Pangaea Supercontinent

Wegener proposed the theory of continental drift, suggesting that Pangaea, a supercontinent, gradually broke apart over millions of years due to the movement of tectonic plates. He believed that the continents drifted to their current positions.

Alfred's super-continent is call Pangaea meaning 'all lands' in Greek!

There have been several cycles of supercontinent formation and breakup in Earth's history. Some of the well-known supercontinents include Rodinia, Pannotia, Gondwana, and Pangaea. These supercontinents formed and broke up over hundreds of millions of years due to the process of plate tectonics.

Pangaea was formed through the consolidation of all Earth's continents into a single supercontinent about 335 million years ago, during the late Paleozoic and early Mesozoic eras. The movement of tectonic plates caused the gradual merging of landmasses that eventually led to the formation of Pangaea.

Pangaea began to break apart around 200 million years ago during the Early Jurassic period. This process of continental drift continued over millions of years to form the continents as we know them today.

Pangaea, the supercontinent, formed approximately 335 million years ago during the late Carboniferous period and began to break apart around 175 million years ago during the Jurassic period.

the plate tectonics. the plates were (and still are) moving which caused the supercontinent to split apart and come into the places where they are today. someday, since the plates are still moving, all the continents will come together again and form another supercontinent.

'Panthalassa' was the great sea that surrounded Pangea.

Yes, the theory of Pangaea is supported by geological evidence which shows that the Earth's landmasses were once connected in a supercontinent about 335 million years ago. The idea is widely accepted in the scientific community as a plausible explanation for the arrangement of continents on Earth.

Pangaea split into two supercontinents, Laurasia and Gondwana, during the Mesozoic Era due to the movement of tectonic plates. The splitting process, called continental drift, was driven by the forces caused by mantle convection beneath the Earth's crust. Over millions of years, these forces gradually separated the landmasses that formed Pangaea.

The earth is broken up into plates. Even when the world was called Pangaea, there were still plates. The plates begin to move, however, only about 1 cm a year. This is why we now have continents. Scientists predict that a few 100 years from now, the world will look even more different.

If you type in the earths tech tonic plates into wikipedia, it might help you a little more than i did.

We can never know what the weather on Pangaea was really like, as it was in existence around 200 million years ago. However, many think that the weather was probably severe, since the supercontinent was so large that most of its landmass was inland, away from the cooling effects of the ocean around it. It was probably very hot and dry- maybe around 150 degrees F!- but also experiencing extreme weather patterns such as monsoons and superhurricanes (since the large ocean would have made more room for a storm to gain momentum). Additionally, parts of Pangaea were situated over the poles, which meant those places were extremely cold.

The evidence supporting the existence of Pangaea includes the matching shapes of continents like South America and Africa, similar rock formations and mountain ranges on different continents, and fossils of the same species found on continents that are now far apart. Additionally, the distribution of certain plant and animal species across different continents suggests that they were once connected.

Alfred Wegener proposed the theory of Pangaea, the supercontinent, in 1912 based on his ideas of continental drift. However, his theory was not widely accepted until after his death in 1930 when further evidence supported the idea of plate tectonics.

After Pangaea began to break up, the continents drifted apart due to plate tectonics. Over millions of years, the separated continents moved to their current positions on Earth's surface. This process resulted in the formation of the continents we recognize today.

1. Fossil evidence of similar plant and animal species found on different continents.
2. Geological evidence of matching rock formations and mountain ranges on different continents.
3. Climate evidence, such as glacial deposits and ancient climate patterns, that suggest continents were once connected.

Pangaea started to break up during the Triassic Period. It continued to split apart in the Jurassic Period and was almost complete in breaking up in the Cretaceous Period. After that it formed into the landmasses that we see today.

About 200 million years ago,there were no crustal plates to speak of.There was only one supper continent,pangea.This was an idea suggested by Alfred Weneger, a german scientist.According to him,Pangea broke into pieces (crustal plates) and slowly moved until they reached their present position

The splitting of Pangaea into two continents is part of the theory of plate tectonics. This theory explains how the Earth's outer layer is divided into large plates that move and interact with each other, reshaping the Earth's surface over millions of years. Pangaea was a supercontinent that existed about 335 million years ago and eventually split into Laurasia and Gondwana, which later separated into the continents we have today.

Alfred Wegener did not develop the theory of climatic regions. He is, however, known for proposing the theory of continental drift, suggesting that Earth's continents were once joined together as a single landmass called Pangaea. This idea laid the foundation for the modern theory of plate tectonics.

supercontinent

Evidence for Pangaea includes the fit of the continents, where coastlines match up like puzzle pieces, as well as similarities in rock formations, fossils, and mountain ranges across different continents. Additionally, paleoclimate data, such as glacial deposits in tropical regions, supports the idea of a supercontinent in the past.

Pangaea broke up during the Mesozoic Era, specifically in the Late Triassic period around 200 million years ago. The breakup of Pangaea eventually led to the formation of the modern continents we see today.