Question map
Consider the following pairs : Glacier River 1. Bandarpunch : Yamuna 2. Bara Shigri : Chenab 3. Milam : Mandakini 4. Siachen : Nubra 5. Zemu : Manas Which of the pairs given above are correctly matched?
Explanation
The correct answer is option A (pairs 1, 2, and 4 are correctly matched).
**Pair 1 (Bandarpunch-Yamuna)** is correct: The Yamuna originates from the Yamunotri Glacier on the western slopes of Banderpunch range (6,316 m)[2], establishing a direct connection between Bandarpunch and the Yamuna River.
**Pair 2 (Bara Shigri-Chenab)** is correct: Bara Shigri glacier is located in Chandra Valley of Lahaul in Himachal Pradesh and is a source of water for River Chenab[3]. Additionally, the Chenab is known as Chandra-Bhaga in Himachal Pradesh, and the Chandra and Bhaga tributaries originate on either side of the Bara-Lacha Pass in Lahul District[4].
**Pair 4 (Siachen-Nubra)** is correct: Nubra river emerges from the Karakoram glaciers[5], and the Shyok-Nubra tributaries arise from the Siachen Glacier (Karakoram Range)[6].
**Pair 3 (Milam-Mandakini)** is incorrect because Milam glacier is the major source of River Gori Ganga[3], not Mandakini. **Pair 5 (Zemu-Manas)** is incorrect as Zemu glacier feeds River Teesta[7], not Manas.
Sources- [1] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > The Yamuna River > p. 13
- [2] INDIA PHYSICAL ENVIRONMENT, Geography Class XI (NCERT 2025 ed.) > Chapter 3: Drainage System > Do you Know? > p. 22
- [3] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 2: Physiography > Table 2.3 > p. 25
- [4] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > The Chenab (Asikni) > p. 10
- [5] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 16: India–Political Aspects > The Siachin/Aksai chin Glacier Dispute > p. 39
- [6] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > 1. The Indus (Sindhu) > p. 9
- [7] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 2: Physiography > Table 2.3 > p. 24
PROVENANCE & STUDY PATTERN
Full viewThis is a textbook 'Table-Lift' question. The pairs are directly sourced from the 'List of Glaciers' tables found in standard books like Majid Husain (Table 2.3) and NCERT. It rewards rote memorization of specific Glacier-River linkages rather than conceptual understanding.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: In the Indian Himalaya, is the Bandarpunch glacier a source or main feeder of the Yamuna River?
- Statement 2: In the Indian Himalaya, is the Bara Shigri glacier a source or main feeder of the Chenab River?
- Statement 3: In the Indian Himalaya, is the Milam glacier a source of the Mandakini River?
- Statement 4: In the Indian Himalaya, is the Siachen glacier the source of the Nubra River?
- Statement 5: In the Indian Himalaya, is the Zemu glacier the source of the Manas River?
- Identifies the Yamuna's source as the Yamunotri Glacier located on the western slopes of Banderpunch (6316 m).
- Directly links the Banderpunch massif area with the origin of the Yamuna River.
- States the Yamuna is the westernmost longest tributary of the Ganga and has its source in the Yamunotri Glacier on the western slopes of Banderpunch range (6,316 m).
- Reinforces the Bandarpunch–Yamunotri connection and the river's Himalayan glacial origin.
- Confirms the Yamuna rises from the Yamunotri Glacier in the Himalayas.
- Provides independent support that the Yamuna's primary source is a Himalayan glacier (Yamunotri).
- Explicitly names Bara Shigri in the Chandra Valley (Lahaul) and labels it as 'Source of water for River Chenab'.
- Places the glacier in the correct valley (Chandra) that is tied to Chenab headwaters.
- Describes Chenab's upper tributaries as Chandra and Bhaga originating near Bara-Lacha Pass in Lahaul.
- Links the Chandra tributary (Chandra-Bhaga system) to the formation of the Chenab, supporting Bara Shigri's role via its Chandra-valley location.
- Identifies the Chenab's source region as the Lahaul Valley of Himachal Pradesh, consistent with Bara Shigri's location.
- Supports geographic context tying named glaciers in Lahaul to the Chenab system.
Lists Milam glacier as the major source of the Gori Ganga (Goriganga) in Uttarakhand, tying Milam to Gori/Goriganga rather than Mandakini.
Using a map or basic regional knowledge, note that Gori Ganga (from Milam) and Mandakini are separate river systems in different parts of the Kumaon/Garhwal Himalaya.
States that the Mandakini (Kali Ganga) originates from the Chorabari Glacier and meets the Alaknanda at Rudra Prayag — giving an explicit, different source for Mandakini.
Compare the geographic locations of Chorabari Glacier (source of Mandakini) and Milam Glacier on a map to see they are distinct.
Notes Mandakini (Kali Ganga) joins Alaknanda at Rudra Prayag, confirming Mandakini's role and identity in the upper Ganga system.
Locate Rudra Prayag and trace upstream to the Mandakini source to verify that it is not Milam.
Associates the Milam/Milam-region glacier with the river known as Goriganga (Sarda) along the Indo-Nepal border, reinforcing Milam→Gori/Goriganga linkage.
Use the stated Milam→Goriganga link plus a map of Indo-Nepal border rivers to distinguish Goriganga's course from Mandakini's.
Gives a general rule that most perennial northern rivers originate in Himalayan glaciers, so identifying glacier names gives direct clues to river sources.
Apply this rule: if a glacier is named as the source of a specific river (e.g., Milam→Gori Ganga, Chorabari→Mandakini), then that glacier is unlikely to be the source of a different named river.
- Explicitly states the Shyok–Nubra tributaries arise from the Siachen Glacier (Karakoram Range).
- Directly links Siachen Glacier meltwater to the Nubra/Shyok branch of the Indus drainage.
- Describes the Siachen glacier in the Karakoram and immediately notes Nubra river emerging from Karakoram glaciers in the same context.
- Places Siachen within the Nubra valley region, supporting its role as a local glacier source.
- Lists Siachen as the largest glacier in the Nubra Valley, linking the glacier geographically to the valley drained by the Nubra River.
- Provides a mapped/glacial association that supports Siachen being the principal glacier in Nubra Valley.
This table explicitly states 'Zemu' is in Sikkim/Nepal and 'it feeds River Teesta', giving a direct glacier→river pairing for Zemu.
A student can use this to suspect Zemu is linked to Teesta (not Manas) and then check maps/river courses to see where Manas originates relative to Teesta/Zemu.
Lists Manas among Himalayan rivers that 'originate on the southern slopes of the Tibetan Highlands', indicating a general source region for Manas.
Combine this with a map to locate Manas' headwaters and compare that location to Zemu's location in Sikkim to judge if Zemu could be Manas' source.
States most perennial northern Indian rivers originate in Himalayan glaciers, framing the general expectation that a named glacier often corresponds to a river source.
Use this rule to look for the specific glacier named as a headwater on maps or gazetteers for the Manas, and see whether Zemu is listed.
Provides concrete examples of glaciers (e.g., Satopanth, Mana, Gangotri, Pindari) being cited as specific river sources, illustrating the pattern of glacier→named river origin.
Apply the same checking method used for these examples: find authoritative source lists/maps that pair glaciers with the Manas headwater to test if Zemu appears.
Explains glacier snouts (e.g., Gaumukh of Gangotri) feeding named rivers, reinforcing the concept that precise glacier identification is used to assign river sources.
Use glacial snout locations and river flow directions on a map to see whether Zemu's snout could feed the Manas catchment.
- [THE VERDICT]: Sitter (if you read Majid Husain Tables) / Trap (if you guessed by region). Source: Majid Husain, Chapter 2, Table 2.3 'Main Glaciers of the Himalayan Region'.
- [THE CONCEPTUAL TRIGGER]: Drainage System > Himalayan Rivers > Specific Headwaters. The shift from asking 'Which state?' to 'Which specific glacier?'.
- [THE HORIZONTAL EXPANSION]: Memorize the 'Rejected' pairs and their neighbors: Zemu → Teesta; Chorabari → Mandakini; Satopanth → Alaknanda; Rimo → Shyok; Hispar → Shigar; Gangotri → Bhagirathi.
- [THE STRATEGIC METACOGNITION]: When studying rivers, never stop at 'Origin: Himalayas'. You must map the specific 'Snout' (Glacier) to the 'Headstream'. Use the 'Panch Prayag' logic to trace sources upstream (e.g., Alaknanda starts at Satopanth, not Gangotri).
The Yamuna originates at the Yamunotri Glacier situated on the western slopes of the Bandarpunch massif.
High-yield for questions on Himalayan river origins and source locations; links physical geography (glacial sources) with river course and human geography (cities along the Yamuna). Mastery helps answer source-location, drainage-basin, and river-system mapping questions.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > The Yamuna River > p. 13
- INDIA PHYSICAL ENVIRONMENT, Geography Class XI (NCERT 2025 ed.) > Chapter 3: Drainage System > Do you Know? > p. 22
Major northern Indian rivers, including the Yamuna, derive their perennial flow from Himalayan glaciers and snowfields.
Essential for topics on river regimes, water resources, and climate impact on hydrology; connects to questions on seasonal flow variability, irrigation, and downstream settlement patterns. Enables comparison-type questions across river systems.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 2: Physiography > 3. Source of Perennial Rivers > p. 29
- CONTEMPORARY INDIA-I ,Geography, Class IX . NCERT(Revised ed 2025) > Chapter 3: Drainage > The Ganga River System > p. 20
The Yamuna is the westernmost and longest tributary of the Ganga, joining it at Prayag/Allahabad.
Important for syllabus items on Indo-Gangetic drainage, basin interrelationships, and regional river politics; helps in tackling map-based, comparative river-system, and inter-state river questions.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > The Yamuna River > p. 13
- INDIA PHYSICAL ENVIRONMENT, Geography Class XI (NCERT 2025 ed.) > Chapter 3: Drainage System > Do you Know? > p. 22
Glaciers in the Himalaya provide meltwater that forms and sustains perennial rivers such as the Chenab, Indus and Brahmaputra.
High-yield for UPSC physical geography and environment topics: explains river source regions, seasonal flows, and links to water security and hydropower. Mastery helps answer map-based source questions and climate-change impacts on river regimes.
- Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 23: India and Climate Change > zJ.z.S. Impacts an Himalayan Glaciers > p. 300
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 2: Physiography > 3. Source of Perennial Rivers > p. 29
The Chenab is formed from the confluence of the Chandra and Bhaga streams in Lahaul, with their origins near Bara-Lacha Pass.
Essential for questions on river systems and inter-state river geography; aids in tracing tributary networks, planning hydrological projects, and answering source-location MCQs and descriptive answers.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > The Chenab (Asikni) > p. 10
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > Table 3.3 > p. 18
Specific glaciers (e.g., Bara Shigri) are tied to particular rivers; knowing these mappings identifies river headwaters precisely.
Useful for objective and descriptive questions asking 'which glacier feeds which river' and for map labeling; integrates with topics on glacier retreat, river basin management, and regional physiography.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 2: Physiography > Table 2.3 > p. 25
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > The Chenab (Asikni) > p. 10
Many Himalayan rivers are explicitly identified as originating from specific glaciers (e.g., Milam → Gori/Goriganga; Chorabari → Mandakini; Gangotri → Bhagirathi).
High-yield for physical geography questions: knowing which glacier feeds which river helps answer source-origin and basin questions, link hydrology to regional physiography, and solve map-based items about river courses and catchments.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 2: Physiography > Table 2.3 > p. 25
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 3: The Drainage System of India > Five Confluences in the upper reaches of Ganga > p. 12
- INDIA PHYSICAL ENVIRONMENT, Geography Class XI (NCERT 2025 ed.) > Chapter 3: Drainage System > The Ganga System > p. 21
Rimo Glacier: Located in the Siachen area (Karakoram), but it drains into the Shyok River, not the Nubra. This is a high-probability trap for a future 'Consider the following pairs' question.
The 'Kedarnath' Logic: Mandakini is the river of Kedarnath. The 2013 tragedy made 'Chorabari Glacier' (the source of the flood) famous. If you recalled Kedarnath = Chorabari, you eliminate Pair 3 immediately. Similarly, Zemu is the pride of Sikkim (Teesta), while Manas is an Assam/Bhutan giant. This mismatch eliminates Pair 5.
Disaster Management (GLOFs): Link Zemu Glacier (Sikkim) to the Teesta River and the recent South Lhonak Lake outburst. Glacial thinning in Zemu is a direct Mains case study for Climate Change impact on Hydrology.