smiliar fossils and plants, matching of the continents as a jig-saw puzzle, remaining of tropical plants
Fossil evidence such as the presence of identical plant and animal species on continents separated by oceans. This suggests that these continents were once connected and later drifted apart.
matching geological features, such as similar rock formations and mountain ranges, on different continents. This suggests that the continents were once connected and have since drifted apart.
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 presence of the same fossils or geological formations on different continents can provide evidence to support the theory of continental drift. This suggests that the continents were once connected and have since drifted apart over geological time scales.
True. The theory of continental drift, proposed by Alfred Wegener in the early 20th century, suggests that the continents were once joined together in a single landmass called Pangaea and have since drifted apart. This theory has been supported by evidence from geology, paleontology, and plate tectonics.
smiliar fossils and plants, matching of the continents as a jig-saw puzzle, remaining of tropical plants
Fossil evidence such as the presence of identical plant and animal species on continents separated by oceans. This suggests that these continents were once connected and later drifted apart.
matching geological features, such as similar rock formations and mountain ranges, on different continents. This suggests that the continents were once connected and have since drifted apart.
because if the same fossils were found in the same spot but on two different continents and if you put the continents together like a puzzle and the fossils were in the same spot, it would mean the continents drifted apart.
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.
they drifted together to form a single continent
The theory is called continental drift, proposed by Alfred Wegener. It suggests that continents were once part of a supercontinent called Pangaea and have since drifted to their current positions. This theory is supported by evidence such as matching coastlines and similar geological features on different continents.
The presence of the same fossils or geological formations on different continents can provide evidence to support the theory of continental drift. This suggests that the continents were once connected and have since drifted apart over geological time scales.
True. The theory of continental drift, proposed by Alfred Wegener in the early 20th century, suggests that the continents were once joined together in a single landmass called Pangaea and have since drifted apart. This theory has been supported by evidence from geology, paleontology, and plate tectonics.
Fossil distribution supports the theory of continental drift by showing similar species of plants and animals that lived on different continents that are now separated by oceans. This suggests that these continents were once joined together and over time drifted apart to their current positions. The presence of identical fossils on continents that are now separated is evidence that they were once part of the same landmass.
One piece of evidence that led Wegener to propose the theory of continental drift was the observation that the coastlines of Africa and South America appeared to fit together like puzzle pieces. This suggested that the continents were once joined together and had subsequently drifted apart.
The edges of Earth's continents fit together like a jigsaw puzzle due to the theory of plate tectonics. This theory suggests that the Earth's crust is divided into large plates that move and interact with each other over time. Over millions of years, the continents have shifted and drifted apart, causing their edges to fit together.