\nAnswer: (a) 1, 2 and 4<\/strong><\/p>\n<\/blockquote>\n\n\n\nNotes:<\/h3>\n\n\n\n\n- Bandarpunch<\/strong>\u00a0is a mountain massif of the\u00a0Garhwal<\/strong> division of the <\/strong>Himalayas<\/strong>, in the\u00a0Indian\u00a0state of\u00a0Uttarakhand<\/strong>.\n
\n- It is part of the Sankari Range and lies within the Govind Pashu Vihar National Park and Sanctuary.<\/li>\n\n\n\n
- It is a source of the Yamuna river<\/strong>, whose source lies above Yamnotri<\/strong>, on the west end of the massif below White Peak.<\/li>\n<\/ul>\n<\/li>\n\n\n\n
- Bara-Shigri glacier<\/strong>\u00a0which is the\u00a0second longest glacier in Himalaya after Gangotri<\/strong>, is located in the\u00a0Chandra valley of Lahaul<\/strong>.\n
\n- The name comes from the Lahaul dialect, where Bara means big and Shigri means glacier.<\/li>\n\n\n\n
- The glacier feeds the Chenab river<\/strong>.<\/li>\n<\/ul>\n<\/li>\n\n\n\n
- Milam glacier<\/strong>\u00a0is a major glacier of the\u00a0Kumaon Himalaya<\/strong>.\n
\n- It is a part of the Pithoragarh district of Uttarakhand<\/strong>, India, about 15 kilometres northeast of Nanda Devi<\/strong>.<\/li>\n\n\n\n
- The glacier is the source of the <\/strong>Goriganga River<\/strong>. <\/li>\n<\/ul>\n<\/li>\n\n\n\n
- Mandakini river<\/strong>\u00a0is a\u00a0tributary of the Alaknanda river<\/strong>\u00a0which originates from the\u00a0Chorabari glacier near Kedarnath<\/strong>\u00a0in Uttarakhand, India.\n
\n- Mandakini is fed by Vasukiganga river<\/strong> at Sonprayag. Mandakini joins Alaknanda at Rudraprayag<\/strong>.<\/strong><\/li>\n\n\n\n
- Alaknanda then proceeds towards Devaprayag<\/strong> where it joins Bhagirathi River to form the Ganges River.<\/li>\n\n\n\n
- Mandakini river flows along NH-107<\/strong> in Rudraprayag district and turns violent during monsoon, often destroying parts of the highway and adjoining villages.<\/li>\n<\/ul>\n<\/li>\n\n\n\n
- Siachen glacier<\/strong>\u00a0is located in the\u00a0eastern Karakoram range<\/strong>\u00a0in the Himalayas just\u00a0northeast of the point <\/strong>NJ9842<\/strong>\u00a0where the LOC\u00a0between\u00a0India\u00a0and\u00a0Pakistan\u00a0ends.\n
\n- The glacier\u2019s melting waters are the main source of the Nubra River<\/strong> in the Indian region of Ladakh, which drains into the Shyok River<\/strong>.<\/li>\n\n\n\n
- The Shyok in turn joins the 3000 kilometre-long Indus River<\/strong> which flows through Pakistan.<\/li>\n<\/ul>\n<\/li>\n\n\n\n
- Zemu glacier<\/strong>\u00a0is the\u00a0largest glacier in the Eastern Himalaya<\/strong>.\n
\n- It is located at the base of Kangchenjunga<\/strong> in the Himalayan region of Sikkim, India.<\/li>\n\n\n\n
- The Zemu glacier drains the east side of Kanchenjunga, the world\u2019s third highest mountain.<\/li>\n\n\n\n
- The glacier is the source of water for numerous rivers<\/strong>, as it feeds them when it melts. One of them is the Teesta river<\/strong>.<\/li>\n<\/ul>\n<\/li>\n\n\n\n
- Manas river<\/strong>\u00a0is a\u00a0transboundary river<\/strong>\u00a0in the Himalayan foothills between\u00a0southern Bhutan and India.<\/strong>\n
\n- \u200b<\/strong>It is the largest river system of Bhutan<\/strong>.<\/li>\n\n\n\n
- The total length of the river is 400 kilometres which flows through Tibet, China for 24 km, flows in Bhutan for 272 kilometres and then flows through Assam for 104 kilometres before it joins the mighty Brahmaputra River at Jogighopa<\/strong>.<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n\n\n\n
Must Read: Important Glaciers in India<\/a><\/strong><\/p>\n\n\n