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Brook Bay is a bay on the south western coast of the Isle of Wight, England. It lies to the west of the village of Brook. It faces south west out into the English Channel. It stretches about 2km from Hanover Point in the east to Sudmoor Point to the west. Much of the surrounding land, including the hamlet of Brookgreen is owned by the National Trust.
The beach is predominantly sand. The seabed is rocky to the west as it consists of the hazardous Brook Ledges but is rock-free near the concrete slipway. [1]
The bay is best accessed from the nearby car park and the slipway down to the beach.
Both Brook Chine and Churchill Chine empty into Brook Bay.
The Isle of Wight Coastal Path runs along the cliff edge for the entire extent of the bay
Alum Bay is a bay near the westernmost point of the Isle of Wight, England, within close sight of the Needles rock formation. Of geological interest and a tourist attraction, the bay is noted for its multi-coloured sand cliffs. The waters and adjoining seabed form part of the Needles Marine Conservation Zone and the shore and heath above are part of the Headon Warren and West High Down Site of Special Scientific Interest.
Brook is a village and former civil parish, now in the parish of Brighstone, on the Isle of Wight, England. In 1931 the parish had a population of 156. On 1 April 1933 the parish was abolished and merged with Brighstone.
Colwell Bay is a bay in the west of the Isle of Wight. It is located between the towns of Totland and Yarmouth. The bay's northernmost point is Cliff's End the closest point of the Island to the British mainland, with Hurst Castle lying at the end of a long peninsula just 1500 metres to the northwest. The southernmost point is Warden Point.
Compton Bay is a bay located on the southwest section of the Isle of Wight, England. Its northwestern edge is defined by the distinctive white chalk cliff of Freshwater Cliff, named after adjacent Freshwater Bay, which forms a small cove with the village of Freshwater situated just behind. Its northeastern edge is formed from the soft red and orange lower cretaceous rocks of Brook Bay, which are rapidly eroding.
The Isle of Wight Coastal Path is a circular long-distance footpath of 70 miles (113 km) around the Isle of Wight, UK. It follows public footpaths and minor lanes, with some sections along roads.
Luccombe Chine is a geological feature and visitor attraction south of the village of Luccombe on the Isle of Wight, England. A wooded coastal ravine, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks, it leads from the clifftop to Luccombe Bay.
Walpen Chine is a geological feature on the south west coast of the Isle of Wight, England. It is west of the village of Chale. It is a sandy coastal ravine, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks. It leads from the 190 feet high clifftop next to the Isle of Wight coastal path to a knickpoint approximately halfway down the cliff face above Chale Bay beach.
Ladder Chine is a geological feature on the south west coast of the Isle of Wight, England. It is west of the village of Chale. It is a sandy coastal ravine, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks. It leads from the 190 foot high clifftop to a knickpoint approximately halfway down the cliff face above Chale Bay beach.
New Chine is a geological feature on the south west coast of the Isle of Wight, England. It is west of the village of Chale. It is a sandy coastal ravine, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks. It leads from the 190 foot high clifftop to a knickpoint approximately one third of way down the cliff face above Chale Bay beach.
Churchill Chine is a geological feature on the south west coast of the Isle of Wight, England. It is west of the village of Brook and just east of Hanover Point. It is a small sandy coastal gully, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks. It leads from the 30 foot high clifftop to the beach of Brook Bay.
Compton Chine is a geological feature on the south west coast of the Isle of Wight, England. It lies between the village of Brook to the east and Freshwater Bay to the west. It is a small sandy coastal gully, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks. It leads from the 50 foot high clifftop to the beach of Compton Bay.
Brook Chine is a geological feature on the south west coast of the Isle of Wight, England. It lies just to the west of the village of Brook. The hamlet of Brookgreen runs along its southern edge.
Grange Chine and Marsh Chine form a geological feature on the south west coast of the Isle of Wight, England. They lie to the south of the village of Brighstone.
Shepherd's Chine is a geological feature on the south west coast of the Isle of Wight, England. It lies to the west of the village of Little Atherfield.
Cowleaze Chine is a geological feature on the south west coast of the Isle of Wight, England. It lies to the west of the village of Little Atherfield.
Shippards Chine is a geological feature on the south west coast of the Isle of Wight, England. It is west of the village of Brook and just north of Hanover Point.
Seagrove Bay is a bay on the northeast coast of the Isle of Wight, England. It lies to the east of the village of Seaview facing towards Selsey Bill with a 2⁄3 mile (1.1 km) shoreline stretching from Nettlestone Point in the north to Horestone Point in the south. The bay has both the Seaside Award Flag and the Water Quality Award.
Brighstone Bay is a bay on the south west coast of the Isle of Wight, England. It lies to the south and west of the village of Brighstone from which it takes its name. It faces south west towards the English Channel, its shoreline is 7 km in length and is gently curving. It stretches from Sudmoor Point in the north west to Artherfield Point in the south east.
Buddle Brook a small river on the Isle of Wight, England. The Brook drains water from the southern side of Brighstone Down and as far to the east as the village of Shorwell. Its flow is the greatest of the streams in the South-West of the Island. Near the village of Brighstone its body is split into a series of mill ponds built to power Yafford Mill and Brighstone Mill, and controlled ways passing through the village and under the noted local landmark, the Dragon Tree Brighstone. Beyond the village the stream is re-connected into one and flows into Grange/Marsh Chine. These are heavily vegetated and are the largest chine on the Island. The Brook runs all the way to the beach where its mouth is at least 13 ft 1 in (4m) wide. Once the stream reaches the pebble beach it soaks in and disappears.
Back of the Wight is an area on the Isle of Wight in England. The area has a distinct historical and social background, and is geographically isolated by the chalk hills, immediately to the North, as well as poor public transport infrastructure. Primarily agricultural, the Back of the Wight is made up of small villages spread out along the coast, including Brighstone, Shorwell and Mottistone.