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Paleozoic Plate Tectonics

The continents came together in a giant landmass known as Pangaea around 250 million years ago; mountain ranges were created from these collisions.

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Paleozoic Plate Tectonics

Why were the continents near the South Pole?

During the Paleozoic the continents were joined and they were not in their current latitudes. In the late Cambrian, for example, they were clustered around the south polar region. It's probably just chance that they found their way there. This was hundreds of millions of years before the first human expedition reached the South Pole in 1911.

The Paleozoic

The Paleozoic is the furthest back era of the Phanerozoic and it lasted the longest. But the Paleozoic was relatively recent, beginning only 570 million years ago. Compared with the long expanse of the Precambrian, the Phanerozoic is recent history. Much more geological evidence is available for scientists to study so the Phanerozoic is much better known.

The Paleozoic begins and ends with a supercontinent. At the beginning of the Paleozoic, the supercontinent Rodinia began to split up. At the end, Pangaea came together.

Formation of Pangaea

A mountain-building event is called an orogeny. Orogenies take place over tens or hundreds of millions of years. As continents smash into microcontinents and island arcs collided, mountains rise.

Geologists find evidence for the orogenies that took place while Pangaea was forming in many locations. For example, Laurentia collided with the Taconic Island Arc during the Taconic Orogeny (Figure below). The remnants of this mountain range make up the Taconic Mountains in New York.

The Taconic Orogeny is an example of a collision between a continent and a volcanic island arc

The Taconic Orogeny is an example of a collision between a continent and a volcanic island arc.

Laurentia experienced other orogenies as it merged with the northern continents. The southern continents came together to form Gondwana. When Laurentia and Gondwana collided to create Pangaea, the Appalachians rose. Geologists think they may once have been higher than the Himalayas are now.


Pangaea was the last supercontinent on Earth. Evidence for the existence of Pangaea was what Alfred Wegener used to create his continental drift hypothesis, which was described in the chapter Plate Tectonics.

As the continents move and the land masses change shape, the shape of the oceans changes too. During the time of Pangaea, about 250 million years ago, most of Earth’s water was collected in a huge ocean called Panthalassa (Figure below).

Map of the supercontinent Pangaea

Pangaea was the sole landform 250 million years ago, leaving a huge ocean called Panthalassa, along with a few smaller seas.


  • The Paleozoic began with the supercontinent Rodinia and ended with the supercontinent Pangaea.
  • As continents come together, orogenies build up mountain ranges.
  • Pangaea was a giant landmass made of all of the continents around 250 million years ago.


  1. What happens to create an orogeny? How are plate tectonics processes related to orogenies?
  2. How did Pangaea come together?
  3. How is the creation of Pangaea related to events like the Taconic orogeny?

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Use this resource (watch up to 8:44) to answer the questions that follow.

  1. What were the continents like at the beginning of the Mesozoic?
  2. How did the area between North/South America and Eurasia/Africa evolve from 200 million years ago to 150 million years ago to 90 million years ago?
  3. Why did a desert exist in the region of the Sahara and the United Kingdom 250 million years ago?
  4. Why is the Grand Canyon important? What is displayed there from 265 million years ago?
  5. What does this video present as the reason for the mass extinction at the end of the Permian?


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orogeny A mountain building event, usually taking place over tens or hundreds of millions of years.

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