To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

From Wikipedia, the free encyclopedia

Corton Cliffs is a 5.5-hectare (14-acre) geological Site of Special Scientific Interest north of Lowestoft in Suffolk.[1][2] It is a Geological Conservation Review site.[3]

This is described by Natural England as a "nationally important" site, as it is the type locality for the Anglian glaciation around 450,000 years ago. The Anglian was the most extreme ice age of the Pleistocene epoch. The site displays the complete Anglian sequence and its relation to the preceding Cromerian stage.[4]

The site is a public beach.

YouTube Encyclopedic

  • 1/2
    Views:
    926
    1 413
  • Corton, Suffolk, a photographic slide show.
  • Wessex Fire lowestoft milesy and jack production

Transcription

References

  1. ^ a b c d "Designated Sites View: Corton Cliffs". Sites of Special Scientific Interest. Natural England. Retrieved 8 May 2017.
  2. ^ "Map of Corton Cliffs". Sites of Special Scientific Interest. Natural England. Retrieved 8 May 2017.
  3. ^ "Corton (Quaternary of East Anglia)". Geological Conservation Review. Joint Nature Conservation Committee. Retrieved 3 May 2017.
  4. ^ "Corton Cliffs citation" (PDF). Sites of Special Scientific Interest. Natural England. Archived from the original (PDF) on 4 May 2015. Retrieved 8 May 2017.

52°30′32″N 1°45′00″E / 52.509°N 1.75°E / 52.509; 1.75

This page was last edited on 24 December 2023, at 14:40
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.