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Ultimately, only one third was disafforested, and commissioners were appointed to ensure any further encroachments did not leave the common lands as the most meagre in quality. However, by this time large-scale quarrying had already begun.Quarry works were set in motion in the 1870s at Tank Quarry and at Little Malvern by Pyx Granite Company.The quality of Malvern water is attributable to its source.The rocks of the Malvern Hills are amongst the oldest and hardest found in England; the geology is responsible for the quality of Malvern's spring water.The Hills Conservators lobbied parliament to pass an Act limiting the exploitation, and although a second Act was passed in 1924 its provisions were largely ineffective. In 1989, the cafe on Worcestershire Beacon burned down.As the Malvern Hills Acts state that no building should be erected on the Conservators' land or on land under their jurisdiction, the Conservators put a bill through Parliament to get the power to build a new one but the House of Lords opposed it.However, excavations at nearby Midsummer Hillfort, Bredon Hill and Croft Ambrey all show evidence of violent destruction around the year 48 AD.This may suggest that the British Camp was abandoned or destroyed around the same time.

There is therefore no evidence that Roman presence ended the prehistoric settlement at British Camp.

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.

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