Jim Corbett National Park - Essay Example

Elephant Safaris are the best way to explore the huge area of the reserve. Jim Corbett tiger reserve and National park geologically fall in the Outer and Shivalik foothills of the Himalayas. The park was known as the Ramganga National Park, after the tributary of Ganga that flows through the reserve from East till West, post India's independence in 1947.

It was renamed Jim Corbett National Park in 1956, to commemorate the memory of Jim Corbett. The "Project Tiger," a conservation project to save the Indian Tiger and its habitat, was launched in 1973 from this park. The special attractProject TigerThe special attraction of the park is the Bengal Tiger, which is an endangered species. In fact, the name of the park - Corbett, is after the famous hunter and naturalist Jim Corbett, who was known for the initiatives he took to save the tiger from extinction.

"Project Tiger" was started with support from the World Wide Fund for Nature by Indian conservationists. The main objective was to protect the tiger from extinction. Corbett with its thick forest cover and plenty of "food" for the tigers - the number of animal species present and also replenished by the Ramganga acted as an apt destination for a natural habitat of the endangered species. [Riley 208]Geology The Chinji Stage and Kamlial Stage are the two types of geological formations that can be found in the Jim Corbett National Park.

Red and maroon shades sandstones, sandstones of grey, purple and grey hues comprise the geological formations of the Park. The Shinji stage that characterizes the uppermost stage of the lower Siwalik geological formations consists of bright-colored sandstones. The sandstones of the area are characterized by intercalations of siltstones. Geologists have estimated these to date back to the Miocene (varying between upper and mid) age. [Negi 50 - 51]The Garhwal group's lowermost formation is Rudraprayag.

Black and grey colored slates and cherts; grey quartzite; compact, medium-grained, grayish-white, and white quartzite comprise the Rudraprayag formation. Over the Rudraprayag, formations are the Lameri formation. Divided into Lameri A, Lameri B, and Lameri C these are mainly dolomite bands, slates, and phyllites.