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Alphabetical List of Indian Cities

A

Agra
Ajanta
Ajmer
Ahmedabad 
Andaman
Alappuzha
Arunachal Pradesh
Aurangabad
 

B

Bangalore
Bandhavgarh
Belur
Bharatpur
Bhopal 
Bombay
Bikaner
 Bodhgaya
Bhubaneshwar
Bundi
 

C

Cochin
 Calcutta
Chandigarh
Chennai
Chitradurga
 

D

Dalhousie
Dharamshala
  Delhi 
  Darjeeling
 

E

Ellora
Ernakulam
 

G

Gangtok

   Goa

   Gwalior
Guwahati
 

H

Hariyana
Helebid
Hyderabad
 

I

Idukki

J

   Jaipur
   Jaisalmer
   Jammu
Jamnagar
Jodhpur
 

K

Kanha
Kalimpong
    Kashmir
Kasaragod
   Kaziranga
    Khajuraho
Kannur
  Kinnuar
Kodaikanal
Konark
Kota
Kovalam
Kozhikode
Kullu
 

 L

    Ladakh

Leh
    Lucknow
 

M

    Mumbai
   Madurai
    Manali
    Malappuram
Meghalaya
Mizoram
Mount Abu
    Mysore
 

N

    Nalanda
Nubra Valley
 

O

   Ooty
    Orchha
 

P

  Palakkad
Pathanamthitta
 Patna
Pemayangtse
Pondicherry
Pune
Punjab
Puri
 

R

Rajkot
Rajgir
 

S

Sasangir
Sawai Madhopur
Shanti Niketan
Shimla
Srirangapatna
Sibsagar
Sundarban
 

T

Tiruchirapalli
Thanjavur
Thiruvananthapuram
Thrissur
 

U

  Udaipur

 

V

  Vaishali
   Varanasi
 

W

Wayanad

 

Monastery, Ladakh

Ladakh

Mahatma Budhha

Ladakh is a land like no other. Bounded by two of the world's mightiest mountain ranges, the Great Himalaya and the Korakaram, it lies athwart two other, the Ladakh range and the Zanskar range.

In geological terms, this is a young land, formed only a few million years ago by the buckling and folding of the earth's crust as the Indian sub-continent pushed with irresistible force against the immovable mass of Asia. Its basic contours, uplifted by these unimaginable tectonic movements, have been modified over the millennia by the opposite process of erosion, sculpted into the form we see today by wind and water.

Yes, water! Today, a high -altitude desert, sheltered from the rain-bearing clouds of the Indian monsoon by the barrier of the Great Himalaya, Ladakh was once covered by an extensive lake system, the vestiges of which still exist on its south -east plateau of Rupshu and Chushul - in drainage basins with evocative names like Tso-moriri, Tsokar, and grandest of all, Pangong-tso.

Occasionally, some stray monsoon clouds do find their way over the Himalaya, and lately this seems to be happening with increasing frequency. But the main source of water remains the winter snowfall. Dras, Zanskar and the Suru Valley on the Himalayas northern flank receive heavy snow in winter; this feeds the glaciers whose meltwater, carried down by streams, irrigates the fields in summer.

For the rest of the region, the snow on the peaks is virtually the only source of water. As the crops grow, the villagers pray not for rain, but for sun to melt the glaciers and liberate their water. Usually their prayers are answered, for the skies are clear and the sun shines for over 300 days in the year.

Ladakh lies at altitudes ranging from about 9,000 feet (2750m) at Kargil to 25,170 feet (7,672m) at Saser Kangri in the Korakaram. Thus summer temperatures rarely exceed about 27-degree celcuis in the shade, while in winter they may plummet to minus 20-degree celcuis even in Leh.

Surprisingly, though, the thin air makes the heat of the sun even more intense than at lower altitudes; it is said that only in Ladakh can a man sitting in the sun with his feet in the shade suffer from sunstroke and frostbite at the same time!

 

 
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