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Landour 1869 Landour. Landour is located in the Lower Western Himalaya, in the Mussoorie Range, the second of the five parallel folds of the Himalaya.On average, Landour is about 984 ft (300 m) above Mussoorie, which itself is mostly at an altitude of 6,800 to 7,798 ft (2,073 to 2,377 m).
Situated in the foothills of the Garhwal Himalayan range located 40 km (25 mi) from New Tehri, the district headquarter, 30 km from the hill station of Mussoorie. Dhanaulti is a tehsil in Tehri Garhwal district, Uttarakhand, India. Dhanaulti is located on the important tourist circuit of Landour, Mussoorie, Kanatal, Chamba and New Tehri. The ...
Mussoorie is at an average altitude of 2,005 metres (6,578 ft). To the northeast are the Himalayan snow ranges, and to the south, the Doon Valley and Shiwalik ranges. The second highest point is the original Lal Tibba in Landour, with a height of over 2,275 m (7,464 ft). Mussoorie is popularly known as The Queen of the Hills. [4] [5]
It is situated 16 km (9.9 mi) away from Landour cantonment, 57 kilometres (35 mi) from Mussoorie and 148 kilometres (92 mi) from New Tehri in the Tehri Garhwal district of Uttarakhand. The Nag Tibba Range is one of the three principal ranges of the Lesser Himalayas , along with the Dhauladhar and the Pir Panjal , which branch off from the Great ...
The British captured the area in 1816 and founded the cities of Landour and Mussourie in 1827–28. The district was added to the Garhwal division in the 1970s. It was established as the capital of Uttarakhand after the establishment of the state as Uttaranchal in the year 2000.
Several recalls were issued in 2024 for Ford Motor Company vehicles. The recall report data is from Jan. 1, 2024, to Dec. 27, 2024. The U.S. Department of Transportation (DOT) compiles data from ...
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The area is known as Jaunsar-Bawar, [2]. In 1901, Chakrata Tehsil was part of the Dehradun district, of United Provinces, with a collective population of 51,101, which consisted of the towns of Chakrata (population 1250) and Kalsi, with a population of 760, [2] which is most known for the rock edict of the Mauryan king Ashoka 2nd century BC, first discovered by John Forest, in 1860.