All the land masses on the planet were joined together into one huge continent called Pangaea.

Toward the end of the era, the continents gathered together into a supercontinent called Pangaea, which included most of the Earth's land area.

Geologically, the Mesozoic starts with almost all the Earth's land collected into a supercontinent called Pangaea.

The combined supercontinent is called Pangaea.

The theory currently accepted by the scientific community is that a single land mass called Pangaea slowly separated by way of continental drift.

About 250 million years ago during the early Triassic period, Atlantic Canada laid roughly in the middle of a giant continent called Pangaea.

The collision involved all of the other continents as well, and formed a supercontinent scientists call Pangaea.

The thesis was that all the continents were once a super land mass called Pangaea.

Groundbreaking research by Alfred Wegener reveals that all the continents were once connected as one single land mass he called Pangaea.

The result of the Variscan Orogeny was that almost all continental mass became united in a supercontinent called Pangaea.