Recorrido por los acantilados de Canterbury y Dover

The White Cliffs of Dover are located on the southeast coast of England in the county of Kent. They face the Strait of Dover and the English Channel, and on a clear day, you can even see across to France. These famous cliffs are a symbol of Britain’s coastal beauty and resilience.

Canterbury Cathedral is one of the oldest and most important Christian structures in England. Founded in 597 AD, it became a major pilgrimage site after the martyrdom of Archbishop Thomas Becket in 1170. It remains a UNESCO World Heritage Site and the spiritual center of the Anglican Church.

Deal is a lovely seaside town in Kent known for its historic fishing heritage, Georgian architecture, and long seafront promenade. It was once England’s busiest port and the site of Julius Caesar’s first landing in Britain in 55 BC. We love its relaxed atmosphere, castle, and cafes.

Dover Castle is often called the “Key to England” due to its strategic importance. Built in the 11th century, it has played a crucial role in defending Britain from medieval times through World War II. The castle’s underground tunnels and towering walls make it one of the most impressive fortresses in Europe.

The White Cliffs of Dover have long symbolised hope, defense, and homecoming for Britain, especially during times of war. Their brilliant white colour comes from chalk deposits formed millions of years ago. They are also a beloved natural landmark and a must-see destination for visitors to Kent.

Canterbury is located in the county of Kent, in southeast England, about 60 miles (100 km) from London. It is perfect for a day tour from London.

Kent is famously called the “Garden of England” due to its fertile land, rolling countryside, and abundance of orchards, hop gardens, and vineyards. For centuries, the county has been a key region for growing fruits, flowers, and crops that supply much of the country. Its gentle hills, patchwork fields, and historic estates have made it a symbol of traditional English rural beauty. On our Canterbury & White Cliffs tour, you’ll see why this nickname still holds true as we travel through some of Kent’s most scenic and storied landscapes.

The White Cliffs of Dover were formed over 70 million years ago during the Late Cretaceous period. They are made primarily of chalK; a soft, white limestone composed of the microscopic remains of marine algae that settled on the seabed. Over millions of years, layers of this sediment built up and were eventually compressed into chalk. Tectonic movements and changes in sea levels later exposed these cliffs to erosion, creating the dramatic vertical faces we see today. Their brilliant white colour comes from the purity of the chalk, which contains very little organic material or impurities.