Taddiford Gap and Hordle Cliff are a classic late Eocene vertebrate and plant locality. The Totland Bay Member contains distinct Mammal, Crocodile, Leaf, Chara and Rodent horizons, whose fossil records depend on careful bed identification. The eroded gap is not a dependable beach descent, and scientific sampling requires appropriate permission. Eocene, Cliffs and Foreshore, Rating: ♦♦♦♦