why india attract most of the tourists around the world .
About 200 million years ago, the super continent (Pangea) started to split into different land masses and moved apart. An extensive sea (Tethys) stretched along the latitudinal area presently occupied by the Himalayas.
The two land masses, the Eurasian (Angara) and the Indian sub-continent (Gondwana) moved closer and closer, then the collision happened and uplifted the highest & youngest mountain ranges on the Earth.
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There were several phases in the Himalayas building process:
Phase I - Upper Cretaceous Period. About 70 million years ago, when the Gondwana plate and Angara plate began to converge and collide. The sea-bed was folded and raised into longitudinal ridges and valleys.
Phase II - Upper Eocene Period. About 65 million years ago, the collision was much more powerful. The Tethys bed was raised high enough to cause the final retreat of the sea and its sedimentary deposits were elevated into mountain ranges and intervening basins into large river valleys. The Great and Tibetan Himalayas were uplifted.
Phase III - Middle Miocene Period. About 25 million years ago, the Lower Himalayas were formed.
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Phase IV - About 2 million years ago, the fourth Himalayan paroxysm occurred. Along with further elevation of the Himalayas ranges, compression forces squeezed and pushed southwards, The Sub Himalayas also raised and folded.
Phase V - Only 600,000 years ago, the final phase more or less determined the present geomorphic form of the Himalayan system.
However the India Plate continuously moving north at the rate of about 2 cm per year. The Himalayas are still geologically active and structurally unstable. For this reason, earthquakes are a frequent occurrence in the entire Himalayan region.
The Himalayas region is an important model for the study of geology and continents tectonics.
2) River manasa sarover :Lake Manasarovar lies at 4,590 metres (15,060 ft) above mean sea level, a relatively high elevation for a large freshwater lake on the mostly saline lake-studded Tibetan Plateau. Despite claims to the contrary, there are hundreds of higher freshwater lakes in the world, including a larger and higher freshwater lake at 4,941 metres (16,211 ft) above sea level and 495 km2 in size, Angpa Tso (East Chihpuchang Hu), further east on the Tibetan Plateau at 33-24N 90-17E. The largest freshwater lake of its size (290 km2) over 5000 meters elevation is Pumoyong Tso (Pumuoyong Tso), also on the Tibetan Plateau, at 28-34N 90-24E and 5,018 metres (16,463 ft) elevation.
Lake Manasarovar is relatively round in shape with the circumference of 88 kilometres (55 mi). Its depth reaches a maximum depth of 90 m (300 ft)[citation needed] and its surface area is 320 square kilometres (120 sq mi). It is connected to nearby Lake Rakshastal by the natural Ganga Chhuchannel. Manasarovar is near the source of the Sutlej River which is the easternmost large tributary of the Indus. Nearby are the sources of theBrahmaputra River, the Indus River, and the Karnali River (Ghaghara), an important tributary of the Ganges River.
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it is the one of famous world strange s . it was built by king shajahan for her wife muntaj mahal . it was built by milk stone . people around the world treat tajmahal as the symbol of love .... it is north india (aagra) .
allepy (kerala) : Alappuzha is a Land Mark between the broad Arabian sea and a net work of rivers flowing into it. In the early first decade of the 20th Century the then Viceroy of the Indian Empire, Lord Curzon made a visit in the State to Alleppey, now Alappuzha. Fascinated by the Scenic beauty of the place, in joy and amazement, he said, Here nature has spent up on the land her richest bounties. In his exhilaration, it is said, he exclaimed, Alleppey, the Venice of the East. Thus the sobriquet found its place in the world Tourism Map. The presence of a port and a pier, criss -cross roads and numerous bridges across them, a long and unbroken sea coast might have motivated him to make this comparison.
Alleppey has a wonderful past. Though the present town owes its existence to the sagacious Diwan Rajakesavadas in the second half of 18th century, district of Alappuzha figures in classified Literature. Kuttanad, the rice bowl of Kerala with the unending stretch of paddy fields, small streams and canals with lush green coconut palms , was well known even from the early periods of the Sangam age. History says Alappuzha had trade relations with ancient Greece and Rome in B.C and in the Middle Ages.
Carved out of erstwhile Kottayam and Kollam (Quilon) districts, Alleppey district was formed on 17th of August 1957.The name of the district Alleppey, the anglicized form was changed as ‘Alappuzha’ as per GO(P) No.133/90/RD dated 7.2.90. It is assumed that the name of Alappuzha was derived by the geographical position and physical features of the place which means ”the land between the sea and the network of rivers flowing into it". As per GO (MS) No.1026/82/(RD) dated 29.10.1982, Pathanamthitta district was newly constituted taking portions from the then Alappuzha, Kollam and Idukki districts. The area transferred from the erstwhile Alappuzha district to Pathanamthitta district is Thiruvalla taluk as a whole and part of Chengannur and Mavelikkara Taluks. Thus the present Alappuzha district comprises of six taluks namely Cherthala, Ambalapuzha, Kuttanad, Karthikappllly, Chengannur and Mavelikkara.
1) himalayas : The Himalayas are relatively young folded mountains. According the Theory of Continental Drift, there were several phases in the genesis history of the Himalayas:
About 250 million years ago, there was a single super continent (Pangea) on Earth. It was surrounded by a large ocean.About 200 million years ago, the super continent (Pangea) started to split into different land masses and moved apart. An extensive sea (Tethys) stretched along the latitudinal area presently occupied by the Himalayas.
The two land masses, the Eurasian (Angara) and the Indian sub-continent (Gondwana) moved closer and closer, then the collision happened and uplifted the highest & youngest mountain ranges on the Earth.
.jpg)
There were several phases in the Himalayas building process:
Phase I - Upper Cretaceous Period. About 70 million years ago, when the Gondwana plate and Angara plate began to converge and collide. The sea-bed was folded and raised into longitudinal ridges and valleys.
Phase II - Upper Eocene Period. About 65 million years ago, the collision was much more powerful. The Tethys bed was raised high enough to cause the final retreat of the sea and its sedimentary deposits were elevated into mountain ranges and intervening basins into large river valleys. The Great and Tibetan Himalayas were uplifted.
Phase III - Middle Miocene Period. About 25 million years ago, the Lower Himalayas were formed.
Phase IV - About 2 million years ago, the fourth Himalayan paroxysm occurred. Along with further elevation of the Himalayas ranges, compression forces squeezed and pushed southwards, The Sub Himalayas also raised and folded.
Phase V - Only 600,000 years ago, the final phase more or less determined the present geomorphic form of the Himalayan system.
However the India Plate continuously moving north at the rate of about 2 cm per year. The Himalayas are still geologically active and structurally unstable. For this reason, earthquakes are a frequent occurrence in the entire Himalayan region.
The Himalayas region is an important model for the study of geology and continents tectonics.
2) River manasa sarover :Lake Manasarovar lies at 4,590 metres (15,060 ft) above mean sea level, a relatively high elevation for a large freshwater lake on the mostly saline lake-studded Tibetan Plateau. Despite claims to the contrary, there are hundreds of higher freshwater lakes in the world, including a larger and higher freshwater lake at 4,941 metres (16,211 ft) above sea level and 495 km2 in size, Angpa Tso (East Chihpuchang Hu), further east on the Tibetan Plateau at 33-24N 90-17E. The largest freshwater lake of its size (290 km2) over 5000 meters elevation is Pumoyong Tso (Pumuoyong Tso), also on the Tibetan Plateau, at 28-34N 90-24E and 5,018 metres (16,463 ft) elevation.
Lake Manasarovar is relatively round in shape with the circumference of 88 kilometres (55 mi). Its depth reaches a maximum depth of 90 m (300 ft)[citation needed] and its surface area is 320 square kilometres (120 sq mi). It is connected to nearby Lake Rakshastal by the natural Ganga Chhuchannel. Manasarovar is near the source of the Sutlej River which is the easternmost large tributary of the Indus. Nearby are the sources of theBrahmaputra River, the Indus River, and the Karnali River (Ghaghara), an important tributary of the Ganges River.
In Hinduism
As per Hindu theology, Lake Manasa Sarovar is a personification of purity, and one who drinks water from the lake will go to the Abode of Lord Shiva after death. He is believed to be cleansed of all his sins committed over even a hundred lifetimes.
Like Mount Kailash, Lake Manasa Sarovar is a place of pilgrimage, attracting religious people from India, Nepal, Tibet and the neighboring countries. Bathing in the Manasa Sarovar and drinking its water is believed to cleanse all sins. Pilgrimage tours are organized regularly, especially from India, the most famous of which is the Kailash Manasa Sarovar Yatra which takes place every year. Pilgrims come to take ceremonial baths in the cleansing waters of the lake.
Manasasarovar lake has long been viewed by the pilgrims as being nearby to the sources of four of the greatest rivers of Asia, namely the Brahmaputra, Karnali, Indus and Sutlej. Thus it is an axial point which has been thronged to by pilgrims for thousands of years. The region was closed to pilgrims from the outside following the Chinese Invasion of Tibet; no foreigners were allowed between 1951 and 1980. After the 1980s it has again become a part of the Indian pilgrim trail.
According to the Hindu religion, the lake was first created in the mind of the Lord Brahma after which it manifested on Earth.[2] Hence, in Sanskrit it is called "Manasa sarovaram", which is a combination of the words manasa (mind) and sarovaram (lake). The lake, in Hindu religious belief, is also supposed to be the summer abode of the Hamsa goose. Considered to be sacred, the Hamsa is an important element in the symbology of the subcontinent, representing wisdom and beauty.
In Buddhism
Buddhists also associate the lake with the legendary lake known as Anavatapta in Sanskrit and Anotatta in Pali, where Queen Maya is believed to have conceived Buddha. The lake has a few monasteries on its shores, the most notable of which is the ancient Chiu Gompa Monastery built on a steep hill, looking as if it has been carved right out of the rock. The lake is very popular in Buddhist literature and associated with many teachings and stories in Buddhism. Lord Buddha, it is reported, stayed and meditated near this lake on several occasions. Buddhists say that famous Uturu-kuru divaina (island or mountain range) was nearby the Anavatapta vila. However, more evidence shows that Uturu-kuru divaina was the Kuril Islands Kuril Islands, as the Sanskrit meaning of Uturu-kuru is Northern-men as Kur meaning man, in the Ainu language. Lake Manasarovar is also the subject of the meditative Tibetan tradition, "The Jewel Tree of Tibet". A modern narration and description of the meditation was made popular by Robert Thurman.
In Jainism
As per Jainism Kailash Mansarovar is associated with first Tirthankar Lord Shree Rishabhdev. Ashtapad mountain which is near to the Kailash mountain is a place where Lord Rishabhdevji attained Nirvana (Moksh) with crores of his disciples.
taj mahal .jpg)
allepy (kerala) : Alappuzha is a Land Mark between the broad Arabian sea and a net work of rivers flowing into it. In the early first decade of the 20th Century the then Viceroy of the Indian Empire, Lord Curzon made a visit in the State to Alleppey, now Alappuzha. Fascinated by the Scenic beauty of the place, in joy and amazement, he said, Here nature has spent up on the land her richest bounties. In his exhilaration, it is said, he exclaimed, Alleppey, the Venice of the East. Thus the sobriquet found its place in the world Tourism Map. The presence of a port and a pier, criss -cross roads and numerous bridges across them, a long and unbroken sea coast might have motivated him to make this comparison.
Alleppey has a wonderful past. Though the present town owes its existence to the sagacious Diwan Rajakesavadas in the second half of 18th century, district of Alappuzha figures in classified Literature. Kuttanad, the rice bowl of Kerala with the unending stretch of paddy fields, small streams and canals with lush green coconut palms , was well known even from the early periods of the Sangam age. History says Alappuzha had trade relations with ancient Greece and Rome in B.C and in the Middle Ages.
Carved out of erstwhile Kottayam and Kollam (Quilon) districts, Alleppey district was formed on 17th of August 1957.The name of the district Alleppey, the anglicized form was changed as ‘Alappuzha’ as per GO(P) No.133/90/RD dated 7.2.90. It is assumed that the name of Alappuzha was derived by the geographical position and physical features of the place which means ”the land between the sea and the network of rivers flowing into it". As per GO (MS) No.1026/82/(RD) dated 29.10.1982, Pathanamthitta district was newly constituted taking portions from the then Alappuzha, Kollam and Idukki districts. The area transferred from the erstwhile Alappuzha district to Pathanamthitta district is Thiruvalla taluk as a whole and part of Chengannur and Mavelikkara Taluks. Thus the present Alappuzha district comprises of six taluks namely Cherthala, Ambalapuzha, Kuttanad, Karthikappllly, Chengannur and Mavelikkara.
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