The Isle of Wight is one of the richest dinosaur localities in Europe, with over 20 species of dinosaur having been recognised from the early Cretaceous Period, some of which were first identified on the island, as well as the contemporary non-dinosaurian species of crocodile, turtle and pterosaur.
William Fox was an English clergyman and palaeontologist who worked on the Isle of Wight and made some significant discoveries of dinosaur fossils.
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.
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.
Little Atherfield is a small settlement in the civil parish of Shorwell, on the Isle of Wight, England. It is near the coast in the Back of the Wight. The Isle of Wight is situated off the south coast of England.
Brighstone is a village and civil parish on the Isle of Wight, 6 miles southwest of Newport on the B3399 road. Brighstone was previously known as "Brixton". The name derives from the Saxon name "Ecgbert's Tun".
Tennyson Down is a hill at the west end of the Isle of Wight just south of Totland. Tennyson Down is a grassy, whale-backed ridge of chalk which rises to 482 ft/147m above sea level. Tennyson Down is named after the poet Lord Tennyson who lived at nearby Farringford House for nearly 40 years. The poet used to walk on the down almost every day, saying that the air was worth 'sixpence a pint'.
Whale Chine is a geological feature near Chale on the south-west coast of the Isle of Wight, England. 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.
The Wessex Formation is a fossil-rich English geological formation that dates from the Berriasian to Barremian stages of the Early Cretaceous. It forms part of the Wealden Group and underlies the younger Vectis Formation and overlies the Durlston Formation. The dominant lithology of this unit is mudstone with some interbedded sandstones. It is part of the strata of the Wessex Basin, exposed in both the Isle of Purbeck and the Isle of Wight. While the Purbeck sections are largely barren of vertebrate remains, the Isle of Wight sections are well known for producing the richest and most diverse fauna in Early Cretaceous Europe.
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 many of such chines on the island created by stream erosion of soft Cretaceous rocks.
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.
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.
Atherfield Ledge is a rocky outcrop extending from the coast of the Back of the Wight, Isle of Wight. This is a famous shipwreck location. Along with Brook Ledge and Brighstone Ledge it is one of the area's main shipping hazards.
Vectidraco, is a genus of azhdarchoid pterosaur from the Lower Cretaceous of England.
Brighstoneus is a genus of hadrosauriform dinosaur from the Early Cretaceous Wessex Formation of the Isle of Wight, England. The genus contains a single species, Brighstoneus simmondsi, known from a partial skeleton.
