Pangaea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras, about 335 to 175 million years ago. The concept of Pangaea was proposed by Alfred Wegener in 1912, based on the jigsaw puzzle-like fit of the continents, similar rock formations and fossils found on different continents, and the distribution of ancient glacial deposits.
The formation of Pangaea is believed to have occurred due to the process of continental drift. This theory suggests that the Earth's continents were once joined together as a single landmass and have since drifted apart over millions of years due to the movement of tectonic plates.
There are several lines of evidence that support the existence of Pangaea, including:
Pangaea began to break apart during the early Mesozoic era, leading to the formation of the separate continents as we know them today. This breakup was driven by the movement of tectonic plates, leading to the formation of new ocean basins and the shifting of continents to their current positions.
To study the concept of Pangaea, it is important to focus on the following key points:
Studying Pangaea provides valuable insights into the dynamic nature of the Earth's geology and the processes that have shaped the planet over millions of years. Understanding the concept of Pangaea is crucial for comprehending the evolution of continents and the distribution of landmasses on Earth.