At one time, they were one land mass that pulled apart, leaving matching outlines.
Africa and Europe have coastlines that fit together snugly, leading some researchers to propose the idea of a single supercontinent, known as Afro-Eurasia. This is based on the matching shapes of the coastlines on the eastern boundary of the Atlantic Ocean.
This concept is known as continental drift, which suggests that the Earth's continents were once part of a single landmass called Pangaea and have since drifted apart over millions of years due to the movement of tectonic plates. This theory is supported by geological evidence such as similar rock formations, fossils, and the matching shapes of coastlines on different continents.
During the formation of Pangaea, the continents fit together in a supercontinent that was surrounded by a single large ocean called Panthalassa. The shapes of today's continents suggest that they were once connected, as evidenced by the matching coastlines of South America and Africa.
Evidence of continental drift includes matching coastlines, geological similarities between continents, and the distribution of fossils and ancient species across continents that are now separated. Additionally, the discovery of mid-ocean ridges and the theory of plate tectonics further support this idea.
Nebraska doesn't have coastlines because there is no ocean around it...
The Arctic Ocean
Chains of volcanos along ocean Coastlines
Alabama
Africa and South America. The matching coastlines of these two continents, particularly along the Atlantic Ocean, led to the development of the theory of continental drift proposed by Alfred Wegener in the early 20th century.
There are Great Whites everywhere in the ocean but you see them mainly near California coastlines, African coastlines, and Australian coastlines.
We find matching types of ancient fossils separated on coinciding land masses across the Atlantic Ocean, where Brazil would abut Africa.
they are separated by the ocean.