Ziyarat Baba Abdullah Reshi - 4 Things to Know Before Visiting

Kheer Bhawani/Ksheer Bhawani is a temple dedicated to the Goddess Kheer Bhavani (originally just Bhawani) constructed over a sacred spring. The worship of Kheer Bhawani is universal among the Hindus of Kashmir. The temple is situated at a distance of 14 miles east of Srinagar near the village of Tul Mul. The term kheer refers to rice pudding that is offered in the spring to propitiate the Goddess, which became part of the name of the temple.

Parihaspora is an old town situated near the district of Baramula at 26 km from Srinagar. This town was the capital of Kashmir during the Shankervarman Regime. It was found in the 8th century AD by the king of Kashmir, Lalityaditya Muktapid. The most popular feature of this place is the ancient archaeological monuments present at the Parihaspora Pattan and the Pattan Bazaar. Apart from these monuments, the town also houses few remains of a Buddhist Stupa and monastery.

Manasbal Lake is located in Ganderbal District in the State of Jammu and Kashmir in India. The name Manasbal is said to be a derivative of the Lake Manasarovar. Lake is encircled by three villages viz., Jarokbal, Kondabal (also called Kiln place, is situated on the north-eastern side of the lake) and Ganderbal and is stated to be the deepest lake in India.

Nigeen Lake is surrounded by a large number of willow and poplar trees. Hence, it has come to be referred to as a "nageena", which means "the jewel in the ring". The word "nigeen" is a local variant of the same word.

The Bangus Valley is a Himalayan sub-valley of the Kashmir Valley. It is situated in the North area of Kupwara District, in Jammu and Kashmir, of Indian administered Kashmir . Bangus has remained largely restricted and an unfavorable tourist spot due to the armed conflict that affects this area, and also due to the lack of infrastructure. However, in recent years, efforts have been made to bring the valley on the tourist map.

Wular lake is one of the largest freshwater lakes in Asia. The lake basin was formed as a result of tectonic activity and is fed by the Jhelum River. The lake's size varies seasonally from 12 to 100 square miles (30 to 260 square kilometers). In addition, much of the lake has been drained as a result of willow plantations being built on the shore in the 1950s.