Margalla Hills National Park (Urdu: مارگلہ پہاڑیاں قومی پارک) is a national park in Pakistan located in Islamabad Capital Territory, near its northern boundary with Haripur District, Khyber Pakhtunkhwa. The park includes the Margalla Hills, which form the foothills of the Himalayas, along with Shakarparian Park and Rawal Lake.
Established in 1980, it is the third-largest national park in Pakistan with an area of 17,386 hectares (42,960 acres). Tilla Charouni, with a height of 1604 m, is tallest peak in the park. The Park is a major tourist destination, with Daman-e-Koh and Pir Sohawa serving as popular hill stations, while the Monal Restaurant, Shakarparian Cultural Complex, and Lake View Park are popular picnic spots.
The park is rich in biodiversity, especially rich in Sino-Himalayan fauna, most notably gray goral, barking deer and the leopard. Combined, MHNP is home to around 600 plant species, 402 bird varieties, 38 mammals, and 27 species of reptiles.PTDC is currently constructing a chairlift project in the park.
Location
Instituted in 1980, the Margalla Hills National Park comprises the Margalla Hills (12605 hectares), the Rawal Lake, and Shakarparian Sports and Cultural complex. Located in Islamabad, the capital of Pakistan. The hill range nestles between an elevation of 685 meters at the western end and 1,604 meters on its east.
Paleontology
Millions of years ago, these mountain peaks didn’t exist. The Asian continent was mostly intact, but the Indian subcontinent was an island floating off the coast of Australia. Around 220 million years ago, around the time that Pangaea was breaking apart, the subcontinent started to move northwards. It travelled some 6,000 kilometers before it finally collided with Asia around 40 to 50 million years ago. Then, part of the Indian landmass began to go beneath the Asian one, moving the Asian landmass up, which resulted in the rise of the Himalayas. It is thought that India’s coastline was denser and more firmly attached to the seabed, which is why Asia’s softer soil was pushed up rather than the other way around. The rock formations are 40 million years old, and fossils of marine life abound, it is a clear indication that before the content collision around 40 to 50 million years ago, these hills were the seabed of the ancient ocean. Fossils of seashells, plants, petrified wood and early sea life Yorgia waggoneri are abound.
These hills are the starting point of the Himalayas. The Himalayas, which stretch some 2,900 kilometers between Pakistan, India, China, and Nepal, is the world’s tallest mountain range.
Flora and fauna
The vegetation of the southern slopes is short stuttered, comprising deciduous and evergreen trees with diverse shrub growth. In the north, stand pines and groves of oak. The fauna is mainly Indo Himalayan, with some overlapping of Palearctic species. The birds found here are residents as well as winter migrants from higher altitudes of the north, spring and summer visitor for breeding, and short day transit species arrive in spring.
Margalla Hills have a number of torrents which gush down in the monsoon. Natural springs are also present. Margalla has a variety of mammals, which include: