Jump to content
Main menu
Main menu
move to sidebar
hide
Navigation
Main page
Recent changes
Random page
Help about MediaWiki
Special pages
Niidae Wiki
Search
Search
Appearance
Create account
Log in
Personal tools
Create account
Log in
Pages for logged out editors
learn more
Contributions
Talk
Editing
Isle of Wight
(section)
Page
Discussion
English
Read
Edit
View history
Tools
Tools
move to sidebar
hide
Actions
Read
Edit
View history
General
What links here
Related changes
Page information
Appearance
move to sidebar
hide
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
===Geology=== {{main|Geology of the Isle of Wight}} The Isle of Wight is made up of a variety of rock types dating from early [[Cretaceous]] (around 127 million years ago) to the middle of the [[Palaeogene]] (around 30 million years ago). The geological structure is dominated by a large [[monocline]] which causes a marked change in age of strata from the northern younger [[Tertiary]] beds to the older Cretaceous beds of the south. This gives rise to a [[Strike and dip|dip]] of almost 90 degrees in the chalk beds, seen best at [[the Needles]]. The northern half of the island is mainly composed of [[clay]]s, with the southern half formed of the [[chalk]] of the central eastโwest downs, as well as Upper and Lower [[Greensand]]s and [[Wealden Group|Wealden]] strata.<ref name="Hopson">{{cite journal | url=http://nora.nerc.ac.uk/15996/1/Hopson_IoW_Geo_History_PGEOLA-D-11-00048R1.pdf | title=The geological history of the Isle of Wight: an overview of the 'diamond in Britain's geological crown' | author=Hopson P. | journal=Proceedings of the Geologists' Association | year=2011 | volume=122 | issue=5 | pages=745โ763 | doi=10.1016/j.pgeola.2011.09.007| bibcode=2011PrGA..122..745H }}</ref> These strata continue west from the island across the [[Solent]] into [[Dorset]], forming the basin of [[Poole Harbour]] (Tertiary) and the [[Isle of Purbeck]] (Cretaceous) respectively. The chalky ridges of Wight and Purbeck were a single formation before they were breached by waters from the [[River Frome, Dorset|River Frome]] during the [[last glacial period|last ice age]], forming the Solent and turning Wight into an island. [[The Needles]], along with [[Old Harry Rocks]] on Purbeck, represent the edges of this breach. All the rocks found on the island are [[sedimentary]], such as [[limestone]]s, [[mudstone]]s and [[sandstone]]s. They are rich in fossils; many can be seen exposed on beaches as the cliffs erode. [[Lignite|Lignitic coal]] is present in small quantities within seams, and can be seen on the cliffs and shore at [[Whitecliff Bay]]. Fossilised [[mollusc]]s have been found there, and also on the northern coast along with [[fossil]]ised [[crocodile]]s, [[turtle]]s and [[mammal]] bones; the youngest date back to around 30 million years ago. The island is one of the most important areas in Europe for [[dinosaur]] [[fossil]]s. The [[Erosion|eroding]] cliffs often reveal previously hidden remains, particularly along the [[Back of the Wight]].<ref>{{cite web|url=http://www.redfunnel.co.uk/island-guide/isle-of-wight-activities/fossil-and-dinosaur-hunting/ |title=Fossil and Dinosaur Hunting|publisher=redfunnel.co.uk |access-date=28 November 2016}}</ref> [[Dinosaur]] bones and [[ichnite|fossilised footprints]] can be seen in and on the rocks exposed around the island's beaches, especially at [[Yaverland]] and [[Compton Bay]], from the strata of the [[Wessex Formation]]. As a result, the island has been nicknamed "Dinosaur Island" and [[Dinosaur Isle]] was established in 2001. The area was affected by sea level changes during the repeated [[Quaternary]] glaciations. The island probably became separated from the mainland about 125,000 years ago, during the [[Eemian|Ipswichian]] [[interglacial]].<ref name="Booth&Brayson">{{cite journal | url=https://core.ac.uk/download/files/79/386230.pdf | title=Geology, landscape and human interactions: examples from the Isle of Wight | author=Booth K.A. & Brayson J. | journal=Proceedings of the Geologists' Association | year=2011 | volume=122 | issue=5 | pages=938โ948 | doi=10.1016/j.pgeola.2011.01.004 | bibcode=2011PrGA..122..938B | access-date=10 March 2016 | archive-date=12 March 2016 | archive-url=https://web.archive.org/web/20160312112130/https://core.ac.uk/download/files/79/386230.pdf | url-status=dead }}</ref> <gallery> File:Isle of Wight OS OpenData map.png|[[Ordnance Survey]] map of the island File:IOW geology.svg|Geological map of the island File:Blackgang Chine c1910 - Project Gutenberg eText 17296.jpg|[[Blackgang Chine]], circa 1910 File:Isle of Wight coastline.jpg|A view of [[the Needles]] and [[Alum Bay]] </gallery>
Summary:
Please note that all contributions to Niidae Wiki may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see
Encyclopedia:Copyrights
for details).
Do not submit copyrighted work without permission!
Cancel
Editing help
(opens in new window)
Search
Search
Editing
Isle of Wight
(section)
Add topic