Because they are made from chalk (calcium carbonate) which is a white material.
The truth is that they are really not that white. If you looked closely you would find that some parts are absolutely full of plant growth and flint.
The effect that causes them to be "so white" also has to do with reflection of light.
The calcium carbonate form coccolith structures that can reflect light. The (south-)western orientation of the cliffs in combination with the rising sun generate the reflection and "light up" the cliffs.
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The White Cliffs of Dover are composed of chalk, a soft, white limestone formed from the remains of marine organisms. The white color comes from the high concentration of calcium carbonate in the chalk.
The cliff face, which reaches up to 350 feet high, owes its striking façade to its composition of chalk (pure white calcium carbonate) accentuated by streaks of black flint.
They are mad of chalk, or the shells of microorganisms that lived in shallow seas millions of years ago.
White cliffs can be found in various locations around the world, but some of the most well-known examples include the White Cliffs of Dover in England, the White Cliffs of Rügen in Germany, and the White Cliffs of Møn in Denmark.
The White Cliffs of Dover reach heights of up to 350 feet (110 meters) above sea level. They are an iconic landmark on the English coastline, known for their distinctive chalky white appearance.
Yes, the White Cliffs of Dover can be seen from France on a clear day, particularly from the cliffs near Calais, which is approximately 21 miles away across the English Channel.
Yes, the White Cliffs of Dover are predominantly made up of sedimentary rocks. These cliffs consist mainly of chalk, which is a soft, white, fine-grained limestone rock formed from the remains of marine organisms.
Chalk