fossils,shape of the continents
Approximately 300 million years ago, the Earth's continents were joined together in a supercontinent known as Pangaea. Over time, Pangaea split apart to form the continents as we recognize them today.
The theory that all present continents were once joined together in a supercontinent called Pangaea was proposed by Alfred Wegener in 1912. He suggested that over time, Pangaea broke apart into the continents we see today, a process known as continental drift.
Evidence for the theory of continental drift includes the fit of the continents like puzzle pieces, similarities in rock formations and geological structures across continents, matching fossil evidence of similar plants and animals found on different continents, and similarities in ancient climate evidence like glaciation patterns. The most notable evidence now comes from the study of plate tectonics, which explains how and why the continents have moved over time.
Antarctica was joined with South America, Australia, and New Zealand 65 million years ago as part of the supercontinent Gondwana. Over time, the breakup of Gondwana led to the separation of these landmasses to form the modern continents.
Approximately 335 million years ago, all the Earth's continents were joined together in a supercontinent called Pangaea. Over time, due to the movement of tectonic plates, Pangaea began to break apart, leading to the formation of the continents as we know them today.
Geraghty Period
Evidence supporting the idea of Pangaea includes the fitting together of continents like puzzle pieces, matching rock formations and geological structures across continents, similar fossil evidence found on different continents, and the distribution of plant and animal species that suggest they were once connected. Additionally, paleoclimatic evidence such as glacial deposits and ancient climate zones also indicate a time when continents were joined.
Scientists have found that the coastlines of continents fit together like puzzle pieces, providing evidence for the theory of continental drift. Additionally, similarities in rock formations, fossils, and geological features across different continents support the idea that they were once connected. Magnetic stripes in the ocean floor also suggest that continents have moved over time.
At one point in history, the continents were joined together as a supercontinent called Pangaea. Over time, the movement of tectonic plates caused the continents to drift apart to form the world map we know today.
Scientists believe that at one time, the entire land mass of the world was joined together. When looking at a flat map of the earth, the shape of the continents look like they would fit together if they were linked.
Alexander du Toit discovered evidence for continental drift in the early 20th century. He proposed that the continents were once joined together in a single supercontinent called Pangaea, and that over time they drifted apart to form the continents as we know them today. His work laid the foundation for the theory of plate tectonics.
Three pieces of evidence used to prove the theory of continental drift were the fit of the continents' coastlines, the distribution of fossils across continents, and the matching geological formations found on separate continents. These observations supported the idea that the continents were once joined together and had drifted apart over time.
pangea is a super-continent formed a long time ago when all of the seven continents came together. the largest amount of evidence scientists have is that all of the continents fit almost perfectly together, like a puzzle.
Approximately 300 million years ago, the Earth's continents were joined together in a supercontinent known as Pangaea. Over time, Pangaea split apart to form the continents as we recognize them today.
Well I know 4 Rock evidence mountain belt evidence fossil evidence puzzle piece evidence Hope it helped.......
The theory that all present continents were once joined together in a supercontinent called Pangaea was proposed by Alfred Wegener in 1912. He suggested that over time, Pangaea broke apart into the continents we see today, a process known as continental drift.
Scientists believe that at one time, the entire land mass of the world was joined together. When looking at a flat map of the earth, the shape of the continents look like they would fit together if they were linked.