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.
they are different because one is farther and one is closer
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
they are different because one is farther and one is closer
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.
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.
Pangaea was a supercontinent that existed around 335 million years ago, which eventual broke apart into two fragments: Laurasia in the north (which includes North America, Europe, and Asia) and Gondwana in the south (which includes South America, Africa, Antarctica, Australia, and the Indian subcontinent).
The theory that explains how the continents drifted from one landmass to their present locations is called plate tectonics. It suggests that the Earth's outer shell is divided into several plates that move and interact with each other, leading to the drifting of continents over time. This movement is driven by processes like seafloor spreading and subduction.
Much different than they are today.
The current locations of rivers emptying into the ocean, similar coastal rock formations and fossil types, and similar plants growing on the continents today.
Rodinia
Stegosaurus lived between 155 and 150 million years ago. By that point, the continents had broken apart, and the seas created barriers to land animals. Thus, Stegosaurus never spread to all the continents. Stegosaurus fossils are known from North America, and its relatives, the stegosaurs, have been found in North America, Europe, Asia, and Africa.
Pangea was a super continent and that was a time when all of the continents were joined together. when Pangaea broke apart, they moved to different locations which are different climate zones so glaciers no longer existed in places where the climate changed from cold to hot.
Mostly. Although some positions will shift and Coastlines will change. However, it is not enough to be considered a difference.