Geoscience Reference
In-Depth Information
(the Quantock Fringes landscape). Geological mapping of the unconformity reveals the
ancient landscape of the Variscan mountains, carved into the Devonian and older bed-
rock between 300 and 200 million years ago, and subsequently buried by Triassic and
Jurassic sediments.
FIG
155.
Natural and man-made features of Area 8.
