The Mesozoic Supercontinent is known as Gondwana or Gondwanaland.
The continents merged into a single supercontinent known as Pangaea during the Paleozoic and Mesozoic eras, specifically in the late Paleozoic era around 300 million years ago. This supercontinent began to break apart during the Mesozoic era, leading to the formation of the current continents.
Pangaea it was the supercontinent that supposedly consisted of all of the present continents combined...in theory they should all fit together like a puzzle
The supercontinent is called Pangaea. It existed during the late Paleozoic and early Mesozoic eras before breaking apart into Laurasia and Gondwana, which eventually formed the continents we have today.
Pangaea existed approximately 335-175 million years ago during the late Paleozoic and early Mesozoic eras. It was a supercontinent that existed before the current continents drifted apart to their present positions.
Laurasia and Gondwana land are the super continents formed millions of years ago in the midst of the Tethys sea.These super continents subsequently broke into present continents due to drift.Laurasia comprised the present parts of Europe and Asia while the Antarctica once used to be the part of Gondwana.
Pangaea. "All the World." It's gone. It was the supercontinent that existed at the beginning of the Age of the Dinosaurs. Its counterpart was Panthalassa, "All the Sea." It broke up by 64 million B.C. and the present continents (Africa, Asia, the Americas, etc.) are parts of it.
The theory that all present continents were once joined together in a supercontinent called Pangaea was proposed by Alfred Wegener in 1912. He suggested that over time, Pangaea broke apart into the continents we see today, a process known as continental drift.
the movement of convection currents in the mantle is the cause of plate motion.
the movement of convection currents in the mantle is the cause of plate motion.
the movement of convection currents in the mantle is the cause of plate motion.
the movement of convection currents in the mantle is the cause of plate motion.
the Hypothesis is Based on an apparent fit between Africa and South America,Wegener hypothesized that at one time all continents were joined together in a "supercontinent" called Pangaea. The supercontinent eventually broke into the smaller continents, which then "drifted" towards their present positions.