The India Gate commemorates Indian soldiers who died in World War I
Delhi is India's main point of arrival for overseas visitors, and the major transport hub for destinations in the states of rajasthan, the Punjab, Himachal Pradesh and Ladakh as well as central north India. Delhi city, the showacse of India, has been the centre of political activity from time immemorial. The ancient fortness, majestic buildings and historic ruins find their modern counterparts in the tall skyscrapers, diplomatic enclaves and well-planned townships of New Delhi. The people here, their lifestyles, traditions and even the climate are a rich and varied mixture of all that is india.
Lotus Temple in South Delhi
Delhi is one of the oldest continually inhabited cities in the world. Having been the capital of several empires in ancient India, Delhi was a major city in the old trade routes from northwest India to the Gangetic Plains. Many ancient monuments, archaeological sites and remains of national importance have been erected in its history.[7] The Mughals built a section of the city (now known as Old City or Old Delhi) that served as the capital of Mughal Empire for a long period. During the British Raj, New Delhi was built as an administrative quarter of the city. New Delhi was declared the capital of India after India gained independence from British rule in 1947. As the seat of the Government of India, New Delhi houses important offices of the federal government, including the Parliament of India, making Delhi a powerhouse of Indian politics.
The Akshardham Temple
Public transport in Delhi is provided by buses, auto rickshaws, a rapid transit system, taxis and suburban railways.
Wednesday, January 23, 2008
Tuesday, January 22, 2008
Saturday, January 19, 2008
India Cricket News
India vs Australia Cricket Series 2007-08
IND vs AUS, Day 4, Perth Test: India end Australia's winning streak (AUS 2:1)India recorded one of their most amazing Test triumphs overseas when they beat Australia by 72 runs in the thrilling third cricket Test to snap the champion team's record 16-match winning streak at Perth on Saturday.
Set 413 to win a world record 17th Test in succession, the Australians were dismissed for 340 to allow the spirited visitors to reduce the margin to 2-1 in the four match series with one full day to spare. Not many had given the Indians any hope at the WACA, regarded as the fastest pitch in the world, but Anil Kumble and his men came out firing on all cylinders to not only pull off a sensational victory but raise hopes of levelling the series.
The Indians celebrated wildly and hugged each other after R P Singh castled last man Shaun Tait, bringing an end to a dramatic Test which saw fortune fluctuating from one team to the other on the four days.
Michael Clarke, who has struggled to find his peak form in the series, was the highest scorer for the Australians with 81 while Michael Hussey (46) and captain Ricky Ponting (45) were the other notable performers. With the hosts reeling at 253 for eight, tailenders Mitchell Johnson (50 not out) and Stuart Clark (32) used the long handle to good effect to give the Indians some anxious moments.
Saturday, January 12, 2008
Kumaon A Little paradise on Earth
Kumaon proper constituted of an old Rajput principality, which became extinct at the beginning of the 19th century after its annexation in the Gurkha war of 1815. For seventy years after the annexation, the region was governed by three administrators, Mr. Traill, Mr. J. H. Batten and Sir Henry Ramsay, on non-regulation basis. Till 1891 the division comprised of the three districts of Kumaon, Garhwal and the Terai. Later, the two districts of Kumaon and the Tarai were redistributed and renamed after their respective headquarters of Nainital and Almora.
As it is today...
Presently, the Kumaon (or Kumaun) region is spread over an area of more than 35,000 sq. kms. and is headquartered at Nainital. It is one of the two main regions and administrative divisions of Uttarakhand (earlier known as Uttaranchal), a hilly state of northern India, the other being Garhwal. The region is spread over the districts of Almora, Bageshwar, Champawat, Nainital, Pithoragarh, and Udham Singh Nagar with the town of Nainital serving as the administrative center.
Situation
It has the serene and peaceful Tibet towards its northern side, on the east is the beautiful Nepal, Uttar Pradesh lies towards the south and on the west, lays the Garhwal region. The Kumaonis, as the people of the region are called, are well known for their bravery and martial skills. The Kumaon Regiment, one of the best regiments of the Indian Army, calls Kumaon its home. Haldwani, Nainital, Rudrapur, Almora, Pithoragarh, Mukteshwar and Ranikhet are among the most important towns of the region.
Geography and the Landscape
Apart from the vast Himalayan tract, the region has two sub-mountain strips called the Terai and the Bhabhar. Up till the1850`s, the sub-mountain strips had an almost impenetrable forest that provided shelter to a large number of wild animals; but after that, the numerous clearings of trees made the area accessible and cultivable. Since then, the strips, having rich and fertile soil, attract a large number of people from the hills who cultivate the rich soil during the hot as well as the cold season and return to the hills during rains.
As for the rest of Kumaon, it is a maze of mountains, all a part of the Great Himalayas, some of which are among the loftiest known. Dotting the landscape, which is only 225 kms. in terms of length and a mere 65 kms. in breadth, are over thirty peaks rising to staggering heights of 5500 m. or more. Among the rivers rising chiefly in the southern slope of the Tibetan watershed, lying to the north of the loftiest peaks, are the Gori, Dhauli and Kali. The rivers flow through the extraordinarily deep and strikingly beautiful valleys and gorges of the Kumaon hills. The main rivers are the Sharda (Kali), the Pindari and Kailganga, whose waters join the Alaknanda. The river Sharda (Kali) also acts as the international boundary between India and Nepal. The route currently used to make the holy pilgrimage to the Kailash-Mansarovar, goes along this river, crossing into Tibet at Lipu Lekh pass.
Flora and Fauna
The Chir Pine, the Himalayan Cypress, the Pindrow Fir, Alder, Sal (or iron-wood), and Saindan are the main varieties of trees growing in the region. As far as the geological formations are concerned, Limestone, Sandstone, Slate, Gneiss and Granite are the principal ones. The area has a number of mines of Iron, Copper, Gypsum, Lead and Asbestos, but almost all of them are under-utilized.
Climate
The climate is mild except in the regions of the sub-mountain strips of Tarai and Bhabhar and the deep valleys. The amount of rainfall received by the outer Himalayan range is almost twice that of the central hills as the outer Himalayas are the first ones to be hit by the monsoons. The precipitation is normally in the average proportion of 2000 mm to 1000 mm. Winter season without snowfall is almost unheard of in the higher ridges and in some years, the snowfall is spread throughout the whole of the mountain tract. Severe frosts are witnessed often, especially in the valleys.
As it is today...
Presently, the Kumaon (or Kumaun) region is spread over an area of more than 35,000 sq. kms. and is headquartered at Nainital. It is one of the two main regions and administrative divisions of Uttarakhand (earlier known as Uttaranchal), a hilly state of northern India, the other being Garhwal. The region is spread over the districts of Almora, Bageshwar, Champawat, Nainital, Pithoragarh, and Udham Singh Nagar with the town of Nainital serving as the administrative center.
Situation
It has the serene and peaceful Tibet towards its northern side, on the east is the beautiful Nepal, Uttar Pradesh lies towards the south and on the west, lays the Garhwal region. The Kumaonis, as the people of the region are called, are well known for their bravery and martial skills. The Kumaon Regiment, one of the best regiments of the Indian Army, calls Kumaon its home. Haldwani, Nainital, Rudrapur, Almora, Pithoragarh, Mukteshwar and Ranikhet are among the most important towns of the region.
Geography and the Landscape
Apart from the vast Himalayan tract, the region has two sub-mountain strips called the Terai and the Bhabhar. Up till the1850`s, the sub-mountain strips had an almost impenetrable forest that provided shelter to a large number of wild animals; but after that, the numerous clearings of trees made the area accessible and cultivable. Since then, the strips, having rich and fertile soil, attract a large number of people from the hills who cultivate the rich soil during the hot as well as the cold season and return to the hills during rains.
As for the rest of Kumaon, it is a maze of mountains, all a part of the Great Himalayas, some of which are among the loftiest known. Dotting the landscape, which is only 225 kms. in terms of length and a mere 65 kms. in breadth, are over thirty peaks rising to staggering heights of 5500 m. or more. Among the rivers rising chiefly in the southern slope of the Tibetan watershed, lying to the north of the loftiest peaks, are the Gori, Dhauli and Kali. The rivers flow through the extraordinarily deep and strikingly beautiful valleys and gorges of the Kumaon hills. The main rivers are the Sharda (Kali), the Pindari and Kailganga, whose waters join the Alaknanda. The river Sharda (Kali) also acts as the international boundary between India and Nepal. The route currently used to make the holy pilgrimage to the Kailash-Mansarovar, goes along this river, crossing into Tibet at Lipu Lekh pass.
Flora and Fauna
The Chir Pine, the Himalayan Cypress, the Pindrow Fir, Alder, Sal (or iron-wood), and Saindan are the main varieties of trees growing in the region. As far as the geological formations are concerned, Limestone, Sandstone, Slate, Gneiss and Granite are the principal ones. The area has a number of mines of Iron, Copper, Gypsum, Lead and Asbestos, but almost all of them are under-utilized.
Climate
The climate is mild except in the regions of the sub-mountain strips of Tarai and Bhabhar and the deep valleys. The amount of rainfall received by the outer Himalayan range is almost twice that of the central hills as the outer Himalayas are the first ones to be hit by the monsoons. The precipitation is normally in the average proportion of 2000 mm to 1000 mm. Winter season without snowfall is almost unheard of in the higher ridges and in some years, the snowfall is spread throughout the whole of the mountain tract. Severe frosts are witnessed often, especially in the valleys.
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