Thar Desert in the context of "Jodhpur"

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⭐ Core Definition: Thar Desert

The Thar Desert (Hindi pronunciation: [t̪ʰaːɾ]), also known as the Great Indian Desert, is an arid region in the north-western part of the Indian subcontinent that covers an area of 200,000 km (77,000 sq mi) in India and Pakistan. It is the world's 18th-largest desert and the world's 9th-largest hot subtropical desert.

About 85% of the Thar Desert is in India, and about 15% is in Pakistan. The Thar Desert is about 4.56% of the total geographical area of India. More than 60% of the desert lies in the Indian state of Rajasthan; the portion in India also extends into Gujarat, Punjab, and Haryana. The portion in Pakistan extends into the provinces of Sindh and Punjab (the portion in the latter province is referred to as the Cholistan Desert). The Indo-Gangetic Plain lies to the north, west and northeast of the Thar desert, the Rann of Kutch lies to its south, and the Aravali Range borders the desert to the east.

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Thar Desert in the context of Northwestern Indian subcontinent

Northwest India is a loosely defined region of India. In modern-day, it consists of north-western states of the Republic of India. In historical contexts, it refers to the northwestern Indian subcontinent (including modern-day Pakistan).

In contemporary definition, it generally includes the states of Haryana, Himachal Pradesh, Punjab, Rajasthan Uttarakhand, and often Uttar Pradesh, along with the union territories of Chandigarh, Jammu and Kashmir, Ladakh, and the National Capital Territory of Delhi. Gujarat, a western coastal state, is occasionally included as well. The mountainous upper portion of Northwest India consists of the Western Himalayas, while the flat lower portion consists of the middle portion of the Indo-Gangetic plains and the Thar Desert.

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Thar Desert in the context of Punjab Plain

The Punjab Plain is a large alluvial plain in northwestern India and eastern Pakistan. The plain includes the Indian states of Punjab and Haryana and the union territory of Delhi, excluding the Shahdara district, and the eastern part of Pakistani Punjab. This plain is around 200–300 meters above mean sea level. The plain is the western part of the Indo-Gangetic Plain, and is bounded by the Sivalik Hills in the north, the Yamuna River in the east, the Thar Desert of Rajasthan to the south, the Ravi River to the northwest and Sutlej River to the southwest. The plain is extensively farmed for cereals and cotton.

The land formed of alluvium in between two rivers known as Doab is found here. 'Doab' is made up of two words — 'do' meaning two and 'ab' meaning water. Similarly 'Punjab', is also made up of two words — 'Punj' meaning five and 'ab' meaning water.

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Thar Desert in the context of North India

North India is a geographical region, loosely defined as a cultural region comprising the northern part of India (or historically, the Indian subcontinent) wherein Indo-Aryans (speaking Indo-Aryan languages) form the prominent majority population, while Tibeto-Burmans (speaking Tibeto-Burman languages) form the significant minority population. It extends from the Himalayan mountain range in the north to the Indo-Gangetic plains, the Thar Desert, till Central Highlands. It occupies nearly two-quarters of the area and population of India and includes one of the three mega cities of India: Delhi. In a more specific and administrative sense, North India can also be used to denote the northern Indo-Gangetic Plain within this broader expanse, to the Thar Desert.

Several major rivers flow through the region including the Indus, the Ganges, the Yamuna and the Narmada rivers. North India includes the states of Himachal Pradesh, Uttarakhand, Punjab and Haryana, Rajasthan, Uttar Pradesh, and union territories of Chandigarh, Delhi, Jammu and Kashmir and Ladakh. Occasionally, states of Western, Central and Eastern India are referred as "North Indian" in a broader term.

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Thar Desert in the context of Rajasthan

Rajasthan (Hindi: Rājasthāna, pronounced [ɾaːd͡ʒəsˈtʰaːn] ; lit. 'Land of Kings') is a state in northwestern India. It is the largest Indian state by area and the seventh largest by population. It covers 342,239 square kilometres (132,139 sq mi) or 10.4 per cent of India's total geographical area. It is on India's northwestern side, where it comprises most of the wide and inhospitable Thar Desert (also known as the Great Indian Desert) and shares a border with the Pakistani provinces of Punjab to the northwest and Sindh to the west, along the Sutlej-Indus River valley. It is bordered by five other Indian states: Punjab to the north; Haryana and Uttar Pradesh to the northeast; Madhya Pradesh to the southeast; and Gujarat to the southwest. Its geographical location is 23°3' to 30°12' North latitude and 69°30' to 78°17' East longitude, with the Tropic of Cancer passing through its southernmost tip.

Its major features include the ruins of the Indus Valley civilisation at Kalibangan and Balathal, the Dilwara Temples, a Jain pilgrimage site at Rajasthan's only hill station, Mount Abu, in the ancient Aravalli mountain range and eastern Rajasthan, the Keoladeo National Park of Bharatpur, a World Heritage Site known for its bird life. Rajasthan is also home to five national tiger reserves, the Ranthambore National Park in Sawai Madhopur, Sariska Tiger Reserve in Alwar, the Mukundra Hills Tiger Reserve in Kota, Ramgarh Vishdhari Tiger reserve and Karauli Dholpur tiger reserve.

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Thar Desert in the context of Western India

Western India is a loosely defined region of India consisting of western states of Republic of India. The Ministry of Home Affairs in its Western Zonal Council Administrative division includes the states of Goa, Gujarat, and Maharashtra along with the Union territory of Dadra and Nagar Haveli and Daman and Diu, while the Ministry of Culture and some historians also include the state of Rajasthan. The Geological Survey of India includes Maharashtra but excludes Rajasthan whereas Ministry of Minority Affairs includes Karnataka but excludes Rajasthan.

Madhya Pradesh is also often included and Haryana, western Uttar Pradesh and southern Punjab are sometimes included. Western India may also refer to the western half of India, i.e. all the states west of Delhi and Chennai, thus also including Punjab, Kerala and surrounding states. The region is highly industrialised, with a large urban population. Roughly, Western India is bounded by the Thar Desert in the north, the Vindhya Range in the east and north and the Arabian Sea in the west. A major portion of Western India shares the Thar Desert with North India and Pakistan and the Deccan Plateau with South and Central India.

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Thar Desert in the context of Ghaggar-Hakra River

The Ghaggar-Hakra River (IPA: [ɡʰəɡːəɾ ɦəkɾaː]) is an intermittent river in India and Pakistan that flows in force only during the monsoon season. The river is known as Ghaggar before the Ottu barrage at 29°29′15″N 74°53′33″E / 29.4875°N 74.8925°E / 29.4875; 74.8925, and as Hakra downstream of the barrage in the Thar Desert. In pre-Harappan times the Ghaggar was a tributary of the Sutlej. It is still connected to this paleochannel of the Sutlej, and possibly the Yamuna, which ended in the Nara River, presently a delta channel of the Indus River joining the sea via Sir Creek.

The Sutlej changed its course about 8,000–10,000 years ago, leaving the Ghaggar-Hakra as a system of monsoon-fed rivers terminating in the Thar Desert. The Indus Valley Civilisation prospered when the monsoons that fed the rivers diminished around 5,000 years ago, and a large number of sites from the Mature Indus Valley Civilisation (2600–1900 BCE) are found along the middle course of the (dried-up) Hakra in Pakistan. Around 4,000 years ago, the Indus Valley Civilisation declined when the monsoons further diminished, and the Ghaggar-Hakra dried up, becoming a small seasonal river.

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Thar Desert in the context of Muhammad of Ghor

Mu'izz al-Din Muhammad ibn Sam (Persian: معز الدین محمد بن سام, romanizedMuʿizz al-Dīn Muḥammad ibn Sām; c. 1144 – 15 March 1206), also known as Muhammad of Ghor or Muhammad Ghori, was a ruler from the Ghurid dynasty based in the Ghor region of what is today central Afghanistan who ruled from 1173 to 1206. Muhammad and his elder brother Ghiyath al-Din Muhammad ruled in a dyarchy until the latter's death in 1203. Ghiyath al-Din, the senior partner, governed the western Ghurid regions from his capital at Firozkoh whereas Muhammad extended Ghurid rule eastwards into South Asia, laying the foundation of Islamic rule in South Asia, which lasted after him for nearly half a millennium under evolving Muslim dynasties.

During his early career as governor of the southern tract of Ghurid Empire, Muhammad subjugated the Oghuz Turks after a series of forays and annexed Ghazni where he was installed by Ghiyath al-Din Muhammad as an independent sovereign. Expanding the Ghurid dominion east of the Indus Delta from his base in Ghazni, Muhammad crossed the river Indus in 1175, approaching it through the Gomal Pass and captured Multan and Uch from the Carmathians within a year. Afterwards, Muhammad took his army by the way of lower Sindh, endeavouring to penetrate into present-day Gujarat through the Thar Desert. However, he was wounded and his forces were routed near Mount Abu at Kasahrada by a coalition of Rajput chiefs led by the Chaulukya king Mularaja. This setback forced him to change his route for future inroads into the Indian Plains. Hence, Muhammad pressed his forces against the Ghaznavids and uprooted them by 1186, conquering the upper Indus Plain along with most of the Punjab. After expelling the Ghaznavids from their last bastion, Muhammad secured the Khyber Pass, the traditional route of entry for invading armies into northern India.

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Thar Desert in the context of Sikh Empire

The Sikh Empire was a regional power based in the Punjab region of the Indian subcontinent. It existed from 1799, when Maharaja Ranjit Singh captured Lahore, to 1849, when it was defeated and conquered by the British East India Company following the Second Anglo-Sikh War. At its peak in the mid-19th century the empire extended from Gilgit and Tibet in the north to the deserts of Sindh in the south and from the Khyber Pass in the west to the Sutlej in the east, and was divided into eight provinces. Religiously diverse, with an estimated population of 4.5 million in 1831 (making it the 19th most populous state at the time), it was the last major region of the Indian subcontinent to be annexed by the British Empire.

In 1799, Ranjit Singh of Sukerchakia Misl captured Lahore from the Sikh triumvirate which had been ruling it since 1765, and was confirmed on the possession of Lahore by the Durrani ruler, Zaman Shah. He was formally crowned on 12 April 1801 by Sahib Singh Bedi, a descendant of Guru Nanak. Ranjit Singh rose to power in a very short period, from a leader of a single misl to finally becoming the Maharaja of Punjab. By 1813 all the remaining Sikh misls had been annexed by Ranjit Singh, and the following years saw progressive expulsion of the Afghans from Punjab; the Afghan influence east of Indus ended after the fall of Multan in 1818. In the subsequent decades Durrani Afghans lost Kashmir and Peshawar to the Sikhs as well. By 1840 Ladakh and Baltistan had been brought under Sikh suzerainty by Gulab Singh. Ranjit Singh modernised his army using the latest training as well as weapons and artillery.

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