Hobbs Quarry
Encyclopedia
Hobbs Quarry is a 0.5 hectare
Hectare
The hectare is a metric unit of area defined as 10,000 square metres , and primarily used in the measurement of land. In 1795, when the metric system was introduced, the are was defined as being 100 square metres and the hectare was thus 100 ares or 1/100 km2...

 geological Site of Special Scientific Interest near Shepton Mallet
Shepton Mallet
Shepton Mallet is a small rural town and civil parish in the Mendip district of Somerset in South West England. Situated approximately south of Bristol and east of Wells, the town is estimated to have a population of 9,700. It contains the administrative headquarters of Mendip District Council...

 on the Mendip Hills
Mendip Hills
The Mendip Hills is a range of limestone hills to the south of Bristol and Bath in Somerset, England. Running east to west between Weston-super-Mare and Frome, the hills overlook the Somerset Levels to the south and the Avon Valley to the north...

 in Somerset
Somerset
The ceremonial and non-metropolitan county of Somerset in South West England borders Bristol and Gloucestershire to the north, Wiltshire to the east, Dorset to the south-east, and Devon to the south-west. It is partly bounded to the north and west by the Bristol Channel and the estuary of the...

, notified in 1984.

This disused quarry, which now forms the back of a builders merchants yard, is a Geological Conservation Review Site which demonstrates early Jurassic
Jurassic
The Jurassic is a geologic period and system that extends from about Mya to  Mya, that is, from the end of the Triassic to the beginning of the Cretaceous. The Jurassic constitutes the middle period of the Mesozoic era, also known as the age of reptiles. The start of the period is marked by...

 transgression, with steeply-dipping Carboniferous Limestone
Carboniferous limestone
Carboniferous Limestone is a term used to describe a variety of different types of limestone occurring widely across Great Britain and Ireland which were deposited during the Dinantian epoch of the Carboniferous period. They were formed between 363 and 325 million years ago...

being overlain by flatter-lying massive limestones (of early Jurassic age) known as the Downside Stone.

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