Manimahesh Kailash or Mountain Kailash is in the watershed of the Budhil valley, which forms part the mid-Himalayan range of hills near Kugti pass and at Harsar. The perpetually snow-covered glacial peak, at the head of its own range, is the source of the
sacred lake of Manimahesh situated beneath it. Manimahesh Ganga River originates in a cascade from the lake and joins the Budhil River on its left bank. This hill range is a contiguous spur that conjoins the main range near the Bara Banghal pass of the
Pir Panjal range. After the Budhal River rises from the slopes of the Kukti (Kugati) pass and Bada Bangal pass, the watershed formed by the Budhil and Ravi rivers takes the form of an inverted triangle with its base at Khadamukh. Budhil itself is formed by several streams which rise from different faces of the Manimahesh Kailas peak. The streams which rise from the peak are: the 'Bhujla' (derived from Bhuja meaning the arm) from the left flank of the peak, which meets Bhudil (also spelt Budhal) below Kukti village; the Dhancho nala, rising from the snowy ranges of the southern flank of the peak, flows in northward direction; Androl stream carrying holy waters of the Manimahesh Lake flowing to the north of the peak and through the Barachundi Meadow, the Siv Karotar stream rises from the foot of the peak and joins Androl; and the Gauri stream from the Gauri Kund joins Androl. All these streams constitute the Dhancho nala that has a confluence with Budhil at Hadsar. In view of so many streams originating from the Manimhesah Peak and the Manimhaesh Lake, and all of which are also linked to legends and the annual yatra pilgrimage, the Budhal or Budhil River is also highly venerated by the Gaddi elders and is nicknamed as 'Bhujl'. Pir Pinjal lies in the lesser Himalayan Zone, which forms the central part of the state of Himachal Pradesh. The peak lies along the water shed between the
Chenab River on the one side and
Ravi and
Beas on the other side. A research study has been carried out on the glacial status of this peak and its range by the
Geological Survey of India. It indicated that the Manimahesh Kailash peak is part of the range, which is long. The average elevation of the studied peaks is . The glacial melt from this range flows towards the north and extends over an area of . The ice content of the glacier has been assessed as 0.137 cubic km. The composition of this proglacial region is reported to be a mixture of ground/recessional moraines with linear country outcrops protruding out. The glaciation must have extended up to a little downstream of Dhanchu as revealed by the terminal moraine hump. During the last 37 years, the glacier receded by with an average retreat of /year. The area vacated is estimated at . == Climb ==