During the time of Pangaea, the land that is now the Philippines was part of a larger landmass clustered in the Southern Hemisphere, located near the western edge of the supercontinent. It would have been closer to present-day Australia and connected to other regions that eventually shifted to form the islands of Southeast Asia.
During the time that Pangaea existed, the land that now makes up the Philippines was located near the equator within the larger landmass of Gondwana. As Pangaea began to break apart around 175 million years ago, the land that is now the Philippines started to drift northward.
Pangaea was located on Earth during the late Paleozoic and early Mesozoic eras, around 300 million years ago. It was a supercontinent that existed before the tectonic plates shifted to form the current continents.
Pangaea existed around 335 to 175 million years ago during the late Paleozoic and early Mesozoic eras.
When all continents were connected, they were part of the supercontinent called Pangaea. Pangaea existed during the late Paleozoic and early Mesozoic eras, before breaking apart into the continents we know today.
The landmass before the current seven continents was known as Pangaea. Pangaea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras.
During the time that Pangaea existed, the land that now makes up the Philippines was located near the equator within the larger landmass of Gondwana. As Pangaea began to break apart around 175 million years ago, the land that is now the Philippines started to drift northward.
Pangaea was located on Earth during the late Paleozoic and early Mesozoic eras, around 300 million years ago. It was a supercontinent that existed before the tectonic plates shifted to form the current continents.
The Panthalassa Ocean surrounded Pangaea. It was the superocean that existed during the time of the supercontinent Pangaea, covering much of the Earth's surface.
During Pangaea, the continent that was located on the South Pole was likely Antarctica. Pangaea was a supercontinent that existed millions of years ago, and through the process of continental drift, the landmasses eventually split and moved to their current positions.
Pangaea existed during the Mesozoic era, specifically during the late Paleozoic and early Mesozoic periods, approximately 335 to 175 million years ago.
Alfred Wegener proposed the concept of Pangaea in 1912, suggesting that this supercontinent existed around 300 million years ago during the late Paleozoic and early Mesozoic eras. Therefore, based on that timeline, Pangaea would have existed approximately 300 million years ago from today.
Pangaea existed during Wegener's time because he proposed the theory of continental drift, suggesting that all the continents were once part of a single landmass that later broke apart. Wegener used evidence such as the fit of the continents, matching rock formations, and similar fossils found on separate continents to support his theory of Pangaea.
The only continent in the Triassic period was the supercontinent known as Pangaea.
Pangaea existed around 335 to 175 million years ago during the late Paleozoic and early Mesozoic eras.
The supercontinent was named Pangaea by Alfred Wegener. It was theorized that Pangaea existed during the late Paleozoic and early Mesozoic eras.
When all continents were connected, they were part of the supercontinent called Pangaea. Pangaea existed during the late Paleozoic and early Mesozoic eras, before breaking apart into the continents we know today.
The landmass before the current seven continents was known as Pangaea. Pangaea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras.