In the case of the Falklands these stratifications run northward, and are very similar to formations in South Africa which run southward; comparison of the two serves as evidence that the block of sand sediments which contains the islands has been rotated.
In the case of the Falklands these stratifications run northward, and are very similar to formations in South Africa which run southward. Comparison of the two serves as evidence that the arenaceous block which contains the islands has been rotated.