English: High Rocks on the outskirts of Tunbridge Wells is an outcrop of Ardingley Sandstone laid down in the Lower Cretaceous period then wind eroded in the last ice age. The site forms a SSSI. They form a visitor attraction and are served by a hotel and station on the Spa Valley steam railway. The first written reference is in 1645, known to James II and George, Prince of Wales.
I, the copyright holder of this work, hereby publish it under the following licenses:
Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License.http://www.gnu.org/copyleft/fdl.htmlGFDLGNU Free Documentation Licensetruetrue
to share – to copy, distribute and transmit the work
to remix – to adapt the work
Under the following conditions:
attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
https://creativecommons.org/licenses/by/3.0CC BY 3.0 Creative Commons Attribution 3.0 truetrue
You may select the license of your choice.
Captions
Add a one-line explanation of what this file represents