Like all limestones, the famous White Cliffs of Dover, on England's south coast, are made from numberless trillions of tiny marine organisms compressed over time into stone, and exist now as huge reservoirs of carbon. {credit 17.13}
The iconic White Cliffs of Dover, located on England's southern shore, are composed of limestone formed from countless tiny marine organisms that were compressed over millions of years. This geological process has turned these organisms into a solid stone structure, showcasing the remarkable natural history of the area.
These cliffs are not only a significant landmark but also represent vast reservoirs of carbon, highlighting their importance in understanding both the Earth's history and the role of natural formations in our ecosystem. The fascinating composition of the cliffs illustrates the intricate relationship between life and geology throughout time.
