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Daily Life In India Homework Help

daily life in india homework help

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Entrust your academic achievements to the hands of our professional writers and you will be getting an outstanding opportunities to do my uni essay for me from now on! Other religions, notably Buddhism and Jainism , originated in India—though their presence there is now quite small—and throughout the centuries residents of the subcontinent developed a rich intellectual life in such fields as mathematics, astronomy, architecture, literature, music, and the fine arts.

Throughout its history, India was intermittently disturbed by incursions from beyond its northern mountain wall.

Especially important was the coming of Islam , brought from the northwest by Arab, Turkish, Persian, and other raiders beginning early in the 8th century ce. Eventually, some of those raiders stayed; by the 13th century much of the subcontinent was under Muslim rule, and the number of Muslims steadily increased.

Only after the arrival of the Portuguese navigator Vasco da Gama in and the subsequent establishment of European maritime supremacy in the region did India become exposed to major external influences arriving by sea, a process that culminated in the decline of the ruling Muslim elite and absorption of the subcontinent within the British Empire.

Direct administration by the British, which began in , effected a political and economic unification of the subcontinent. When British rule came to an end in , the subcontinent was partitioned along religious lines into two separate countries—India, with a majority of Hindus, and Pakistan , with a majority of Muslims; the eastern portion of Pakistan later split off to form Bangladesh.

Many British institutions stayed in place such as the parliamentary system of government ; English continued to be a widely used lingua franca; and India remained within the Commonwealth. Hindi became the official language and a number of other local languages achieved official status , while a vibrant English-language intelligentsia thrived.

India remains one of the most ethnically diverse countries in the world. Apart from its many religions and sects, India is home to innumerable castes and tribes, as well as to more than a dozen major and hundreds of minor linguistic groups from several language families unrelated to one another.

Religious minorities, including Muslims, Christians, Sikhs, Buddhists, and Jains, still account for a significant proportion of the population; collectively, their numbers exceed the populations of all countries except China. Earnest attempts have been made to instill a spirit of nationhood in so varied a population, but tensions between neighbouring groups have remained and at times have resulted in outbreaks of violence.

At independence, India was blessed with several leaders of world stature, most notably Mohandas Mahatma Gandhi and Jawaharlal Nehru , who were able to galvanize the masses at home and bring prestige to India abroad.

The country has played an increasing role in global affairs. The history section of the articles Pakistan and Bangladesh discuss those countries since their creation.

It is bounded to the northwest by Pakistan , to the north by Nepal , China , and Bhutan ; and to the east by Myanmar Burma. Bangladesh to the east is surrounded by India to the north, east, and west. The island country of Sri Lanka is situated some 40 miles 65 km off the southeast coast of India across the Palk Strait and Gulf of Mannar.

The land of India—together with Bangladesh and most of Pakistan—forms a well-defined subcontinent, set off from the rest of Asia by the imposing northern mountain rampart of the Himalayas and by adjoining mountain ranges to the west and east. In area, India ranks as the seventh largest country in the world. India has two union territories composed entirely of islands: When the two finally collided approximately 50 million years ago , the northern edge of the Indian-Australian Plate was thrust under the Eurasian Plate at a low angle.

The collision reduced the speed of the oncoming plate, but the underthrusting, or subduction, of the plate has continued into contemporary times. The effects of the collision and continued subduction are numerous and extremely complicated.

An important consequence, however, was the slicing off of crustal rock from the top of the underthrusting plate. Those slices were thrown back onto the northern edge of the Indian landmass and came to form much of the Himalayan mountain system.

The new mountains—together with vast amounts of sediment eroded from them—were so heavy that the Indian-Australian Plate just south of the range was forced downward, creating a zone of crustal subsidence. Continued rapid erosion of the Himalayas added to the sediment accumulation, which was subsequently carried by mountain streams to fill the subsidence zone and cause it to sink more. Further information on the geology of India is found in the article Asia.

That great, geologically young mountain arc is about 1, miles 2, km long, stretching from the peak of Nanga Parbat 26, feet [8, metres] in the Pakistani-administered portion of the Kashmir region to the Namcha Barwa peak in the Tibet Autonomous Region of China. Between those extremes the mountains fall across India, southern Tibet, Nepal, and Bhutan.

The width of the system varies between and miles and km. North of the Himalayas are the Plateau of Tibet and various Trans-Himalayan ranges, only a small part of which, in the Ladakh region of Jammu and Kashmir state in the Indian-administered portion of Kashmir , are within the territorial limits of India. Because of the continued subduction of the Indian peninsula against the Eurasian Plate, the Himalayas and the associated eastern ranges remain tectonically active.

As a result, the mountains are still rising, and earthquakes —often accompanied by landslides —are common. Several since have been devastating, including one in in what is now Bihar state that killed more than 10, people.

In another tremor the Bhuj earthquake , farther from the mountains, in Gujarat state, was less powerful but caused extensive damage, taking the lives of more than 20, people and leaving more than , homeless. Still others—notably the quake in Pakistani-administered Kashmir and the temblor in Nepal —principally affected those regions but also caused widespread damage and hundreds of deaths in adjacent parts of India.

The relatively high frequency and wide distribution of earthquakes likewise have generated controversies about the safety and advisability of several hydroelectric and irrigation projects. The southernmost of the three mountain belts are the Outer Himalayas, also called the Siwalik or Shiwalik Range. Crests in the Siwaliks, averaging from 3, to 5, feet to 1, metres in elevation, seldom exceed 6, feet 2, metres. The range narrows as it moves east and is hardly discernible beyond the Duars , a plains region in West Bengal state.

Interspersed in the Siwaliks are heavily cultivated flat valleys dun s with a high population density. To the south of the range is the Indo-Gangetic Plain. Weakly indurated, largely deforested, and subject to heavy rain and intense erosion, the Siwaliks provide much of the sediment transported onto the plain.

To the north of the Siwaliks and separated from them by a fault zone, the Lesser Himalayas also called the Lower or Middle Himalayas rise to heights ranging from 11, to 15, feet 3, to 4, metres.

Their ancient name is Himachal Sanskrit: The mountains are composed of both ancient crystalline and geologically young rocks, sometimes in a reversed stratigraphic sequence because of thrust faulting. The Lesser Himalayas are traversed by numerous deep gorges formed by swift-flowing streams some of them older than the mountains themselves , which are fed by glaciers and snowfields to the north.

The northernmost Great, or Higher, Himalayas in ancient times, the Himadri , with crests generally above 16, feet 4, metres in elevation, are composed of ancient crystalline rocks and old marine sedimentary formations. Between the Great and Lesser Himalayas are several fertile longitudinal vales; in India the largest is the Vale of Kashmir , an ancient lake basin with an area of about 1, square miles 4, square km.

Other high mountains in India include Nanda Devi 25, feet [7, metres] , Kamet 25, feet [7, metres] , and Trisul 23, feet [7,] in Uttarakhand. The Great Himalayas lie mostly above the line of perpetual snow and thus contain most of the Himalayan glaciers. Those are especially prominent in the northwest, where the Zaskar Range and the Ladakh and Karakoram ranges all in Jammu and Kashmir state run to the northeast of the Great Himalayas.

Also in Jammu and Kashmir is the Pir Panjal Range , which, extending along the southwest of the Great Himalayas, forms the western and southern flanks of the Vale of Kashmir. Collectively, the latter group is also designated as the Shillong Meghalaya Plateau.

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India is mainly an agricultural country, however it also has a large iron and steel industry and produces every type of manufactured goods. Life in India is very different in .

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