Mandi district is mostly rock. CGWB's 2013 booklet puts about 65% of it in old crystalline and metamorphic hard rock, where yields are low (under 3 litres a second) and springs and hand pumps are the usual sources; 32% in Siwalik and Subathu rocks, low to moderate (2–10 litres a second); and only about 3% in valley alluvium — the Balh valley, part of Sarkaghat and small pockets — where yields are high (10–30 litres a second).
CGWB, Mandi District booklet (2013)
Yes. CGWB records artesian, free-flowing conditions in low-lying ground along the Suketi khad in the south-west of the Balh valley — water rises out of the well on its own. In the rest of the district, a bore needs a pump.
CGWB's own guide for the district: in the valley's soft deposits, tube wells of 100–120 m by percussion or rotary rigs; in hard rock, bore wells of 100–150 m by DTH with ODEX — the air-hammer method for rock, with casing driven through the boulders. It also notes the Balh valley's development stage was 15% — 'safe', with room for more wells.
In the Balh valley, CGWB records tube wells 38 to 141 metres deep. In the hard rock that covers about two-thirds of the district, state hand-pump bores are 30 to 60 metres. The right depth depends on the site.
It depends on the ground. CGWB rates the valley alluvium high (10–30 litres a second), the Siwalik rocks low to moderate (2–10) and the hard rock low (under 3). Balh valley tube wells gave 15 to 999 litres a minute.
Yes, by project. We are at Bhunter, just up the Beas from Aut and the Mandi district line. Call or WhatsApp with the location.
Central Ground Water Board, Ground Water Information Booklet, Mandi District (September 2013) — cgwb.gov.in/sites/default/files/2022-10/mandi.pdf Checked 8 October 2026.
Site enquiry
Where the site is, what the water is for, and whether the rig truck can reach it. We call you back — or send it on WhatsApp.