Formation and Break-Up of Pangaea

Which event marked the beginning of the break-up of Pangaea?

What was the primary result of the collision between India and Eurasia?

During which geological period did the continents reach their current positions?

Which supercontinent existed around the South Pole during the late Cambrian period?

What significant geological process occurred from the late Carboniferous to the Triassic period?

What phenomenon caused the opening of the Atlantic Ocean?

What key event took place during the mid-Ordovician Period?

Which statement is true regarding the formation of the North American continent?

Formation of Continents

The Gondwana Supercontinent, including Baltica, Siberia, and Laurasia, existed around the South Pole during the late Cambrian period (514 Ma).
During the mid-Ordovician Period (458 Ma), Laurasia collided with Baltica, closing the Iapetus Sea.
These collisions resulted in the pre-Pangaea continent during the early Devonian period (390 Ma).
The North American continent formed by the late Carboniferous (306 Ma).
By the Triassic Period (255-210 Ma), Pangaea existed.
Pangaea began to break apart from 210-180 Ma.
The breakup of Pangaea continued into the Late Cretaceous period, creating larger oceans.
Continental drift proceeded into the Tertiary Period.
Continents reached their current positions during the Quaternary period.

Pangaea's Break-Up

The present-day continents were part of the supercontinent Pangaea, existing until approximately 200 Ma.
Around 160 Ma, Pangaea split into two large landmasses: Gondwanaland and Laurasia.
The subcontinent of India moved northward and separated from Gondwana around 140 Ma.
India collided with Eurasia, initiating the formation of the Himalayan mountain range.
Australia separated from Antarctica around 100 Ma, further breaking Gondwana apart.
The separation of Gondwana and Laurasia led to the opening of the Atlantic Ocean.

Explore the fascinating history of the formation and break-up of the supercontinent Pangaea. This quiz covers key events from the late Cambrian to the Quaternary period, including the collisions of ancient continents and the eventual drift that shaped today's geography.