they are different because one is farther and one is closer
65 million years ago, the continents were in different positions due to plate tectonic movement. For example, North America was closer to Europe and Africa, South America was located near Antarctica, and India had not yet collided with Asia. These movements have continued over time, leading to the current positions of the continents.
Approximately 65 million years ago, the continents were grouped together in a supercontinent known as Pangea. Over time, Pangea began to break apart through the process of plate tectonics, eventually forming the continents as we know them today.
Pangaea was a supercontinent that existed about 335 million years ago. It is believed to have later broken apart into the continents we know today due to the movement of tectonic plates. This theory of continental drift helps explain the similarities in geology and fossil evidence found across different continents.
The supercontinent that split into today's continents is called Pangaea. It is believed to have been a single landmass around 335 million years ago before breaking apart into the continents we have today.
The supercontinent Pangaea connected all the continents about 300 million years ago. Over time, Pangaea split apart, leading to the formation of the continents as we know them today.
they are different because one is farther and one is closer
65 million years ago, the continents were in different positions due to plate tectonic movement. For example, North America was closer to Europe and Africa, South America was located near Antarctica, and India had not yet collided with Asia. These movements have continued over time, leading to the current positions of the continents.
Approximately 65 million years ago, the continents were grouped together in a supercontinent known as Pangea. Over time, Pangea began to break apart through the process of plate tectonics, eventually forming the continents as we know them today.
Pangaea was a supercontinent that existed about 335 million years ago. It is believed to have later broken apart into the continents we know today due to the movement of tectonic plates. This theory of continental drift helps explain the similarities in geology and fossil evidence found across different continents.
Pangaea was a supercontinent that existed about 335 million years ago and began to break apart around 175 million years ago, eventually forming the continents we recognize today. Evidence for Pangaea's existence includes the fit of the coastlines of continents, similar rock formations and mountain ranges across continents, and the distribution of fossils of the same species on different continents.
The supercontinent that split into today's continents is called Pangaea. It is believed to have been a single landmass around 335 million years ago before breaking apart into the continents we have today.
It is commonly accepted that the continents have not always been in their current locations. They are thought to have all been part of a super continent known as Pangaea.
The supercontinent Pangaea connected all the continents about 300 million years ago. Over time, Pangaea split apart, leading to the formation of the continents as we know them today.
220 million years ago, the Earth's landmasses were connected in a supercontinent called Pangaea. Over time, this supercontinent broke apart, leading to the formation of the continents we have today. The shifting and drifting of tectonic plates caused the continents to move to their current positions.
Pangaea is the large landmass hypothesized to have broken apart about 200 million years ago, eventually forming the continents we see today.
The continents started breaking apart around 200 million years ago during the breakup of the supercontinent Pangaea. This process continued over millions of years, leading to the formation of the continents as we know them today.
Much different than they are today.