Category
page 1Geology of England
Chiltern Hills
hills in South East England

Avalonia
thumb|upright=1.35|Current extent of Avalonia highlighted in yellow
Avalonia was a microcontinent in the Paleozoic era. Crustal fragments of this former microcontinent are terranes in parts of the eastern coast of North America: Atlantic Canada, and parts of the East Coast of the United States. In addition, terranes derived from Avalonia also make up portions of Northwestern Europe, being found in England, Wales and parts of Ireland.
South Downs
range of hills in the United Kingdom
North Downs
ridge of chalk hills in south east England
Salisbury Plain
chalk plateau in England
chine
thumb|Chine forming on soft cliffs at Compton, Isle of Wight
thumb|Shanklin Chine, circa 1910.
A chine () is a steep-sided coastal gorge where a river flows to the sea through, typically, soft eroding cliffs of sandstone or clays. The word is used in central Southern England—notably in East Devon, Dorset, Hampshire and the Isle of Wight—to describe such topographical features. The term 'bunny' is sometimes used to describe a chine in Hampshire. The term chine is also used in some Vancouver suburbs in Canada to describe similar features.
Cranborne Chase
Plateau in southern England
Tees-Exe line
Weald–Artois Anticline
geologic structure in southern England and northern France