The plate boundary between the African and South American tectonic plates is located along the Mid-Atlantic Ridge, which runs down the center of the Atlantic Ocean. This ridge is situated roughly equidistant from the Coastlines of both continents, separating them as they drift apart due to seafloor spreading. The closest points of the boundary to the coastlines are near the eastern coast of South America and the western coast of Africa.
North America, South America, Europe and Africa
the relative location of south America is that it is south of North America and west of Africa
the relative location of south America is that it is south of North America and west of Africa
South Africa and South America.
Africa and South America have coastlines that appear to fit together, particularly along the bulge of Brazil and West Africa. This observation supports the theory of continental drift and the idea that these two continents were once connected as part of the supercontinent Pangea.
the relative location of south America is that it is south of North America and west of Africa
The continents with the most apparent fit of their coastlines are Africa and South America, forming what is known as the "Atlantic coast fit." This fit is often cited as evidence for the theory of continental drift and the former existence of the supercontinent Pangaea.
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.
Europe's relative location is to the north of Africa, to the west of Asia, and to the east of North America.
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.
Brachiosaurus lived in North America. Its relative Giraffatitan lived in Africa.
Matching coastlines are coastlines from different continents that seem to fit together like puzzle pieces. This observation led to the development of the theory of continental drift and plate tectonics, as it suggests that these continents were once joined together as a single landmass. A famous example of matching coastlines is the fit between the eastern coast of South America and the western coast of Africa.