AJANTA ELLORA CAVES

Located near the city of Aurangabad in Maharashtra, the famous Ajanta and Ellora are cave shrines cut out of rock, by hand, and rank amongst some of the most outstanding specimens of ancient Indian architectural heritage. The 34 caves at Ellora and the 29 caves at Ajanta, were remained shrouded in obscurity for over a millennium, till John Smith, a British Army Officer, accidentally stumbled upon them while on a hunting expedition in 1819. Ajanta has been designated as a World Heritage Site, to be preserved as an artistic legacy that will come to inspire and enrich the lives of generations to come.

Ajanta Caves
It was only in the 19th century, that the Ajanta group of caves, lying deep within the Sahyadri hills, cut into the curved mountain side, above the Waghora river, were discovered. They depict the story of Buddhism, spanning a period from 200 BC to 650 AD.

The 29 caves were built as secluded retreats of the Buddhist monks, who taught and performed rituals in the Chaityas and Viharas, the ancient seats of learning, and nerve - centers of the Buddhist cultural movement. Using simple tools like hammer and chisel, the monks carved out the impressive figures adorning the walls of these structures. Many of the caves house panels depicting stories from the Jatakas, a rich mine of tales of the several incarnations of the Buddha. Images of nymphs and princesses amongst others, are also elaborately portrayed.

Ellora Caves
The Ellora caves, 34 in number, are carved into the sides of a basaltic hill, 30 kms from Aurangabad. The finest specimens of cave - temple architecture, they house elaborate facades and exquisitely adorned interiors. These structures representing the three faiths of Hinduism, Buddhism and Jainism, were carved during the 350 AD to 700 AD period. The 12 caves to the south are Buddhist, the 17 in the centre dedicated to Hinduism, and the 5 caves to the north are Jain.

The sculpture in the Buddhist caves accurately convey the nobility, grace and serenity inherent in the Buddha. Caves 6 and 10 house images from the Buddhist and Hindu faith, under the same roof, the latter dedicated to Vishwakarma, the patron saint of Indian craftsmen. The Vishvakarma cave is both a Chaitya and a Vihara, with a seated Buddha placed in the stupa. Its two - storied structure sports a colourful pageant of dwarfs, dancing and making music.

GEOLOGY OF HIMALAYAS

Ecology

The flora and fauna of the Himalayas varies with climate, rainfall, altitude, and soils. The climate ranges from tropical at the base of the mountains to permanent ice and snow at the highest elevations. The amount of yearly rainfall increases from west to east along the front of the range. This diversity of climate, altitude, rainfall and soil conditions generates a variety of distinct plant and animal communities.

Lowland forests

On the Indo-Gangetic plain at the base of the mountains, an alluvial plain drained by the Indus and Ganga-Brahmaputra river systems, vegetation varies from west to east with rainfall. The xeric Northwestern thorn scrub forests occupy the plains of Pakistan and the Indian Punjab. Further east lie the Upper Gangetic plains moist deciduous forests of Uttarakhand and Uttar Pradesh and Lower Gangetic plains moist deciduous forests of Bihar and West Bengal. These are monsoon forests, with drought-deciduous trees that lose their leaves during the dry season. The moister Brahmaputra Valley semi-evergreen forests occupy the plains of Assam.

The Terai belt

Above the alluvial plain lies the Terai strip, a seasonally marshy zone of sand and clay soils. The Terai has higher rainfall than the plains, and the downward-rushing rivers of the Himalaya slow down and spread out in the flatter Terai zone, depositing fertile silt during the monsoon season and receding in the dry season. The Terai has a high water table due to groundwater percolating down from the adjacent zone. The central part of the Terai belt is occupied by the Terai-Duar savanna and grasslands, a mosaic of grasslands, savannas, deciduous and evergreen forests that includes some of the world's tallest grasslands. The grasslands of the Terai belt are home to the Indian Rhinoceros (Rhinoceros unicornis).

Bhabhar belt

Above the Terai belt is an upland zone known as the Bhabhar, a zone of porous and rocky soils, made up of debris washed down from the higher ranges. The Bhabhar and the lower Shiwalik ranges have a subtropical climate. The Himalayan subtropical pine forests occupy the western end of the subtropical belt, with forests dominated by Chir Pine (Pinus roxburghii). The central part of the range is home to the Himalayan subtropical broadleaf forests, dominated by sal (Shorea robusta).

Shiwalik Hills

Also called Churia or Margalla Hills, Sivalik Hills is Intermittent outermost range of foothills extending across Himalayan region through Pakistan, India, Nepal and Bhutan. Consists of many sub-ranges. Summits generally 600 to 1,200 meters. Steeper southern slopes form along a fault zone called Main Frontal Thrust; northern slopes are gentler. Permeable conglomerates and other rocks allow rainwater to percolate downslope into the Bhabhar and Terai, supporting only scrubby forests upslope.

Inner Terai or Dun Valleys

The Inner Terai valleys are open valleys north of Shiwalik Hills or nestled between Shiwalik subranges. Examples include Dehra Dun in India and Chitwan in Nepal.

Lesser Himalaya

Prominent range 2,000 to 3,000 meters high forming along the Main Boundary Thrust fault zone with a steep southern face and gentler northern slopes. Nearly continuous except for river gorges. Rivers gather in candelabra form to the north to break through this range in relatively few places.

Midlands

'Hilly' region averaging about 1,000 meters immediately north of the Mahabharat Range, rising over about 100 km to about 4,000 meters at the Main Frontal Thrust fault zone where the Greater Himalaya begin.

• Montane forests - At the middle elevations of the range, th e subtropical forests yield to a belt of temperate broadleaf and mixed forests, with the Western Himalayan broadleaf forests at the western end of the range, and the Eastern Himalayan broadleaf forests in Assam and Arunachal Pradesh. Above the broadleaf forests are the Western and Eastern Himalayan subalpine conifer forests.

Alpine shrub and grasslands

Shilla (7026 m) above the Spiti Valley in Kashmir

Above the tree line are the Northwestern, Western, and Eastern Himalayan alpine shrub and meadows, which yield to tundra in the higher Himalayan range. The alpine meadows are the summer habitat of the endangered Snow Leopard (Uncia uncia).

Origins and growth

The 6,000 km plus journey of the India landmass (Indian Plate) before its collision with Asia (Eurasian Plate) about 40 to 50 million years ago.

The Himalayas are among the youngest mountain ranges on the planet and consist mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, their formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. This is referred to as a fold mountain.

The collision began in the Upper Cretaceous period about 70 million years ago, when the north-moving Indo-Australian Plate, moving at about 15 cm per year, collided with the Eurasian Plate. About 50 million years ago, this fast moving Indo-Australian plate had completely closed the Tethys Ocean, the existence of which has been determined by sedimentary rocks settled on the ocean floor and the volcanoes that fringed its edges. Since these sediments were light, they crumpled into mountain ranges rather than sinking to the floor. The Indo-Australian plate continues to be driven horizontally below the Tibetan plateau, which forces the plateau to move upwards. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.

The Indo-Australian plate is still moving at 67 mm per year, and over the next 10 million years it will travel about 1,500 km into Asia. About 20 mm per year of the India-Asia convergence is absorbed by thrusting along the Himalaya southern front. This leads to the Himalayas rising by about 5 mm per year, making them geologically active. The movement of the Indian plate into the Asian plate also makes this region seismically active, leading to earthquakes from time to time.

Glaciers and river systems

Glaciers near by K2 in Pakistan.

The Himalayan range encompasses about 15,000 glaciers, which store about 12,000 km³ of freshwater. The 70 km long Siachen Glacier at the India-Pakistan border is the second longest glacier in the world outside the polar region. Some of the other more famous glaciers include the Gangotri and Yamunotri (Uttarakhand), Nubra, Biafo and Baltoro (Karakoram region), Zemu (Sikkim) and Khumbu glaciers (Mount Everest region).

The higher regions of the Himalayas are snowbound throughout the year in spite of their proximity to the tropics, and they form the sources for several large perennial rivers, most of which combine into two large river systems:

• The western rivers combine into the Indus Basin, of which the Indus River is the largest. The Indus begins in Tibet at the confluence of Sengge and Gar rivers and flows southwest through Pakistan to the Arabian Sea. It is fed by the Jhelum, the Chenab, the Ravi, the Beas, and the Sutlej rivers, among others.

• Most of the other Himalayan rivers drain the Ganga-Brahmaputra Basin. Its two main rivers are the Ganga and the Brahma and the Yamuna among other tributaries. The Brahmaputra originates as the Yarlung Tsangpo River in western Tibet, and flows east through Tibet and west through the plains of Assam. The Ganga and the Brahmaputra meet in Bangladesh, and drain into the Bay of Bengal through the world's largest river delta.

The eastern-most Himalayan rivers feed the Ayeyarwady River, which originates in eastern Tibet and flows south through Myanmar to drain into the Andaman Sea.

The Salween, Mekong, the Yangtze and the Huang He (Yellow River) all originate from parts of the Tibetan plateau that are geologically distinct from the Himalaya mountains, and are therefore not considered true Himalayan rivers. Some geologists refer to all the rivers collectively as the circum-Himalayan rivers. In recent years scientists have monitored a notable increase in the rate of glacier retreat across the region as a result of global climate change. Although the effect of this won't be known for many years it potentially could mean disaster for the hundreds of millions of people who rely on the glaciers to feed the rivers of northern India during the dry seasons.

According to a UN climate report, the Himalayan glaciers that are the sources of Asia's biggest rivers could disappear by 2035 as temperatures rise and India, Tibet, Pakistan, Bangladesh, Nepal and Myanmar could experience floods followed by droughts in coming decades.

REAL VIEW OF HIMALAYAS

The Himalaya Range or Himalayas for short (Sanskrit: हिमालय, IPA pronunciation: [hɪ'mɑlijə]), meaning "abode of snow" [2]), is a mountain range in Asia, separating the Indian subcontinent from the Tibetan Plateau. By extension, it is also the name of a massive mountain system that includes the Karakoram, the Hindu Kush, and other, lesser, ranges that extend out from the Pamir Knot.

The Himalayan mountain system is the planet's highest and home to the world's highest peaks, the Eight-thousanders, which include Mount Everest and K2. To comprehend the enormous scale of this mountain range consider that Aconcagua, in the Andes, at 6,962 m (22,841 feet), is the highest peak outside Asia, whereas the Himalayan system includes over 100 mountains exceeding 7,200 meters (23,622 feet).^[1]

The Himalayan system, which includes outlying subranges, stretches across six countries: Afghanistan, Bhutan, China, India, Nepal, and Pakistan. Some of the world's major rivers, the Indus, the Ganges, the Brahmaputra, and the Yangtze, rise in the Himalayas, and their combined drainage basin is home to some 1.3 billion people. The Himalayas have profoundly shaped the cultures of South Asia; many Himalayan peaks are sacred in both Hinduism and Buddhism.

The main Himalaya range runs, west to east, from the Indus river valley to the Brahmaputra river valley, forming an arc 2,400 km long (1,491 miles), which varies in width from 400 km in the western Kashmir-Xinjiang region to 150 km in the eastern Tibet-Arunachal Pradesh region. The range consists of three coextensive sub-ranges, with the northern-most, and highest, known as the Great or Inner Himalayas.

CHAR DHAM - PLACED AT HIMALAYAS

KEDARNATH

The Celestial Jyotirlingam
Amidst the dramatic mountainscapes of the majestic Kedarnath range stands one of the twelve 'Jyotirlingas' of Kedar or Lord Shiva. Lying at an altitude of 3584 mts. on the head of river Mandakini, the shrine of Kedarnath is amongst the holiest pilgrimages for the Hindus.

Kedarnath is a majestic sight, standing in the middle of a wide plateau surrounded by lofty snow covered peaks. The present temple, built in the 8th century by Adi Shankaracharya, stands adjacent to the site of an earlier temple built by the Pandavas. The inner walls of the assembly hall are decorated with figures of various deities and scenes from mythology. Outside the temple door a large statue of the Nandi Bull stands as guard.

Dedicated to Lord Shiva, the exquisitely architectured Kedarnath temple is said to be more than a 1000 years old. Built of extremely large, heavy and evenly cut gray slabs of stones, it evokes wonder as to how these heavy slabs were handled in the earlier days. The temple has a " Garbha Griha" for worship and a Mandap apt for assemblies of pilgrims and visitors. A conical rock formation inside the temple is worshipped as Lord Shiva in his Sadashiva form.

Location
Kedarnath is situated in the Uttar Kashi district of the northern state of Uttaranchal. Very close to the Indo-Chinese border, it is the source of the Mandakini River. It is couched in the scenic locales of the Garhwal Himalayas at 3583 meters above sea level. It is very cold in the winters with the ground being covered with snow. In the summers, the mercury barely crosses the 20°C mark. The place experiences about 150 cm of rainfall during the monsoons and so the best time to visit is between May and October. Kedarnath is near to Rishikesh (234 km) and Dehradun (250 km).

History
According to legend, Lord Shiva wished to elude the Pandavas, who had come to seek penitence for having killed their kin in the battle of Kurukshetra. He took refuge in Kedarnath in the form of a bull. Bhima, one of the Pandava brothers, found Shiva amongst a herd of cattle. Having identified the meanest and most arrogant of the herd as Shiva, Bhima is said to have grabbed him by the hindquarters. What remains at the shrine in Kedarnath is the rear end of the bull, with the rest of its body scattered throughout the Garhwal. Shiva dived into the ground leaving behind him a hump on the surface. This conical protrusion is worshipped as the idol. It is the main site of the Panch Kedar temples.

There are Four Other Kedars

• Madhyamaheshwar
• Tunganath
• Kalpeshwar
• Rudranath

Three of these (barring Kalpeshwar) are in mountain meadows at higher altitudes than Kedarnath. The climb to Rudranath is the most strenuous though worth the trouble, as this meadow is one of the finest in Garhwal.

Mythological Myth
Legend has it that when the Pandavas sought penance following the great war of the Mahabharata they came in search of Lord Shiva. Arriving at this site they found that Shiva had elusively taken the form of a bull. Bhim the strongest of the Pandavas went after Shiva who dived deep into the ground. Only Shiva's tail was left in Bhim's hand. This spot is known as the Kedarnath and is also considered the main Kedar. The rest of Shiva's body emerged at four other places in Garhwal - Tunganath, Madhyamaheshwar, Kalpeshwar and Rudranath.

BADRINATH

The Abode Of Lord Vishnu
Cradled in the twin mountain ranges of Nar and Narayan is the holiest of the four main shrines, Badrinath along the left bank river Alaknanda. With the splendid Neelkanth mountains as the backdrop, it is an important destination on the scared itinerary of every devour Hindu. Once the spot was carpeted with 'badris' or wild berries and hence was famous as 'Badri Van'.

Badrinath is considered the holiest of the four important shrines in Garhwal. The town is at an altitude of 3,133 m. above sea level, situated on the left bank of river Alaknanda and exactly between the two mountains Nara and Narayan. The shrine is dedicated to Vishnu, the preserver and falls in the religious itinerary of every devout Hindu.

The present temple was built about two centuries ago by Garhwal Kings. It is a conical structure, 15 m. tall and has small cupola of a gilt bull and spire. There are 15 idols in the temple complex, each sculpted in black stone. The principal idol represents Vishnu in a meditative posture and is flanked by Nara-Narayan. Legend dates it prior to the Vedic age though it is believed to have been re-established by Adi Shankaracharya, an important Hindu saint in 8th century A.D. Some of the other images include Laxmi (Vishnu's consort), Garud (Vishnu's mount), Shiva & Parvati and Ganesha.

The temple has been renovated several times due to damages by avalanches. It looks fairly modern now due to the colourful "Singh Dwara" or the main entrance gate. It has three parts- Garbha Griha (the sanctum sanctorum), Darshan Mandap (for pujas) and Shobha Mandap (for devotees to assemble). The revered shrine is still alive with myriad legends from mythology. Its sanctity is emphasised in the ancient scriptures as "There are many sacred spots of pilgrimage in the heavens, earth and the nether world, but there has been none equal to Badri, nor shall there be".

Mythological Legend
Legend has it, when the Ganga was requested to descend to earth to help suffering humanity, the earth was unable to withstand the force of its descent. Therefore the mighty Ganaga was split into twelve holy channels. Alaknanda was one of them that later became the abode of Lord Vishnu or Badrinath.

The temple of Shri Badrinathji on the banks of the Alaknanda river, dates back to the vedic times. Situated at an altitude of 3,133 mts., the present temple is believed to have been built by Adi Guru Shankaracharya- an 8th century's philosopher-saint, who also established a 'math' here. Also known as 'Vishal Badri', Badrinath is one of the Panch Badris.

YAMUNOTRI

The Sacred Origin Of the Yamuna
The Garhwal Himalayas have been blessed with some of the holiest Hindu pilgrimage sites and Yamunotri is one such. One of the Char Dhams according to Hindu mythology, Yamunotri is the origin of the sacred river Yamuna. Famous for its thermal springs and glaciers, it is one of the most important stopovers on the itinerary of the Hindu pilgrim. According to an old legend, Asit Muni, the revered sage, used to reside here.

Location and Climate
Perched at an altitude of 3293 meters above sea level, Yamunotri is located in the Uttarkashi district of the northern state of Uttar Pradesh. It is very close to the Indo-Chinese border and is surrounded by the Himalayan offshoots on all sides. Yamunotri, lies near the Bandarpunch Mountain, which is 6315 m high and lies to the north. The glacial lake of Saptarishi Kund, on the Kalind Parbat, at an altitude of 4421 m, is the real source of the Yamuna River. Yamunotri is at a distance of 278 km from Dehradun, 236 km from Rishikesh, 176 km from Chamba, and 21 km from Sanya Chatti. It remains cool even during summers. The winters are snow-bound and temperatures fall below 0°C. One is advised to carry light or heavy woolens depending on the time of visit.

The first stopover for the Char Dham Yatra is the westernmost shrine of Yamunotri in the Garhwal Himalayas. Dedicated to Goddess Yamuna, it is perched atop a flank of the Bandar Poonchh peak (3165 mts. above sea level) and is situated opposite to Gangotri. The shrine attracts devotees in large numbers from May to October.

Yamunotri is the source of the revered river Yamuna which originates from the Champassar Glacier lying 1 km ahead of the shrine, at an altitude of 4421 mts. Pilgrims do not frequently visit the source of the river as it is not easily accessible.

Yamunotri finds a special mention in the Hindu mythology. According to a legend, this secluded hilly spot was the home of an ancient sage, Asit Muni.

Among the major attractions of Yamunotri are hot water springs nearby. Devotees prepare rice and potatoes to offer at the shrine, by dipping them in these hot water springs, tied in muslin cloth.

The trek to Yamunotri is spectacular, dominated by a panorama of rugged peaks and dense forests.

From Rishikesh, a 213 kms. journey by road takes one to Hanumanchatti. From here, the remaining 13 kms. trek is covered on foot or on ponies. Palanquins and Porters are also available on hire.

Prime Pilgrimage Attractions Yamunotri Temple The main temple is dedicated to Goddess Yamuna. The present temple was built by Maharani Guleria of Jaipur in the late nineteenth century. Once destroyed by an earthquake, it has been rebuilt. A holy dip in the nearby tank filled by hot springs and cooking rice in its water are common rituals performed by the devotees. Surya Kund One of the important thermal springs known for its very high temperature of 190°F. Pilgrims cook rice and potatoes here to offer to the deity in the temple. Divya Shila A huge rock pillar venerated before entering the Yamunotri Temple. Hanumanchatti The confluence of Hanuman Ganga and Yamuna rivers forms the starting point for the scenic Dodi TaL Trek. Sayanachatti A scenic spot along the banks of river Yamuna that makes a lovely sight enroute the trek upto Yamunotri. Chamba A sylvan spot on way to Tehri that offers an excellent view of the Himalayan peaks. Situated at an altitude of 1,676 mts., Chamba is an ideal summer retreat.

GANGOTRI

Gangotri - The Eternal Gift Of Bhagirath's Penance
Be it man's urge to placate the Gods above or to quench his desire for adventure, Gangotri is an ideal location. Gangotri, the origin of the sacred river Ganges, attracts tourists in large numbers every year. The confrontation with the daunting rivers and attempts to unravel the mysteries of the supernatural world are ubiquitous sights here. Along with the thrill of conquering nature, what one experiences here is the mystical aura that India is so famous for.

Location
Couched in the magnificent Garhwal hills, Gangotri is at an altitude of 3048 meters above sea level. It is on the northernmost part of the state of Uttar Pradesh and is very near the Indo-Tibetan border. It is approximately 300 km from Dehradun, 250 km from Rishikesh and 105 km from Uttarkashi. The summers are relatively cool and winters are freezing cold, with rains in the months of May and June. For the devotees and tourists, the gates of the temple are open only in the months of May to November.

Mythological Legend
According to an old legend, Lord Shiva rewarded King Bhagirath after his penance and Ganga came down to earth. However, due to her pride, and the fact that the earth would be devastated if Ganga came down in her full force, Lord Shiva caught her in his locks. It was then proclaimed that Goddess Uma or Parvati, Shiva's consort, would bathe in the Ganges daily and only then would she descend on the earth. The sacred stone near the temple denotes the place where Ganga first came down to earth. This is why Ganga is also called by the name of Bhagirathi.

Unique Pilgrimage Attraction Submerged Shivling The natural rock Shivling, submerged in the river, is an amazing sight reinforcing the power of the divine. According to mythology, Lord Shiva sat at this spot to receive the Ganaga in his matted locks. The shivling is visible in the early winters when the water level goes down. The picturesque pilgrimage in the hinterlands of the Himalayas is the most sacred spot where Ganga, the stream of life, touched earth for the first time. Mythological Mystery According to mythology, Goddess Ganga- the daughter of heaven, manigested herself in the form of a river to absolve the sins of King Bhagirath's predecessors, following his severe penance of several centuries. Lord Shiva received into his matted locks to minimise the immense impact of her fall. She came to be called Bhagirathi at her legendary source. A long the right bank of Bhagirathi stands the shrine of Gangotri dedicated to the Goddess. Perched at a height of 3042 mts., it was constructed in the early 18th century by a Gorkha Commander, Amar Singh Thapa. Every year, lakhs of pilgrims throng the sacred temple between May and October. By November, Gangotri is covered by snow. It is believed that the Goddess retreats to Mukhba, her winter abode.

Prime Pilgrimage Attraction Gangotri Temple The 18th century's temple dedicated to Goddess Ganga is located near a sacred stone where King Bhagirath worshipped Lord Shiva. Ganga is believed to have touched earth at this spot. According to another legend, Pandavas performed the great 'Deva Yagna' here to atone the deaths of their kinsmen in the epic battle of Mahabharata. The temple is an exquisite 20 ft. High structure made of white granite.