History of the Isle of Wight proposal. History of the Isle of Wight The Isle of Wight is rich in historical and archaeological sites, from prehistoric fossil beds with dinosaur remains, to dwellings and artefacts dating back to the Bronze Age, Iron Age, and Roman periods. The River Solent was the largest tributary of the Channel River that drained the Hampshire Basin from the Early Pleistocene or late Pliocene. During the Mesolithic period, sea levels in northern Europe were some 30 to 40 metres lower than today, and the land that became Britain was a peninsula of northern Europe. The island was formed at the end
Geology of the Isle of Wight the north of the monoclines the Paleogene sequence is deformed into a gentle syncline, the Bouldnor Syncline. Geology of the Isle of Wight The geology of the Isle of Wight is dominated by sedimentary rocks of Cretaceous and Paleogene age. This sequence was affected by the late stages of the Alpine Orogeny, forming the Isle of Wight monocline, the cause of the steeply-dipping outcrops of the Chalk Group and overlying Paleogene strata seen at The Needles, Alum Bay and Whitecliff Bay. Rocks of Devonian, Triassic and Jurassic age are known to be present in the subsurface of the island from