1912
The concept of Pangaea, the supercontinent, was first proposed by Alfred Wegener in 1912 as part of his theory of continental drift.
The concept of Pangaea, the supercontinent that existed during the late Paleozoic and early Mesozoic eras, was first proposed in the early 20th century. Alfred Wegener, a German scientist, introduced the idea of Pangaea in 1912 as part of his theory of continental drift.
Pangaea began to break up during the Triassic period, around 200 million years ago. This breakup eventually led to the formation of the continents we recognize today.
Alfred Wegener had discovered pangaea in the year of 1912.
The Pangaea began to break down about 200 billion years ago.
The concept of Pangaea, the supercontinent, was first proposed by Alfred Wegener in 1912 as part of his theory of continental drift.
The concept of Pangaea, the supercontinent that existed during the late Paleozoic and early Mesozoic eras, was first proposed in the early 20th century. Alfred Wegener, a German scientist, introduced the idea of Pangaea in 1912 as part of his theory of continental drift.
1980
Pangaea began to break up during the Triassic period, around 200 million years ago. This breakup eventually led to the formation of the continents we recognize today.
age of reptiles
Alfred Wegener had discovered pangaea in the year of 1912.
The Pangaea began to break down about 200 billion years ago.
Alfred Wegner proposed the concept of a supercontinent called Pangaea, which he believed existed around 300 million years ago. Wegner suggested that Pangaea later split apart to form the continents that we see today.
pangaea
The hypothesis of the supercontinent Pangaea was not rejected, but rather supported by geological evidence such as matching rock formations, fossils, and mountain ranges across different continents. The concept of plate tectonics provided a framework to explain the breakup of Pangaea into separate continents over time.
Pangaea's
We do not know the exact answer, but scienctists approximate the late Carboniferous period; about 300 million years ago.