under the NPP, Daudhan Dam construction, concern over tree felling in Panna Tiger Reserve (over 17,000 trees identified, 12,000+ already felled). Mains expects a balanced analysis weighing water security benefits (irrigation, drinking water, hydropower) against environmental costs (submergence, displacement, ecological damage to tiger habitat).
Current Affairs Connect
| Topic Link | Relevance |
|---|---|
| Ujiyari -- Geography News | Latest developments in physical geography, river projects, and geological surveys |
| Ujiyari -- Editorials | Analysis of river interlinking, Himalayan ecology, and coastal erosion policies |
| Ujiyari -- Daily Updates | Daily news on natural disasters, river floods, landslides, and seismic activity |
Sources: Know India -- Physical Features (india.gov.in) | Know India -- Rivers | Know India -- Length of Important Indian Rivers | Central Water Commission -- About Basins | NCERT -- Physical Features of India
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