Search Any thing About Nagpur The Orange City...



The present city was founded in the early 18th century by Bhakt Buland, a Gond prince of the kingdom of Deogad in the Chhindwara district. Seeing the advantage of civilized life in Delhi, he started to build Nagpur as his new capital. His successor Chand Sultan continued the work. On Chand Sultan's death in 1739, disputes regarding succession arose and Raghuji Bhonsle, the Maratha governor of Berar, helped to restore the elder son to the throne. As the dissentions continued, Raghuji Bhonsle again intervened in 1743, and the control of Nagpur slowly passed on from the Gonds to the Marathas. It became the capital of the Bhonsles.

HOW TO REACH NAGPUR

Road Links : The district is well connected by roads with all industrial centres of the Country. National Highways passing through Nagpur are Bombay Calcutta NH-6 & Kanyakumari Varanasi NH-7.


The length of the roads in the Nagpur district is as under :
National Highways 230 km.
Major State Highway 129 km.
State Highways 699 km.
Major District Roads 717 km.
Other District Roads 1043 km.
Village and Other Roads 2974 km.

Rail Links : Electrified broad gauge railway track connects Nagpur to all four major metros. The length of broad gauge railwayline is 266.06 kms and that of narrow gauge railway line is 134.32 kms. Destinations connected included Mumbai, Delhi, Calcutta, Chennai, Kolhapur, Pune, Ahmedabad, Hyderabad, Jammu, Amritsar, Lucknow, Varanasi, Bhubaneshwar, Trivendrum, Cochin, Gorakhpur, Visakhapatnam, Bangalore, Mangalore, Patna, Indore.

Air Routes : The Sonegaon Airport is 8 kilometers south of Nagpur City. It is connected to Mumbai, Calcutta, Delhi Hyderabad, Pune, Bhubaneswar, Raipur.

The underlying rock type in the Western and Southern localities is Deccan Trap, the lava flows gave rise to flat topped and terraced features. The Eastern halfs covered by crystalline Metamorphic Rock such as gneiss’s, schist and granites. In the Northern part of the city, yellowish sand stones and clays of the lower Gondwana formations are found. In maximum part of the town, the underlying rock strata are covered with alluvial deposits resulting from the flood plain of the Kanhan River. In some places these gives rise to granular, sandy soils, but in many places, particularly in low lying, poorly drained areas, the soils are alluvial
clays with poor permeability characteristics.