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

A part of Lyme Bay, with The Spittles and Black Ven on the left.

The Spittles is an area of coastal cliff in the county of Dorset on the south coast of England. It is situated between the settlements of Lyme Regis to the west and Charmouth to the east. It forms part of the Jurassic Coast, a World Heritage Site designated in 2001. The cliff contains layers of Blue Lias and clay; in wet seasons the clay causes the layers above to become saturated and hence landslips occur, exposing many fossils. Mary Anning famously found an Ichthyosaurus in the Spittles.[1]

The Spittles also lies just to the west of another popular fossiling location along the Jurassic Coastline at Black Ven. The base of the Black Ven mudslide is one of the best places to find fossils along the Jurassic Coastline. The sea washes the fossils out of the mud and leaves them to be found amongst the shingle between the boulders.[2]

It is possible to walk here from Lyme Regis, but care must be taken not to get cut off by the tide. The area is also prone to rock falls and mudslides, particularly during winter storms.

See also

References

  1. ^ Lyme Bay Fossils: Jurassic Beach Guide. NClarke, Nigel J. (2004) ISBN 978-0-907683-01-8
  2. ^ The Spittles - Quick Facts Area

50°43′55″N 2°55′12″W / 50.732°N 2.920°W / 50.732; -2.920

This page was last edited on 2 November 2022, at 00:06
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.