Pangea, also spelled pangaea or pangæa. The wikipedia article is probably a good place to start, if you want to find out more about it.
The hypothesis that states the continents once formed a single landmass, broke up, and drifted to their present locations is known as the theory of plate tectonics. This theory explains the movement of Earth's lithosphere plates and the distribution of continents and oceans on the planet's surface. It is supported by evidence from fossil records, rock formations, and the matching coastlines of continents like South America and Africa.
The continents began to separate around 200 million years ago during the breakup of the supercontinent Pangaea. This process led to the formation of the current continents and their modern configurations.
Alfred Wegener presented several lines of evidence to support his theory of continental drift, including the fit of the continents like a jigsaw puzzle, similarities in rock formations and mountain ranges across continents, and the distribution of fossils of the same species on different continents separated by oceans.
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.
There is no city present in all continents. Each continent has its own distinct cities.
Gondwanaland is a landmass thought to have been compromised of present-day southern continents.
One piece of evidence that indicates the continents were once connected is the shape of the continents. Many of the continents look as if they fit together like a puzzle.
Present day and animals and rocks on different continents compare the been separated for a long time by scientist examines rocks to find out about earth's history and structure
pangea
They are spread apart now because before the were one big landmass.
Pangea was the giant supercontinental landmass that existed on the Earth's surface about 250 million years ago. It was essentially all of the present continents 'stuck together' in one large grouping. It is proposed by plate tectonics that the movement of tectonic plates moved portions of this landmass apart and around the world, forming the present continents in their existing distribution.
The hypothesis that states the continents once formed a single landmass, broke up, and drifted to their present locations is known as the theory of plate tectonics. This theory explains the movement of Earth's lithosphere plates and the distribution of continents and oceans on the planet's surface. It is supported by evidence from fossil records, rock formations, and the matching coastlines of continents like South America and Africa.
The continents began to separate around 200 million years ago during the breakup of the supercontinent Pangaea. This process led to the formation of the current continents and their modern configurations.
Evidence supporting the theory of the supercontinent Pangaea includes the jigsaw-like fit of continents, similarities in rock formations and mountain ranges across continents that align when continents are brought together, distribution of fossils of identical species across distant continents, and similarities in ancient climates and geological records found on separate continents. These pieces of evidence work together to suggest that the current continents were once part of a single landmass.
Pangaea was a supercontinent that existed around 335 million years ago, while Earth now is divided into several separate continents. The major difference is in the landmass arrangement, as Pangaea was a single large landmass, whereas the current continents are separated by oceans. Additionally, the climate, ecosystems, and species distribution were different during the time of Pangaea compared to the present day.
Australia separated from the supercontinent Gondwana, which included present-day continents like Africa, South America, Antarctica, and India. This separation began around 85 million years ago during the Late Cretaceous period. Over millions of years, Australia drifted northward to its current position, becoming a distinct landmass. This geological process shaped Australia's unique ecosystems and biodiversity.
The Indian subcontinent was once a separate landmass known as the Indian Plate. It is estimated to have separated from the supercontinent Gondwana around 100 million years ago, and eventually collided with the Eurasian Plate, leading to the formation of the Himalayan mountain range.