Which of these names connects a tributary of the indus, a mountain range in ladakh, and a breed of pony adapted to the region?

The correct answer is the Indus river. Key Points • Nubrariveroriginatesfrom the Siachen glacier. • Nubra River isa tributary of the Shyok River which is a tributary of Indus. • In Tibet, the Nubra River is known by the name Yarma Tsangpo. • It is the second-longest non-polar glacier in the world. • The Indus receives a number of Himalayan tributaries such as the Shyok, the Gilgit, the Zaskar, the Hunza, the Nubra, the Shigar, the Gasting and the Dras. • About Indus River: ​ • It is one of the largest river basins of the world, covering an area of 11,65,000 sq. km (in India it is 321, 289 sq. km and a total length of 2,880 km (in India 1,114 km). • The Indus is also knownas the Sindhu, is the westernmost of the Himalayan rivers in India. • It originates from a glacier near Bokhar Chu (31°15' N latitude and 81°40' E longitude) in the Tibetan region at an altitude of 4,164 m in the Kailash Mountain range. • In Tibet, it is known as ‘ Singi Khamban; or Lion’s mouth. • After flowing in the northwest direction between the Ladakh and Zaskar ranges, it passes through Ladakh and Baltistan. • It cuts across the Ladakh range, forming a spectacular gorge near Gilgit in Jammu and Kashmir.​

The major river systems in India have been divided into two groups the Himalayan River system and the peninsular River system. The Himalayan River system comprises the three major rivers- the Indus river system, the Ganga river system and the Brahmaputra river system. These rivers are very long and have many tributaries. The river along with its tributaries make up the River system. The rivers of Himalayan river system are even older than the Himalayas. These rivers are perennial and are the greatest source of water for northern India. Before the formation of the Himalayas these rivers were flowing into the Tethys sea and their source is the Tibetan plateau region. Most of the Himalayan rivers form the antecedent drainage pattern. Indus River System • The name of India is after the Indus river and the famous Indus valley civilization was around this river. • The source of the Indus river is Kailash range in Tibet near Mansarovar lake. • The length of the Indus river is about 3180 km and it flows through the Ladakh region of India and its length in India is 1114 km. • Some of the Himalayan tributaries of the Indus river are Zanskar river, Shyok river, Gilgit, Dras, Shigar and Hunza. • The main tributaries of the Indus river are Jhelum, Chenab, Ravi, Beas and Satluj. • The gradient of the Indus river in Jammu and Kashmir is very gentle. • The river drains into the Arabian Sea south of Karachi after forming a huge delta. Jhelum River • The Jhelum river arises from a spring at...

Hint: If a river flows into a second river, then a tributary of the second river is the first river. A water body that flows into another body of water is a tributary.River Indus is an excellent trans- Himalayan river in Asia. It covers a large area in South Asia. Complete answer: The drainage area of Indus river is about 1165000 square km. It lies in the foothills and ranges of the Hindu Kush, Himalayas, and Karakoram Range. It also lies in the semi-arid plains of Pakistan. About 58 cubic miles is the river's annual flow. The river's name is derived from a Sanskrit name from Tibet. In the ancient Vedas, the mention of the river is seen. This river rises from the autonomous region of China near Lake Mapam in southwestern Tibet. It crosses the southwest boundary of Kashmir and flows about 200 miles North West. The river Shigar joins the river Indus near the banks of Skardu in Baltistan. The river Indus gets most of its tributes from the eastern Punjab plain. The river becomes larger after it receives the water from Punjab, and during the flood season, it is complete. 1. Ravi: The Budhil and Nai or Dhona join the major tributaries of the Ravi River 64 kilometers (40 mi) downstream from its source. Thus, this option is incorrect. 2. Beas: The Beas River flows south through the Kullu Valley, receiving tributaries from flanking mountains, and then turns west to flow into the Kangra Valley past Mandi. Thus, this option is incorrect. 3. Jhelum: The Jhelum river is an Indus River ...

Aerial view of the Indus River Valley in Karakoram, Pakistan. The Indus River is fed by numerous glaciers and small rivers of the Himalayan, Hindu Kush, and Karakoram Mountain ranges. Some of the major tributaries of the Indus include the Zanskar River, the Shyok River, the Shigar River, the Gilgit River, the Astor River, the Kabul River, the Kurram River, the Gomal River, the Jhelum River, the Chenab River, the Beas River, the Ravi River, and the Sutlej River. The five major tributaries of the River Indus – Beas, Ravi, Chenab, Jhelum, and Sutlej (“Panjnad”), give the name to the region of Punjab (“the land of five rivers”) that is divided between the countries of India and Pakistan. Adjacent to the town of Tatta, in Pakistan’s Sindh Province, the Indus divides into many distributaries that form a large delta before draining into the Arabian Sea. The Indus River Delta covers an area of more than 7,800 sq. km and extends along the coast for about 120km. The climate of the Indus River Basin varies from subtropical arid and semiarid to temperate subhumid on the plains of Pakistan’s Punjab and Sindh Provinces to alpine climatic conditions in the north. In the lowlands, the annual precipitation ranges between 100 and 500mm whereas in the mountain slopes the precipitation is about 2,000mm. Since the tributaries of the Indus River are snow-fed, their flow varies greatly throughout the year, with minimum discharge during the winter months of December to February. There is a rise i...

Himalayan River Systems • The Indus, the • The Himalayan Rivers existed even before the formation of the Himalayas i.e. before the collision of the Indian Plate with the Eurasian plate. • They were flowing into the Tethys Sea.These rivers had their source in the now Tibetan region. • The deep gorgesof the Indus, the Satluj, the Brahmaputra, etc. clearly indicate that these rivers are older than the Himalayas. • They continued to flow throughout the building phase of the Himalayas; their banks rising steeply while the beds went lower and lower due to vertical erosion (Vertical down cutting was significant and was occurring at a rate faster than the rising of Himalayas), thus cutting deep gorges. • Thus, many of the Himalayan Rivers are typical examples of antecedent drainage. Indus River System • It originates from a glacier near Bokhar Chu in the Tibetan region at an altitude of 4,164 m in the Kailash Mountain range near the Mansarovar Lake. • The river flows northwest and enters in Ladakh region in India from a place called Demchok, after entering India Indus river flows in between Karakoram and Ladakh range but more closer to the Ladakh range. At a place called Dungti, the river takes a sharp southwest turn and cuts through the Ladakh range and then takes a northwestern course and continues to flow towards the Leh region of Ladakh between LadhakRangeand ZaskarRange. After reaching Leh river countinues the northwestern course and reaches the town of Batalik which is in t...

• Study Material • Magazine Download • PYQ download • UPSC Notes • 1 minute read • Daily MCQ • Difference b/w • Full Forms • Free Courses • Free content for download • Video Lectures • UA Batches • Prelims • Environment • Agriculture • Geography • History-Freedom Struggle • Art & Culture • Polity • International relation • Sci & Tech • Economy • Mains • GS 1 • GS 2 • GS 3 • GS 4 • Exam Updates • UPSC Syllabus • Exam Dates • Results • Eligibility Criteria • Mains Syllabus • Prelims Syllabus • Notifications • Test & Practice • Daily MCQ • Prelims PYQs • Mains Questions • Rankers Guide • Topper Notes • Topper Interviews • Exam Tips • Paper Analysis Introduction The Himalayan mountain range refers to the mountain range in Asia that splits up the Indian subcontinent from the Tibetan Plateau. There are three ranges of Himalayas – Outer Himalayas, Middle Himalayas, and the Inner Himalayas. The northernmost range of the Himalayas is known as Himadri or Greater Himalayas. The Himalayan Mountain Range System: • The Himalayan mountain range system has three parts, and the Himalayas is one of them • The three parts are structurally folded mountains that go over the northern borders of India • The Himalayan Ranges stretch from west to east, from the Indus to the Brahmaputra river • The three parts are formed by the tectonic collision of the Indian Plate with the Eurasian Plate • The Himalayas are the highest mountain ranges with glaciers, gorges, deep valleys, and the highest peaks in ...

Interactive map outlining Ladakh range Country India, Pakistan District City 34°40′N 76°53′E / 34.66°N 76.88°E / 34.66; 76.88 Parent range Borders on The Ladakh Range is a mountain range in central Geography [ ] The Ladakh Range is regarded as a southern extension of the The Ladakh Range forms the northeastern bank of the The Ladakh Range has an average height of about 6,000 metres and has no major peaks. Some of its peaks are less than 4,800 metres. The main mountain passes are Habitation [ ] The city of Leh was for centuries trade centre for fine Two English explorers, The nomadic Ladakh is a beautiful desert region. Culturally/geographically close to Tibet, it has few resources with an extreme climate. The The extension of the Ladakh Range into China is known as References [ ] • ^ a b c • • • • • • Bibliography [ ] • Karim, Afsir (2009), Himalayan Frontiers of India: Historical, Geo-Political and Strategic Perspectives, Routledge, pp.56–66, 978-1-134-03294-5 • Kaul, H. N. (1998), Rediscovery of Ladakh, Indus Publishing, 978-81-7387-086-6 • Mehra, Parshotam (1992), An "agreed" frontier: Ladakh and India's northernmost borders, 1846-1947, Oxford University Press, 978-0-19-562758-9 • Negi, S. S. (1998), Discovering the Himalaya, Volume 1, Indus Publishing, 978-81-7387-079-8 • Warikoo, K. (2009), "India's gateway to Central Asia: trans-Himalayan trade and cultural movements through Kashmir and Ladakh, 1846–1947", in K. Warikoo (ed.), Himalayan Frontiers of India: Historical...

The Indus civilization developed in the 3rd millennium BCE, making it one of the earliest of the world’s civilizations, and it lasted into the 2nd millennium BCE. Indus civilization, also called Indus valley civilization or Harappan civilization, the earliest known bce, though the southern sites may have lasted later into the 2nd bce. Among the world’s three earliest civilizations—the other two are those of The recovery and study of the Indus civilization The Indus civilization is known to have consisted of two large cities, Harappa and Mohenjo-daro, and more than 100 towns and villages, often of relatively small size. The two cities were each perhaps originally about 1 mile (1.6 km) square in overall dimensions, and their outstanding magnitude suggests political centralization, either in two large states or in a single great empire with Society and political system Despite a growing body of archaeological evidence, the social and political structures of the Indus “state” remain objects of conjecture. The apparent craft specialization and localized craft groupings at Mohenjo-daro, along with the great divergence in house types and size, point toward some degree of social stratification. Trade was

The Great Himalayas, which normally would form the main water divide throughout their entire length, function as such only in limited areas. That situation exists because the major Himalayan rivers, such as the Indus, the Brahmaputra, the Sutlej, and at least two headwaters of the Ganges—the Alaknanda and the Bhagirathi—are probably older than the mountains they The role of the Great Himalaya Range as a watershed, nevertheless, can be seen between the Sutlej and Indus valleys for 360 miles (580 km); the drainage of the northern slopes is carried by the north-flowing Zaskar and Dras rivers, which drain into the Indus. Baltoro Glacier moves about 6 feet (2 metres) per day, while others, such as the Khumbu, move only about 1 foot (30 cm) daily. Most of the Himalayan glaciers are in retreat, at least in part because of Soils The north-facing slopes generally have a fairly thick soil cover, supporting dense forests at lower elevations and grasses higher up. The forest soils are dark brown in colour and silt loam in texture; they are ideally suited for growing fruit trees. The mountain meadow soils are well developed but vary in thickness and in their chemical properties. Some of the wet deep upland soils of that type in the eastern Himalayas—for example, in the