Search results
Results from the WOW.Com Content Network
View south across the Weald of Kent as seen from the North Downs Way near Detling. The Weald (/ ˈ w iː l d /) is an area of South East England between the parallel chalk escarpments of the North and the South Downs. It crosses the counties of Hampshire, Surrey, West Sussex, East Sussex, and Kent.
You are free: 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 are free: 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.
The High Weald National Landscape is in south-east England. Covering an area of 1,450 square kilometres (560 sq mi), it takes up parts of Kent, Surrey, East Sussex, and West Sussex. [1] It is the fourth largest Area of Outstanding Natural Beauty (AONB) in England and Wales. It has an attractive landscape with a mosaic of small farms and ...
Media in category "Golf logos" The following 60 files are in this category, out of 60 total. ... File:Richmond Golf Club logo.png; File:RyderCup1997Logo.png; File ...
Other nearby settlements include Ticehurst, Burwash, Mayfield and Heathfield in East Sussex, and Lamberhurst, Hawkhurst and Cranbrook in Kent. Physically, Wadhurst lies on a high ridge of the Weald – a range of wooded hills running across Sussex and Kent between the North Downs and the South Downs. The reservoir of Bewl Water is nearby.
Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!
The geology of East Sussex is defined by the Weald–Artois anticline, a 60 kilometres (37 mi) wide and 100 kilometres (62 mi) long fold within which caused the arching up of the chalk into a broad dome within the middle Miocene, [1] which has subsequently been eroded to reveal a lower Cretaceous to Upper Jurassic stratigraphy.