Born above, pure by nature
The Shivalik subterranean aquifer
Deep beneath the outer Himalayan foothills, rain and alpine snowmelt percolate across centuries of ancient sandstone. Naturally pressurized and pristine, Himspring rises without surface contamination.
64
TDS (mg/L)
180 to 220M
Aquifer depth
Shivalik Spring
Source
7.6
pH balance
Chapter I — Geological filtration
Centuries of subterranean refinement
Sub-surface rainwater travels through dense sandstone, quartz, and alluvial gravel layers in the Shivalik basin. This natural micro-filtration strips away all impurities while dissolving optimal trace minerals.
The result is a low-TDS profile of 64 mg/L with an exceptionally smooth, soft palate mouthfeel and a naturally alkaline pH of 7.6.
Subterranean sandstone percolation in the Shivalik foothills
Confined aquifer geology at 180m to 220m depth
Chapter II — Hydrogeological security
Sealed beneath 200 metres of impermeable rock
Unlike shallow surface springs exposed to rain variations and agricultural runoff, Himspring is drawn from a confined hydrogeological pocket sealed by thick clay capstones.
Natural sub-artesian pressure lifts the water gently to the surface wellhead where it is captured directly into bottles without chemical treatment or storage tanks.
Chapter III — Provenance parameters
Uncompromising water standards
Range
Shivalik, Outer Himalaya
Aquifer depth
180 to 220 metres
Pressure system
Sub-artesian self-rising flow