White Cliffs of Dover, Chalk cliffs in Dover, England.
The White Cliffs of Dover are chalk formations along the English Channel that extend roughly 13 kilometers and rise in places up to 110 meters above the water. Their white surface shows distinct layers of chalk interspersed with dark flint bands that catch the sunlight and stand out clearly against the sea.
For centuries, these formations served as a navigation point for sailors crossing the channel and heading toward British ports. Their prominent position also helped warn ships of danger and played a role in various defense strategies over time.
For generations, these chalk formations have served as a recognizable emblem of the nation, appearing in songs, paintings, and written works. Many travelers visit because the cliffs hold a deep connection to the country's identity and continue to inspire artistic expression today.
Several walking trails run along the top of the formations, allowing visitors to stroll with views over the water and, on clear days, toward the French coastline. Viewing platforms are set up at different points to make it easier to reach the best outlooks.
The cliff faces hold millions of fossils from the Cretaceous period, showing remains of tiny sea organisms and forming a natural archive of prehistoric life. Careful observers can spot small imprints and shell fragments directly in the chalk surface.
Location: Dover
Website: https://nationaltrust.org.uk/the-white-cliffs-of-dover
GPS coordinates: 51.13472,1.35711
Latest update: December 3, 2025 20:28
Cliffs rank among Earth's most striking geological formations, ranging from coastal precipices to inland mountain faces. Along oceans, they shape coastlines for thousands of miles, while in mountain regions they form vertical walls that draw climbers from around the world. This collection documents significant cliffs across six continents, including Ireland's 214-meter (702-foot) Cliffs of Moher, England's white chalk cliffs at Dover, and Norway's Preikestolen, which rises 604 meters (1,982 feet) above Lysefjord. Among the locations are some of Earth's highest vertical walls. Hawaii's Kalaupapa Cliffs on Molokai reach 1,010 meters (3,315 feet), while Pakistan's Trango Towers rise above 6,000 meters (19,685 feet) with nearly vertical rock faces. Coastal formations like Normandy's Étretat cliffs, Ireland's Slieve League, and Australia's Bunda Cliffs along the Nullarbor Plain demonstrate the power of marine erosion. Inland, formations such as California's El Capitan, China's Zhangjiajie National Forest Park towers, and South Africa's Table Mountain create distinctive landscape features shaped by different geological processes over millions of years.
Fan Bay Deep Shelter
319 m
Swingate transmitting station
1.5 km
South Foreland
1.2 km
Dover to Kingsdown Cliffs
1.6 km
St Margaret's Bay Windmill
1.6 km
South Foreland Upper Lighthouse
1.2 km
South Foreland Lower Lighthouse
1.5 km
Church of St Peter
2.2 km
Swingate Inn
2 km
Langdon Beach
466 m
Royal Flying Corps Memorial, Dover
1 km
Wallets Court
2.1 km
Wanstone Farmhouse
1 km
The Headmasters House
2.2 km
Bere Farmhouse
1.6 km
The Infirmary
2.2 km
Eastern Arm, Dover Harbour
1.4 km
Milestone, Guston, E of tree screen to Duke of York's Royal Military School, quarter mile S of A2 jct
2.1 km
High Gaut
1.7 km
A pair of acoustic mirrors at Fan Bay
304 m
Buried Reserve And Pillbox, Former Swingate Chain Home Radar Station
1.5 km
Receiver Site And Royal Observer Corps Underground Nuclear Monitoring Post, Former Swingate Chain Home Radar Station
1.2 km
Transmitter Site (Excluding Tower 2), Former Swingate Chain Home Radar Station
1.5 km
Fan Bay Sound Mirrors
300 m
National Trust White Cliffs of Dover
1.4 km
East Entrance Lodges Gates And Flanking Walls
2.2 km
Scenic viewpoint
850 m
Scenic viewpoint, bench
398 mReviews
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