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Tethys
Pagaea split so it created 2 smaller super continents called Gondwanaland and Laurasia.
Pangaea started to break apart about 250 million years ago forming Laurasia (Not sure if that is spelled right) and Gondwanaland (I'm serious that's the name, ridiculous right) about 185-200 million years ago So your answer is Laurasia and Gondwanaland, one of the two. Hopes this helps :)
Pangaea is believed to have formed around 300 million years ago and began to break up around 175 million years ago.
Laurasia and Gondwanaland
Laurasia and Gondwanaland formed during the late Carboniferous period, around 300 million years ago, through the breakup of the supercontinent Pangaea. Laurasia was located in the northern hemisphere, while Gondwanaland was in the southern hemisphere.
Pangaea broke into Gondwanaland and Laurasia.
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Tethys
Pangaea, Laurasia, and Gondwanaland are all supercontinents that existed millions of years ago. Pangaea was the ancient supercontinent that eventually split into Laurasia in the north and Gondwanaland in the south due to tectonic plate movements. These supercontinents played a significant role in shaping the Earth's landmasses and continents as we know them today.
The two continents that formed when Pangaea broke apart are Laurasia in the north and Gondwana in the south. These two supercontinents eventually broke up further to form the continents we have today.
Laurasia and Gondwanaland were part of the supercontinent Pangaea, which formed around 335 million years ago through the collision and joining of several smaller landmasses. As tectonic plates shifted and moved over millions of years, Laurasia drifted northward and Gondwanaland moved southwards to eventually break apart and form the continents we know today.
Pangea split into two continents: Laurasia and Gondwanaland.
One of the two supercontinents that Pangaea split into is Laurasia.
When Pangaea split in two, there where two island landmasses. The Northern landmass was Laurasia. The Southern landmass was Gondwanaland.
When the continents separated, it is referred to as continental drift or plate tectonics. This is the theory that explains how the Earth's continents move and change position over time due to the movement of tectonic plates.