earthquakes
The theory of plate tectonics provides evidence that continents have moved over time. This evidence includes matching geological features between continents that were once part of the same landmass, like the coastlines of Africa and South America. Additionally, the distribution of fossils and the alignment of mountain ranges suggest that continents were once connected and have since drifted apart.
The matching coastlines and geologic similarities between continents, specifically between South America and Africa, led some to suspect that the continents were once connected. This evidence, known as continental drift, was proposed by Alfred Wegener in the early 20th century.
North America, South America,Europe, Asia, Africa,Antarctica,Austrailia.
An example of evidence from land features that supported Wegener's idea of continental drift might include the piecing together of map layouts which show the way that the continents fit together. Wegener is famous for sharing this example.
The five continents on Earth are Africa, Europe, Asia, North America, and South America. Some geographers and organizations may consider different continents or groupings depending on their definitions.
Features such as glacial striations, glacial deposits, and the distribution of fossil remains of ancient plants and animals that are typically associated with polar regions provide evidence that many continents were at one time near Earth's south pole. Additionally, the alignment of mountain ranges and geological formations across different continents suggests past connections when the continents were located closer together.
A) glacial deposits
Antarctica was and is.
The continents of Africa and South America are often used as evidence for the continental puzzle due to their matching coastlines and geological features, suggesting they were once connected. This supports the theory of continental drift and plate tectonics.
One main evidence is the fit of the continents' coastlines, particularly the fit of South America and Africa. Fossil evidence of similar species found on different continents also supports the idea of continental drift. Additionally, the matching geological features and rock formations across continents provide further evidence for the theory of continental drift.
The theory of plate tectonics provides evidence that continents have moved over time. This evidence includes matching geological features between continents that were once part of the same landmass, like the coastlines of Africa and South America. Additionally, the distribution of fossils and the alignment of mountain ranges suggest that continents were once connected and have since drifted apart.
The matching coastlines and geologic similarities between continents, specifically between South America and Africa, led some to suspect that the continents were once connected. This evidence, known as continental drift, was proposed by Alfred Wegener in the early 20th century.
North America, South America,Europe, Asia, Africa,Antarctica,Austrailia.
The evidence for moving continents, known as continental drift, includes the fit of the coastlines of continents like South America and Africa, the similarity of rock formations and fossils on different continents, and the presence of ancient glaciation patterns on continents that are now located in warmer climates. These pieces of evidence formed the basis for the theory of plate tectonics.
An example of evidence from land features that supported Wegener's idea of continental drift might include the piecing together of map layouts which show the way that the continents fit together. Wegener is famous for sharing this example.
Evidence supporting the hypothesis of continental drift includes the fit of continents like South America and Africa, matching geological features and rock formations across continents, and similar fossil records found on separate continents. Additionally, the presence of ancient glacial deposits and the alignment of mountain ranges between continents provide further support for the movement of continents over time.
The five continents on Earth are Africa, Europe, Asia, North America, and South America. Some geographers and organizations may consider different continents or groupings depending on their definitions.