In geology, a supercontinent is a landmass comprising more than one continental core, or craton. The assembly of cratons and accreted terranes that form Eurasia qualifies as a supercontinent today.
Identifier (URI) | Rank |
---|---|
dbkwik:resource/T81XMbsPBPG_2c7yDiu6yQ== | 5.88129e-14 |
dbr:Supercontinent | 5.88129e-14 |