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They are known for their spring water – initially made famous by the region's many holy wells, and later through the development of the 19th-century spa town of Great Malvern, a process which culminated in the production of the modern bottled drinking water.The Malvern Hills are part of an Area of Outstanding Natural Beauty, with scenic views over both Herefordshire and Worcestershire.Malvern water is rainwater and snow meltwater that percolates through fissures created by the pressures of tectonic movements about 300 million years ago when advancing sedimentary layers of Silurian shale and limestone were pushed into and under older Precambrian rock.When the fissures are saturated, a water table forms and the water emerges as springs around the fault lines between the strata.Depending on rainfall, the flow can vary from as little as 36 litres (7.9 imp gal; 9.5 US gal) per minute to over 350 litres (77 imp gal; 92 US gal) per minute.Rainfall on the Malvern Hills is thought to be sufficient to account for all the water that runs out of the springs, reflected for example in some spring flows six to eight weeks after heavy rainfall, and in reduced flows after a dry period.

It consists of a series of faults and folds which have the effect of bringing old Malvernian rocks to the surface.Being largely hard igneous rocks, they have resisted erosion better than those of the surrounding countryside and result in a striking line of hills of which the Malvern Hills are the most impressive.