Which one among the following is at the highest altitude ?

1. Structure and Zonation of the Himalayas (basic)

The Himalayas are geologically young and structurally fold mountains that form a massive arc across the northern borders of India Contemporary India-I, Class IX NCERT, Physical Features of India, p.7. Stretching approximately 2,400 to 2,500 km from the Indus in the west to the Brahmaputra in the east, they act as the loftiest mountain barrier in the world. Interestingly, their width is not uniform; they are much broader in the west (400 km in Kashmir) and taper significantly as they move east (150 km in Arunachal Pradesh). This narrowing in the east is accompanied by greater altitudinal variations compared to the western half Contemporary India-I, Class IX NCERT, Physical Features of India, p.7.

Structurally, the Himalayas are organized into three parallel longitudinal ranges. Each zone has distinct geological and climatic characteristics:

• The Greater Himalayas (Himadri): This is the northernmost, highest, and most continuous range. It consists of the loftiest peaks with an average height of 6,000 meters and remains perpetually snow-covered. Famous peaks like Mount Everest and Kanchenjunga are located here Exploring Society: India and Beyond, Class VII NCERT, Geographical Diversity of India, p.6.
• The Lesser Himalayas (Himachal): Located south of the Himadri, this range is highly rugged with altitudes ranging between 3,700 and 4,500 meters. It is famous for its scenic hill stations such as Shimla, Mussoorie, and Nainital Contemporary India-I, Class IX NCERT, Physical Features of India, p.8.
• The Outer Himalayas (Shiwaliks): The southernmost and lowest range (900–1500m). Between the Shiwaliks and the Lesser Himalayas lie 'Duns'—longitudinal valleys such as Dehradun and Patli Dun Geography of India, Majid Husain, Physiography, p.12.

Range	Other Name	Avg. Elevation	Key Feature
Inner Himalayas	Himadri	6,000m+	Perennial snow & highest peaks
Middle Himalayas	Himachal	3,700 – 4,500m	Popular hill stations
Outer Himalayas	Shiwalik	900 – 1,500m	Unconsolidated sediments & Duns

Sources: Contemporary India-I, Class IX NCERT, Physical Features of India, p.7-8; India Physical Environment, Class XI NCERT, Structure and Physiography, p.11; Exploring Society: India and Beyond, Class VII NCERT, Geographical Diversity of India, p.6; Geography of India, Majid Husain, Physiography, p.12

2. Regional Longitudinal Divisions of the Himalayas (basic)

While we often look at the Himalayas in terms of height (the North-to-South latitudinal zones), geographers also divide them from West to East. This is known as the Regional or Longitudinal classification. These divisions are not defined by altitude, but by the major river valleys that cut through the mountain range, acting as natural boundaries. This classification was famously proposed by Sir Sidney Burrard and helps us understand the distinct geological and cultural identities of the mountains across their 2,500 km span Geography of India, Majid Husain, Physiography, p.13.

The four primary regional divisions are defined by five major rivers acting as markers:

• Punjab Himalayas: Located between the Indus and the Satluj rivers. This section is also regionally known as the Kashmir and Himachal Himalayas.
• Kumaon Himalayas: This part lies between the Satluj and the Kali rivers CONTEMPORARY INDIA-I, Physical Features of India, p.10.
• Nepal Himalayas: The segment stretching between the Kali and the Teesta rivers. This section contains some of the highest peaks in the world.
• Assam Himalayas: Found between the Teesta and the Dihang (Brahmaputra) rivers.

Beyond the Dihang gorge, the Himalayas take a sharp southward bend and are known as the Purvachal or Eastern Hills. These hills run through the north-eastern states and are primarily composed of strong sedimentary sandstones CONTEMPORARY INDIA-I, Physical Features of India, p.10. Understanding these boundaries is crucial for mapping because it allows us to pinpoint exactly which state or country a specific peak or pass belongs to.

Regional Division	Western River Boundary	Eastern River Boundary
Punjab Himalayas	Indus	Satluj
Kumaon Himalayas	Satluj	Kali
Nepal Himalayas	Kali	Teesta
Assam Himalayas	Teesta	Dihang (Brahmaputra)

Sources: CONTEMPORARY INDIA-I, Physical Features of India, p.10; Geography of India (Majid Husain), Physiography, p.1, 13

3. The 'Eight-Thousanders' of the World (intermediate)

In the world of physical geography, the term 'Eight-Thousander' refers to the elite group of 14 independent mountains that rise more than 8,000 metres (26,247 feet) above sea level. What makes these peaks truly remarkable is their concentration: every single one of them is located in Asia, specifically within the Himalayan and Karakoram mountain ranges. These giants are not just geological marvels; they act as the 'Water Tower of Asia' because their massive glaciers melt during summer to feed perennial rivers like the Ganga, Indus, and Brahmaputra, supporting the lives of hundreds of millions Exploring Society: India and Beyond, Class VII, p.4.

While Mount Everest (8,848m) is the highest, it is followed by K2 (8,611m) and Kanchenjunga (8,598m). It is a common point of confusion for students to mix these up with other high peaks. For instance, while Nanda Devi (7,817m) is a magnificent peak and the highest located entirely within India, it does not qualify as an eight-thousander because it falls just short of the 8,000-metre mark Contemporary India-I, Class IX, p.8. Most of these giants are clustered in the Central Himalayas, a region stretching from the Kali river to the Tista river, which includes peaks like Dhaulagiri and Annapurna Geography of India, Majid Husain, p.16.

Understanding their relative heights is crucial for mapping and identifying regional geography. Below is a comparison of some of the most significant peaks often discussed in Indian geography:

Peak Name	Height (m)	Location/Region
Mount Everest	8,848	Nepal/China Border
Kanchenjunga	8,598	India (Sikkim)/Nepal
Dhaulagiri	8,172	Nepal
Nanga Parbat	8,126	India (UT of Ladakh/J&K context)
Nanda Devi	7,817	India (Uttarakhand) — Not an 8k-er

Sources: Exploring Society: India and Beyond, Social Science-Class VII (NCERT 2025), Geographical Diversity of India, p.4; Contemporary India-I, Geography, Class IX (NCERT 2025), Physical Features of India, p.8; Geography of India, Majid Husain (McGrawHill 9th ed.), Physiography, p.16

4. Major Himalayan Glaciers and River Origins (intermediate)

Welcome back! Now that we’ve explored the structural layout of the Himalayas, let’s look at their 'frozen heart'—the glaciers. These are not just masses of ice; they are the perennial water towers of India. A key concept to understand first is the snowline, the altitude above which snow remains on the ground throughout the year. Interestingly, the snowline is lower in the Eastern Himalayas (around 4,400 m in Arunachal Pradesh) due to higher humidity from the Bay of Bengal, whereas in the drier Karakoram, it starts much higher at 5,500 m and above Majid Husain, Geography of India, Physiography, p.23.

The Karakoram Range houses some of the world's largest non-polar glaciers. The Siachen Glacier (76 km long) is the most famous, feeding the Nubra River. Other giants like the Biafo and Hispar (the world's longest glacial system outside the poles) eventually contribute to the Shigar and Indus river systems. Moving into the Greater Himalayas, the glaciers become the primary source for the Ganga and Brahmaputra basins. For instance, the Zemu Glacier in the Sikkim/Nepal region is the largest in the Eastern Himalayas and is the lifeblood of the Teesta River Majid Husain, Geography of India, Physiography, p.24.

In the Uttarakhand Himalayas, glaciers are vital for the Panch Prayag (five sacred confluences). The Gangotri Glacier (specifically at Gaumukh) gives rise to the Bhagirathi, while the Satopanth Glacier is the source of the Alaknanda. These two meet at Dev Prayag to finally become the Ganga. Further east in the Kumaon region, the Milam Glacier feeds the Gori Ganga, and the Pindari Glacier gives rise to the Pindar River Majid Husain, Geography of India, The Drainage System of India, p.12. Understanding these specific links is crucial for mapping the hydrology of the Indian subcontinent.

Glacier	Location/Range	Primary River/Tributary
Bara Shigri	Himachal (Chandra Valley)	Chenab
Chong Kumdan	Karakoram (Ladakh)	Shyok
Sonapani	Pir Panjal	Chandra (Chenab tributary)
Drang Drung	Zanskar Range	Suru (Indus system)

Sources: Geography of India (Majid Husain), Physiography, p.23-25; Geography of India (Majid Husain), The Drainage System of India, p.12

5. Geography of Pilgrimage Sites (Chota Char Dham) (intermediate)

The Chota Char Dham is a prestigious pilgrimage circuit located in the Garhwal region of the Himalayas in Uttarakhand. While the traditional 'Char Dham' spans the four corners of India, this 'small' (Chota) circuit is concentrated within a single high-altitude geographic belt. The four sites include Yamunotri, Gangotri, Kedarnath, and Badrinath. These shrines are not just spiritual centers but are geographically significant as they are located near the headwaters of major Himalayan rivers: Yamunotri (Yamuna), Gangotri (Bhagirathi/Ganga), Kedarnath (Mandakini), and Badrinath (Alaknanda) Majid Husain, Geography of India, p.30. From a physical mapping perspective, these sites are situated in the Greater Himalayas (Himadri) at elevations ranging from approximately 3,100 to 3,600 meters. For example, Badrinath sits at about 3,300 meters. It is crucial for a geography student to distinguish these pilgrimage altitudes from the massive 'eight-thousander' peaks. While these shrines are high, they are significantly lower than the towering giants like Nanda Devi (7,817m) or Kamet (7,756m), which are the highest peaks in the Indian Uttarakhand sector NCERT Class IX, Physical Features of India, p.8. The accessibility of these sites is governed by the snowline. In the Kumaun and Garhwal Himalayas, the snowline typically begins between 5,100m and 5,500m Majid Husain, Physiography, p.23. Because the pilgrimage sites are located below this permanent snowline, they are accessible during the summer months but remain buried under seasonal snow during the harsh winter, necessitating the seasonal closing of the temples. This region is also a hub of glacial activity, with the Gangotri glacier being one of the largest in the Himalayas, serving as the primary source of the Bhagirathi river.

Sources: Geography of India (Majid Husain), The Drainage System of India, p.30; Geography of India (Majid Husain), Physiography, p.23; CONTEMPORARY INDIA-I (NCERT Class IX), Physical Features of India, p.8

6. Highest Peaks Entirely Within India (exam-level)

When discussing the highest peaks in India, we must distinguish between peaks that are physically located within India's borders and those that are shared with neighboring countries or situated in contested territories. This distinction is a frequent source of confusion in competitive exams. Geographically, while Mt. Everest (Nepal) and K2 (POK/Pakistan) are higher, they do not fall entirely within India's undisputed territory. Even Kanchenjunga (8,598m), the highest peak in India, sits on the border between Sikkim and Nepal CONTEMPORARY INDIA-I, Geography, Class IX, p.8.

The highest peak located entirely within India is Nanda Devi, standing at 7,817 metres. Situated in the Garhwal Himalayas of Uttarakhand, it is the 23rd highest peak in the world. Its surrounding Nanda Devi National Park is a UNESCO World Heritage site, protected by rugged mountain walls that make it one of the most inaccessible massifs in the world. Other significant peaks located entirely within Indian territory include Kamet (7,756m) and Trishul (7,120m), both in Uttarakhand.

To put this into perspective, compare these Indian-exclusive peaks with those in Nepal or on the borders:

Peak	Height (m)	Status/Location
Kanchenjunga	8,598	Shared (India-Nepal Border)
Dhaulagiri	8,172	Nepal
Nanga Parbat	8,126	POK (Claimed by India)
Nanda Devi	7,817	Entirely within India
Kamet	7,756	Entirely within India

It is also useful to note the highest peaks in other regions of India to understand the relief variations. While the Himalayas host the tallest peaks, the peninsular region's highest point is Anai Mudi (2,695m) in the Western Ghats, and Mahendragiri (1,501m) is the highest in the Eastern Ghats CONTEMPORARY INDIA-I, Geography, Class IX, p.12.

Sources: CONTEMPORARY INDIA-I ,Geography, Class IX, Chapter 2: Physical Features of India, p.8; CONTEMPORARY INDIA-I ,Geography, Class IX, Chapter 2: Physical Features of India, p.12

7. Comparative Heights: Dhaulagiri, Annapurna, and Nanda Devi (exam-level)

To master the physical mapping of the Himalayas, we must distinguish between the 'Eight-thousanders'—the elite club of 14 global peaks rising above 8,000 meters—and other significant high-altitude summits. Among the giants of the Central Himalayas, Dhaulagiri and Annapurna both cross this prestigious threshold. Dhaulagiri, located in Nepal, stands at 8,172 meters, making it the 7th highest mountain in the world CONTEMPORARY INDIA-I, Chapter 2: Physical Features of India, p.8. Just to its east lies the Annapurna massif; its highest point, Annapurna I, reaches 8,078 meters (though some records cite 8,091m), ranking as the 10th highest peak globally Geography of India, Chapter 2: Physiography, p.16. Moving westward into the Indian state of Uttarakhand, we encounter Nanda Devi. While it is a crown jewel of the Indian Himalayas and the highest peak situated entirely within India, it does not reach the 8,000-meter mark, standing at 7,817 meters CONTEMPORARY INDIA-I, Chapter 2: Physical Features of India, p.8. It is important for aspirants to distinguish these massive peaks from high-altitude pilgrimage sites like Badrinath. Although Badrinath is nestled in the high Garhwal Himalayas, the town itself sits at an elevation of approximately 3,100 to 3,300 meters—significant, but far below the glaciated summits of the Great Himalayan range Geography of India, Chapter 2: Physiography, p.12.

Understanding the relative heights helps in visualizing the 'staircase' effect of the Himalayan ranges as they move from the Nepal sector (home to most 8,000m+ peaks) toward the Kumaon and Garhwal sectors in India.

Peak	Height (m)	Country/Region	Status
Dhaulagiri	8,172	Nepal	Eight-thousander (7th Highest)
Annapurna I	8,078	Nepal	Eight-thousander (10th Highest)
Nanda Devi	7,817	India (Uttarakhand)	Highest peak entirely in India

Sources: CONTEMPORARY INDIA-I ,Geography, Class IX, Chapter 2: Physical Features of India, p.8; Geography of India ,Majid Husain, Chapter 2: Physiography, p.16; Geography of India ,Majid Husain, Chapter 2: Physiography, p.12

8. Solving the Original PYQ (exam-level)

Now that you have mastered the structural divisions of the Himalayas, this question puts your knowledge of the Himadri (Great Himalayas) into practice. In your learning path, you explored how the highest peaks are concentrated in the central section of the range, specifically within the Nepal Himalayas. To solve this, you must apply the concept of 'Eight-thousanders'—the elite group of peaks exceeding 8,000 meters. While both Annapurna I and Dhaulagiri belong to this category, your conceptual map of the Dhaulagiri-Annapurna massif in Nepal helps you identify that Dhaulagiri (8,172m) stands slightly taller than Annapurna I (8,091m), making it the highest among the given choices.

As a coach, I want you to notice the logical elimination process here. You should immediately categorize the options: Badrinath is a famous pilgrimage town and peak in Uttarakhand, but it sits at a much lower altitude (approx. 3,300m) compared to the giants. Nanda Devi (7,817m) is a critical landmark as the highest peak entirely within Indian territory, but it falls just short of the 8,000-meter mark. By recognizing that Dhaulagiri belongs to the world's top ten highest peaks, you can confidently select (C) Dhaulagiri as the correct answer. Always prioritize peaks located in the Nepal-Tibet stretch when looking for maximum elevation.

UPSC often uses common traps by mixing well-known religious sites with geographical extremes. Many students mistakenly choose Badrinath because of its fame, or Nanda Devi because of its status within India. However, as noted in NCERT Class IX Geography and Geography of India by Majid Husain, the Great Himalayan range reaches its maximum verticality in the Nepal sector. Distinguishing between the specific heights of 8,000m+ peaks is a classic test of your factual precision and your ability to visualize the Physiography of India beyond political boundaries.