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Kotu Baig Springs

Ghizer, Gilgit-Baltistan, Pakistan
Kotu Baig Springs
Location
Ghizer, Gilgit-Baltistan, Pakistan
Water type
sulfurous
Temperature
40 °C
pH
6.5

Water profile

Thermicity
Sedative
40 °C
LowHigh

Relaxing — deep, immediate muscle release.

Mineralisation
Bio-active
LowHigh

Rich in active gases or metals — a strong mineral character.

Buoyancy
Standard buoyancy
LowHigh

Soft water — natural, classic buoyancy.

SoufreSulfuresSulfates

Kotu Baig Springs is a natural geothermal site in the remote Gilgit-Baltistan region of northern Pakistan, one of the world's most mountainous and geologically dynamic territories where the Himalayas, Karakoram, and Hindu Kush mountain ranges converge and where lightly mineral oligomineral thermal water surfaces from the ancient basement rocks along active fault systems. The springs serve the highland communities of Gilgit-Baltistan, who have long used natural thermal water for bathing within the thermal traditions of the Shina, Balti, and Burusho peoples. The extraordinary landscape of Gilgit-Baltistan — home to K2, four other 8,000-metre peaks, and some of the world's greatest concentration of glaciers outside the polar regions — provides a setting of unparalleled mountain grandeur.

Insider tip — Kotu Baig Springs rise in the Ghizer Valley of Gilgit-Baltistan, where the Hindu Kush, Karakoram, and Himalayan ranges converge in a tectonic knot that generates intense geothermal activity. The springs emerge beside the Ghizer River at an elevation where poplar trees turn brilliant gold each October, framing the steam pools in dramatic color. Local Kho people have used these waters for generations as treatment for skin ailments and cold-weather fatigue.
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Frequently asked questions

How hot is the water?
The water runs quite hot here, around 40 °C — a sedative water that brings immediate muscle release.
What type of water is found here?
This spot features sulfurous water.
What is the best season to visit?
The most favourable period for this spot is: Toute l'année (idéal automne-hiver).