Worcestershire Beacon - Geology

Geology

The hills are mostly igneous and metamorphic rocks from the late pre-Cambrian, around 600 million years old and the Beacon is part of the watershed that permits the rise of the mineral springs and wells of the famous Malvern water that is bottled commercially on a large scale and sold worldwide, and they were responsible for the development of Malvern from a village to a busy spa town in the early 19th century. Hundreds of millions of years of erosion and glacial passage have given the Beacon and its neighbouring peaks their characteristic smoothly rounded features.

Read more about this topic:  Worcestershire Beacon