
The cone-shaped island was original part of the fort interior, before 2000 years of erosion separated it from the mainland. The surviving portion of the site tops the cliffs to the left of the island.
Image credit: A. Brookes (23.4.2015)
The cone-shaped island was original part of the fort interior, before 2000 years of erosion separated it from the mainland. The surviving portion of the site tops the cliffs to the left of the island.
The outer bank. The inner banks can be seen beyond, way over to the left.
The outer bank.
Looking towards the inner banks. The outer rampart is behind me, separated from the inner by a wide strip of clifftop.
The twin inner banks.
The eroded ends of the inner banks, a section sliced cleanly through.
The fort occupies the flat clifftop above the beach. Part of the interior has fallen into the sea.
Castell Bach Cwmtydu, situated atop a level coastal cliff promontory along the Irish Sea.