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 a supercontinent that existed during the late Paleozoic and early Mesozoic eras .
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 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.
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.
The northern piece of Pangaea is called Laurasia. It was a supercontinent that existed during the Paleozoic and Mesozoic eras before eventually breaking apart to form the continents we have today.
The supercontinent Pangaea was formed about 335 million years ago and split into two large landmasses, Laurasia and Gondwana, around 180 million years ago. The modern countries we know today did not exist during Pangaea's time, as landmasses were still connected.
The Alps are younger than Pangaea. The formation of the Alps began around 30 million years ago during the Tertiary period, while Pangaea existed around 335 to 175 million years ago during the Paleozoic and Mesozoic eras.
Pangaea (Pangæa) was the latest of several supercontinents that existed during the prehistoric periods on Earth. It formed about 300 million years ago, then began to rift about 200 million years ago, creating the current continents.
Pangaea was a supercontinent that formed approximately 300 million years ago. It existed during the Paleozoic and early Mesozoic eras, breaking apart to form the continents we know today after about 100 million years.