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English Riviera Geopark
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The English Riviera Geopark (ERG) in Torbay is one of eight Geoparks in the United Kingdom, and one of fifty-three worldwide. It is the only urban Geopark, and was declared a Geopark on 16 September 2007. The Geopark covers 6,200 hectares of land and 4,100 hectares of sea bed.
Geopark status was granted to Torbay on the grounds that the area has a varied geology covering several geological periods, which are exposed to the surface in many areas, and also that Torbay Council and other bodies have worked to promote the area's distinctive geology to the community via education.
places in Torbay are part of the Geopark.

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Encyclopedia
The English Riviera Geopark (ERG) in Torbay is one of eight Geoparks in the United Kingdom, and one of fifty-three worldwide. It is the only urban Geopark, and was declared a Geopark on 16 September 2007. The Geopark covers 6,200 hectares of land and 4,100 hectares of sea bed.
Geopark status was granted to Torbay on the grounds that the area has a varied geology covering several geological periods, which are exposed to the surface in many areas, and also that Torbay Council and other bodies have worked to promote the area's distinctive geology to the community via education.
Selected sites
Many places in Torbay are part of the Geopark. Babbacombe cliffs has upside down layering of slates and limestone formed during the Variscan orogeny. Permian red breccia is also visible there. Berry Head to Sharkham Point has exposed marine cave systems. Black Head to Anstey's Cove has Torbay's largest outcrop of igneous rock. Crystal Cove has a 25 metre wide zone of calcite. Kents Cavern and Brixham Cavern contained fossils of the Woolly Rhinoceros and Cave Lion. Dyers Quarry is rich in coral fossilised in its growing position, as well as Late Eifelian limestone. Hollicombe Head to Corbyn Head have features of alluvial fan conglomerate deposits and seasonal river sandstones, both Permian in origin. Hopes Nose features gold and palladium mineral deposits left by hydrothermal fluids, and the area is also important for the study of Quaternary stratigraphy and sea level change. Long Quarry features evidence of the development, formation and growth of a stromatoporoid reef. Lummaton Quarry's shell deposits led to the naming of the Devonian period. Saltern Cove is a regionally important unconformity and Site of Special Scientific Interest.
See also
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