Undulating hills of Aravali, supporting the dry deciduous
forests, provide an unbelievable wonderful ambience. The area is
rich in floral diversity- mainly medicinal plants. It has
several floral and faunal species of global conservation
importance. The rare flora comprises Kadaya (giving medicinal
gum), Gugal, amla and Moosli etc. The main trees are- Khair,
Salai, Modad, Dhavada, Khakhara, Timru. During late winters
(February-March) Khakhara-the flame of the forests- known by
many different names such as- Palash, Tesu, Kesudo, Dhak etc. is
generally in bloom with its prominent red color resembling
flames in the forests. The rare animals comprise sloth bear,
striped hyena, leopard, bluebull, porcupine, fox, small Indian
civet, Indian pangolin and a number of reptiles including
venomous and non-venomous snakes, monitor lizards, star tortoise
etc. The rare birds of this area are adjutant Stork, spoonbill,
osprey, white backed Vulture and black vultures.
The northern end of the range continues as isolated hills and
rocky ridges into Haryana state, ending in Delhi. The well-known
Delhi Ridge is the last leg of the Aravalli Range, which cross
through South Delhi and terminates into Central Delhi where
Raisina hill is its last extension. It is one of the world's
oldest mountain ranges. It dates back to a pre-Indian
subcontinental collision with the mainland Eurasian Plate. The
southern end is at Palanpur close to Ahmedabad, Gujarat. The
highest peak is Guru Shikhar in Mount Abu in Rajasthan. Rising
to 5650 feet (1722 meters), it lies near the south-western
extremity of the range, nereby the border with Gujarat District.
The city of Udaipur with its lakes lies on the south slope of
the range in Rajasthan. Numerous rivers rise amidst the ranges
together with the Luni River, the Banas River, the Sakhi ,Sabarmati,
and the Sahibi River.
Old fold mountains are portrayed by having stopped growing
higher due to the cessation of upward thrust caused by the
stopping of movement of the tectonic plates in the Earth's crust
below them. In ancient times they were extremely high but since
have worn down almost completely by millions of years of
weathering. In contrast, the Himalayas are continuously rising
young fold mountains of today. |