Dean Hill Anticline
From Wikipedia, the free encyclopedia
The Dean Hill Anticline is an east–west trending fold in the Cretaceous chalk of Hampshire, England. It lies immediately to the north of the Hampshire Basin and south of Salisbury Plain.
From Wikipedia, the free encyclopedia
The Dean Hill Anticline is an east–west trending fold in the Cretaceous chalk of Hampshire, England. It lies immediately to the north of the Hampshire Basin and south of Salisbury Plain.