Himalayan Natural Mineral Water is a still natural mineral water originating from the foothills of the Shivalik Range in the Indian Himalayas. Its natural cycle begins with glacial ice and snowmelt in the upper reaches of the mountains. The water then spends approximately 20 years passing through layers of Himalayan rock, sand, and silt that act as a natural geological filter. During this journey, it gradually acquires minerals and collects in a confined underground aquifer. The aquifer is located at a depth of approximately 120 meters and is protected by impermeable layers of clay. The water is drawn and bottled directly at its source in Dhaula Kuan near Paonta Sahib in the Indian state of Himachal Pradesh. Its pH ranges from 7.1 to 7.7, giving it a neutral to mildly alkaline character. Its natural mineral composition contributes to a mild and balanced taste without a pronounced aftertaste. Since the water contains naturally dissolved mineral salts, fine white particles may occasionally appear in the bottle because of temperature changes during storage or transportation.