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Whitecliff Bay
Whitecliff Bay is a sandy bay near Foreland which is the easternmost point of the Isle of Wight, England, about two miles south-west of Bembridge and just to the north of Culver Down. The bay has a shoreline of around and has a popular sandy shingle beach which is over half a mile long. It is a tourist site with three holiday parks in the vicinity of the bay; it has two cafes though minimal facilities. Access is limited and only possible down two steeply sloping concrete tracks. The site is of major geological interest, being part of the Whitecliff Bay And Bembridge Ledges SSSI. Geology Whitecliff Bay has nearly identical geology to the lesser known Alum Bay, being a coastal section of the same strata which run east–west across the island. It displays a classic sequence of fossil-bearing Eocene beds of soft sands and clays, separated by an unconformity from the underlying Cretaceous Chalk Formation forming the headland of Culver Down to its south. Due to geological foldi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Horseshoe Bay, Isle Of Wight
Horseshoe Bay is a small bay on the south-east coast of the Isle of Wight, England. It lies at the east end of the headland of Culver Down. It faces south-east towards the English Channel and its shoreline is approximately in length. It should not be confused with a similarly named Horseshoe Bay about southwest at Bonchurch. The seabed is rocky and the beach comprises a steep bank of flint pebbles. The cliffs are sheer, concave and are made of chalk, which is unstable and persons on the beach are at risk of being injured by falling rocks dislodged by the many seabirds that use the cliff as a breeding ground. Horseshoe Bay lies north-north-east and adjacent to, two caves known as The Nostrils. These can be reached by scrambling over a small rocky outcrop and are partly submerged at high tide. The beach can only be reached at high tide by boat; but in low tide it can be reached at beach level from the headland from Whitecliff Bay. At a certain time of the year, on very low ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bembridge
Bembridge is a village and civil parish located on the easternmost point of the Isle of Wight. It had a population of 3,848 according to the 2001 census of the United Kingdom, leading to the implausible claim by some residents that Bembridge is the largest village in England. Bembridge is home to many of the Island's wealthiest residents. The population had reduced to 3,688 at the 2011 Census. Bembridge sits at the extreme eastern point of the Isle of Wight. Prior to land reclamation the area of Bembridge and Yaverland was almost an island, separated from the remainder of the Isle of Wight by Brading Haven. On the Joan Blaeu map of 1665, Bembridge is shown as ''Binbridge Iſle'', nearly separated from the rest of Wight by River Yar. Prior to the Victorian era Bembridge was a collection of wooden huts and farmhouses, which only consolidated into a true village with the building of the church in 1827 (later rebuilt in 1846). Facilities The historical heart of the village is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bays Of The Isle Of Wight
A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or another bay. A large bay is usually called a gulf, sea, sound, or bight. A cove is a small, circular bay with a narrow entrance. A fjord is an elongated bay formed by glacial action. A bay can be the estuary of a river, such as the Chesapeake Bay, an estuary of the Susquehanna River. Bays may also be nested within each other; for example, James Bay is an arm of Hudson Bay in northeastern Canada. Some large bays, such as the Bay of Bengal and Hudson Bay, have varied marine geology. The land surrounding a bay often reduces the strength of winds and blocks waves. Bays may have as wide a variety of shoreline characteristics as other shorelines. In some cases, bays have beaches, which "are usually characterized by a steep upper foreshore with a broad, flat fronting terrace".Maurice Schwartz, ''Encyclopedia of Coastal Science'' (2006), p. 129. Bays were sig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tourist Attractions On The Isle Of Wight
Tourism is travel for pleasure or business; also the theory and practice of touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tours. The World Tourism Organization defines tourism more generally, in terms which go "beyond the common perception of tourism as being limited to holiday activity only", as people "travelling to and staying in places outside their usual environment for not more than one consecutive year for leisure and not less than 24 hours, business and other purposes". Tourism can be domestic (within the traveller's own country) or international, and international tourism has both incoming and outgoing implications on a country's balance of payments. Tourism numbers declined as a result of a strong economic slowdown (the late-2000s recession) between the second half of 2008 and the end of 2009, and in consequence of the outbreak of the 2009 H1N1 influenza virus, but slowly recovered until the COVID-19 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Priory Bay
Priory Bay is a small privately owned bay on the northeast coast of the Isle of Wight, England. It lies to the east of Nettlestone village and another mile along the coast from Seaview. It stretches from Horestone Point in the north to Nodes Point in the south, the bay is surrounded by woodland known as Priory Woods owned by the National Trust. The bay faces east towards Selsey Bill and has a shoreline and can be accessed by walking round Horestone Point from Seagrove Bay. Geography The northern part of the bay has a straight coastline that makes a beach that is sandy with some pebbles. At the southern end the bay curves round to the east. Here the coast is rocky with evidence of walls and buttresses that were built to protect the coastline. These have largely been breached and lie scattered along the shore. The cliffs around the bay rise to around but are under 'active erosion' from the sea, particularly affecting the southern part of the bay. The seabed is predominantly ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandown
Sandown is a seaside resort and civil parishes in England, civil parish on the south-east coast of the Isle of Wight, United Kingdom with the resort of Shanklin to the south and the settlement of Lake, Isle of Wight, Lake in between. Together with Shanklin, Sandown forms a built-up area of 21,374 inhabitants. The northernmost town of Sandown Bay, Sandown has an easily accessible, sandy shoreline with beaches that run continuously from the cliffs at Battery Gardens in the south to Yaverland in the north. Geography The town grew as a Victorian era, Victorian resort surrounded by a wealth of natural features. The coastal and inland areas of Sandown are part of the Isle of Wight Biosphere Reserve designated by UNESCO's Man and the Biosphere Programme in June 2019, and Sandown's sea front and clifftops form part of the Isle of Wight Coastal Path. The Bay that gives Sandown its name is an excellent example of a concordant coastline with five miles of well-developed tidal be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
French Invasion Of The Isle Of Wight (1545)
The French invasion of the Isle of Wight occurred during the Italian Wars in July 1545. The invasion was repulsed. France had a long history of attacking the Isle of Wight, and the 1545 campaign proved to be the last time to date that the French have attempted to take it. Although the French forces, led by Claude d'Annebault, greatly outnumbered those of the English, the battles fought (including the battles of the Solent and Bonchurch) ended without a clear winner. However, as the French were repelled, it could be considered an English victory. Although the operation was inconclusive, the English suffered heavily, including the loss of the carrack ''Mary Rose'' in the Battle of the Solent. Details of the conflict have not been very well recorded, and some accounts claim that the French were defeated at each battle rather easily. French strategy was to effect a landing at Whitecliff Bay and cross Bembridge Down to attack Sandown, and another landing at Bonchurch with a view ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Molluscs
Mollusca is the second-largest phylum of invertebrate animals after the Arthropoda, the members of which are known as molluscs or mollusks (). Around 85,000 extant taxon, extant species of molluscs are recognized. The number of fossil species is estimated between 60,000 and 100,000 additional species. The proportion of undescribed species is very high. Many taxa remain poorly studied. Molluscs are the largest marine biology, marine phylum, comprising about 23% of all the named marine organisms. Numerous molluscs also live in freshwater mollusc, freshwater and Terrestrial molluscs, terrestrial habitats. They are highly diverse, not just in size and anatomical structure, but also in behaviour and habitat. The phylum is typically divided into 7 or 8 Taxonomy (biology), taxonomic class (biology), classes, of which two are entirely extinct. Cephalopod molluscs, such as squid, cuttlefish, and octopuses, are among the most neurobiology, neurologically advanced of all inve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossil Hunting
Fossil collecting (sometimes, in a non-scientific sense, fossil hunting) is the collection of fossils for scientific study, hobby, or profit. Fossil collecting, as practiced by amateurs, is the predecessor of modern paleontology and many still collect fossils and study fossils as amateurs. Professionals and amateurs alike collect fossils for their scientific value. A commercial trade in fossils has also long existed, with some of this being practised illegally. Process Locating fossils Rock type Fossils are generally found in sedimentary rock with differentiated strata representing a succession of deposited material. The occurrence of fossil bearing material depends on environmental factors before and after the time of preservation. After death, the first preserving factor is a rapid burial in water bodies or terrestrial sediment which would help in preserving the specimen. These rocks types are usually termed clastic rock, and are further subdivided into fine, medium and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeocene
The Paleocene, ( ) or Palaeocene, is a geological epoch that lasted from about 66 to 56 million years ago (mya). It is the first epoch of the Paleogene Period in the modern Cenozoic Era. The name is a combination of the Ancient Greek ''palaiós'' meaning "old" and the Eocene Epoch (which succeeds the Paleocene), translating to "the old part of the Eocene". The epoch is bracketed by two major events in Earth's history. The K–Pg extinction event, brought on by an asteroid impact and possibly volcanism, marked the beginning of the Paleocene and killed off 75% of living species, most famously the non-avian dinosaurs. The end of the epoch was marked by the Paleocene–Eocene Thermal Maximum (PETM), which was a major climatic event wherein about 2,500–4,500 gigatons of carbon were released into the atmosphere and ocean systems, causing a spike in global temperatures and ocean acidification. In the Paleocene, the continents of the Northern Hemisphere were still connected via ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalk Formation
The Chalk Group (often just called the Chalk) is the lithostratigraphic unit (a certain number of rock strata) which contains the Upper Cretaceous limestone succession in southern and eastern England. The same or similar rock sequences occur across the wider northwest European chalk 'province'. It is characterised by thick deposits of chalk, a soft porous white limestone, deposited in a marine environment. Chalk is a limestone that consists of coccolith biomicrite. A biomicrite is a limestone composed of fossil debris ("bio") and calcium carbonate mud ("micrite"). Most of the fossil debris in chalk consists of the microscopic plates, which are called coccoliths, of microscopic green algae known as coccolithophores. In addition to the coccoliths, the fossil debris includes a variable, but minor, percentage of the fragments of foraminifera, ostracods and mollusks. The coccolithophores lived in the upper part of the water column. When they died, the microscopic calcium carbonate pla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
