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Stevns Klint, known as the Cliffs of Stevns in English, is a white chalk cliff located some 6 km (3.7 mi) southeast of Store Heddinge on the Danish island of Zealand. Stretching 17 km (11 mi) along the coast, it is of geological importance as one of the best exposed Cretaceous-Tertiary (K/T) boundaries in the world. [ 1 ]
Atop the cliff, there is an almost flat top of approximately 25 by 25 metres (82 ft × 82 ft). Preikestolen is located near the western part of the fjord, and on its north side. Tourism at the site has been increasing in the early 21st century, with 300,000 visitors in 2024, [ 2 ] making it one of the most-visited natural tourist attractions in ...
View of the Streckelsberg in 1954. The Streckelsberg is an approximately 58-metre high coastal cliff on the island of Usedom in North Germany. [1] After the Golm and the Kückelsberg, the Streckelsberg is the third highest elevation on the island.
We’re ready for a whole new set of explorations in 2025 with picks for 25 top places to visit. Take cues from the worst-behaved travelers of 2024 for what not to do in the year ahead.
Preikestolen is a massive cliff 604 metres (1982 ft) above Lysefjorden, opposite the Kjerag plateau, in Forsand. Western Norway is the third largest region in Norway by area. It covers an area of 58,582 km 2 (22,619 sq mi).
Type area - coastal outcrops from Black Head, Weymouth to Chapman's Pool The Kimmeridge Clay is a sedimentary deposit of fossiliferous marine clay which is of Late Jurassic to lowermost Cretaceous age and occurs in southern and eastern England and in the North Sea . [ 1 ]
The massive waves hammered beaches, piers and shore cliffs and led to multiple water rescues. Heavy surf causes coastal chaos across SLO County. See the photos and video
Carsaig Arches are natural arch cliff formations on the Ross of Mull in the south of the Isle of Mull, on the west coast of Scotland. They are situated below Malcolm's Point, [1] at the base of the Rudha Fhaoilean cliffs. [2] To the east are Carsaig Bay, [3] and Eas na Dabhaich.