Whale Chine | |
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Coordinates: 50°36′11″N1°20′19″W / 50.60306°N 1.33861°W | |
Location | Chale, Isle of Wight |
Age | Jurassic, Cretaceous |
Elevation | 0 m |
Whale Chine is a geological feature near Chale on the south-west coast of the Isle of Wight, England (the Back of the Wight). One of a number of such chines on the island created by stream erosion of soft Cretaceous rocks, it is a narrow and steep coastal ravine dropping 140 feet through Lower Greensand rocks from clifftop farmland to Chale Bay.
Its name probably originates from the Wavell family, owners of the nearby Atherfield Farm between 1557 and 1636. [1] It is reached from a car park on the A3055 coastal road, where a stream running parallel to the cliff takes a right-angled bend to descend to the beach. [2] In the past, descent to the beach at Whale Chine could be achieved by some 126 wooden steps, since their closure in 2005, these steps were washed away by the sea in the winter storms of 2013/14. As the beach is a popular fishing site, Local fisherman have constructed a new flight of stairs by carving steps down through the rock, although this is not recommended. Despite the old steps forming part of a footpath and legal Right of Way (footpath C34, Chale Parish), the Isle of Wight Council refused to repair them, stating that "major structural works at great expense would be required to make the path safe for use with no guarantee that such works would be a permanent solution." They have been inaccessible to the public since at least 2005 and subject to a "temporary closure" since then.
Geologically the cliffs here belong to the Wealden supergroup and were deposited in a large scale meandering river and floodplain facies about 150 million years ago. [3] The cliffs are famous for their fossil content which are commonly found in flash flood sandy deposits. These deposits can usually be recognized by the abundance of pyrite rich fossilized wood, and usually form as trough shapes. These troughs are characteristic of infilled stream channels caused by the deposition of the high energy carried material and organisms. Due to this the deposits are poorly sorted and the fossils amongst them are usually broken up. [4]
Whale Chine is a popular fishing spot for many anglers. It boosts very clear sandy ground with intermittent rock features. The species caught here vary, but it is locally known as one of the best spots on the island for ray fishing: This is best from March–October. All summer species can be caught here, and it's not uncommon for shoals of mackerel and bass to drive whitebait onto the shore. Throughout the winter the fishing declines abit, with pout being the most common fish caught.
Whale Chine was the location of the wreck of the cargo ship Cormorant on 21 December 1886. [5]
A chine is a steep-sided coastal gorge where a river flows to the sea through, typically, soft eroding cliffs of sandstone or clays. The word is still in use in central Southern England—notably in East Devon, Dorset, Hampshire and the Isle of Wight—to describe such topographical features. The term 'bunny' is sometimes used to describe a chine in Hampshire. The term chine is also used in some Vancouver suburbs in Canada to describe similar features.
Blackgang Chine is the oldest amusement park in the United Kingdom, having opened in 1843. Named after a now-destroyed chine in the soft Cretaceous cliffs, it is about 6 miles from Ventnor at the southern tip of the Isle of Wight just below St Catherine's Down. Blackgang Chine and its sister park Robin Hill are owned by the Dabell family. Blackgang Chine is home to many lands of imagination, including Pirate Cove, Restricted Area 5, Fairy Land and Village, and Cowboy Town. Owing to the unstable land on which the park is situated, landslides occur frequently, meaning that attractions have been moved further inland to safer ground on several occasions.
Chale is a village and civil parish on the Isle of Wight of England, in the United Kingdom. It is located three kilometres from Niton in the south of the Island in the area known as the Back of the Wight. The village of Chale lies at the foot of St. Catherine's Down.
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.
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.
Barnes Chine is a geological feature on the south west coast of the Isle of Wight, England. The chine lies just to the west of a small rise called Barnes High and south west of the hamlet of Yafford. It is a small sandy coastal ravine, one of a number of such chines on the island created by erosion of the cliff edge made of soft Cretaceous rock.
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.
The Chilton 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 Brighstone. It is a small coastal gully, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks.
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.
Chale Bay is a bay on the south-west coast of the Isle of Wight, England. It lies to the west of the village of Chale from which it takes its name. It faces south-west towards the English Channel, its shoreline is 3+1⁄4 miles (5.2 km) in length and is gently curving. It stretches from Artherfield Point in the north-west to Rocken End in the south-east.
Widdick Chine is a geological feature on the west coast of the Isle of Wight, England. It is west of the village of Totland.
Luccombe Bay is a bay on the south-east coast of the Isle of Wight, England. It lies to the east of Luccombe Village from which it takes its name. It faces south-east towards the English Channel, its shoreline is 2⁄3 mile (1.1 km) in length. It consists of a predominantly sand and shingle beach lined with sea cliffs which range from 200 to 280 feet in height. It stretches from Horse Ledge in the north to Bordwood Ledge in the south. The sea bottom is a mixture of mud and rocks.
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.