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Rock Lifeboat Station

Buildings and structures in CornwallLifeboat stations in Cornwall
RNLI Lifeboat Station, Rock geograph.org.uk 2442654
RNLI Lifeboat Station, Rock geograph.org.uk 2442654

Rock Lifeboat Station is the base for Royal National Lifeboat Institution (RNLI) search and rescue operations on the River Camel in Cornwall, United Kingdom. It operates a D-class (IB1) lifeboat, which since 2014 has been the Rusper II.

Excerpt from the Wikipedia article Rock Lifeboat Station (License: CC BY-SA 3.0, Authors, Images).

Rock Lifeboat Station
Rock Road,

Geographical coordinates (GPS) Address Nearby Places
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Wikipedia: Rock Lifeboat StationContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 50.54428 ° E -4.92343 °
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Address

Rock Road
PL27 6FD , St. Minver Lowlands
England, United Kingdom
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RNLI Lifeboat Station, Rock geograph.org.uk 2442654
RNLI Lifeboat Station, Rock geograph.org.uk 2442654
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Nearby Places

Brea Hill
Brea Hill

Brea Hill (Cornish: Bre, meaning hill), pronounced "Bray Hill" is a round hill beside the River Camel estuary in north Cornwall, England, United Kingdom The hill is 62 metres (203 ft) high and there are Bronze Age tumuli (burial mounds) at the summit. The underlying geology in this area of Cornwall is Devonian slates. Brea Hill is situated at the south end of Daymer Bay between the settlements of Trebetherick and Rock in the civil parish of St Minver Lowlands. approximately five miles northwest of WadebridgeOn the west side, Brea Hill rises straight from the foreshore; on the north and south it rises from low sand dunes. To the east, the dunes give way to a golf course and grassland with St Enodoc's Church (where the poet Sir John Betjeman is buried) just below the hill. Brea Hill is within the Rock Dunes SSSI (Site of Special Scientific Interest). The reason that Brea Hill is such a positive feature in the landscape is that the centre of the hill, west to east, is a dolerite dyke, well-seen from the beach on the west and in the quarry on the east slope and in both exposures soft-sediment deformation is seen implying the intrusion followed shortly after deposition of the material which later became slate during the Variscan Orogeny. The dyke is shown on the British Geological Survey map Sheets 335 and 336, and memoir, for the Geology around Trevose Head and Camelford. The South West Coast Path follows the west flank of the hill with an alternative route passing to the east. Brea Hill is grassed and treeless (except for a small wooded area low on the south flank) with rough footpaths leading to the summit and burial mounds.