All continental rifts have three geometrical characteristics in common: they are typically asymmetric, have widths that are typical of the region in which they originate, and are segmented along axes at a length scale that is likewise typical of the region.
- More about continental rifting :
- There are weak spots in the continental lithospheric plate where continental rift zones can emerge. A rift zone in a continental plate that enlarges to the point of rupturing it frequently evolves into a mid-ocean ridge, with seawater filling the hole.
- The four largest active continental rift valleys on Earth are the East African Rift, the Baikal Rift Valley, the West Antarctic Rift, and the Rio Grande Rift.
- The last rifting took place about 240 million years ago, Pangaea was a real place. Approximately 200 million years ago, this supercontinent started to fragment. Pangaea split into fragments over the course of millions of years, and each piece migrated away from the other. These components gradually came together to form the continent that is known today.
To know more about continental rifting, kindly click on the link below :
https://brainly.com/question/90770?referrer=searchResults
#SPJ4
