<P> Widespread distribution of Permo - Carboniferous glacial sediments in South America , Africa , Madagascar , Arabia , India , Antarctica and Australia was one of the major pieces of evidence for the theory of continental drift . The continuity of glaciers , inferred from oriented glacial striations and deposits called tillites , suggested the existence of the supercontinent of Gondwana , which became a central element of the concept of continental drift . Striations indicated glacial flow away from the equator and toward the poles , based on continents ' current positions and orientations , and supported the idea that the southern continents had previously been in dramatically different locations , as well as being contiguous with each other . </P>
<P> Widespread distribution of Permo - Carboniferous glacial sediments in South America , Africa , Madagascar , Arabia , India , Antarctica and Australia was one of the major pieces of evidence for the theory of continental drift . The continuity of glaciers , inferred from oriented glacial striations and deposits called tillites , suggested the existence of the supercontinent of Gondwana , which became a central element of the concept of continental drift . Striations indicated glacial flow away from the equator and toward the poles , based on continents ' current positions and orientations , and supported the idea that the southern continents had previously been in dramatically different locations , as well as being contiguous with each other . </P>
what is the name for the supercontinent in the continental drift hypothesis
what is the name for the supercontinent in the continental drift hypothesis
Gondwana
Gondwana