Rodinia
Rodinia is a relatively famous supercontinent that existed towards the end of the Proterozoic Eon. Nevertheless, many people don't know it. It existed from the Stenian period to right before the Cryogenian period encompassing nearly all of the Tonian period. It was almost exactly on the opposite side of where Pangea formed. It turned inside out during the Cryogenian period to become Pannotia, leaving out exposed rocks that sucked up carbon dioxide, thus causing a snowball earth. Pannotia somehow still didn't make it into the Phanerozoic Eon. Rodinia wasn't by itself unlike other supercontinents. It had a continent to the west of it as its companion. Made of parts of South America and Africa, this continent was called Congo. While Rodinia turned itself inside out, Congo got caught in between the two halves, completing Pannotia.
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