Geography
Chester lies at the southern end of a 2-mile (3.2 km) Triassic sandstone ridge that rises to a height of 42 m within a natural S-bend in the River Dee (before the course was altered in the 18th century). The bedrock, which is also known as the Chester Pebble Beds, is noticeable because of the many small stones trapped within its strata. Retreating glacial sheet ice also deposited quantities of sand and marl across the area where boulder clay was absent.
The eastern and northern part of Chester consisted of heathland and forest. The western side towards the Dee Estuary was marsh and wetland habitats.
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