The change of the earth's crust as a result of the movement apart and make it look current. Cracks in the stone age of the Alpine lithosphere and oceans.
The process has changed as a result of plate tectonics causes the lithosphere to move separately to make it look like today. In a crevice of the stone age, and lithosphere plates on the klangomhatmuthon mountains.
The process of change as a result, the crust of the earth keepers of the public sector has moved apart from each other so that the current as the cracks of the earth in middle of the ocean and mountains on Stone Age