In the middle of the ocean there is much seismic activity and there material is constantly being thrust up to form mid-oceanic ridges which are larger in scale than are the Himalayas.
Material is constantly being thrust up and forms mid-oceanic ridges which are larger in scale than the Himalayas. In the middle of the ocean there is much seismic activity.
In the middle of the ocean there is much seismic activity. Material is constantly being thrust up and forms mid-oceanic ridges which are larger in scale than the Himalayas.
In the middle of the ocean there is much seismic activity. Material is constantly being thrust up and forms mid-oceanic ridges which are larger in scale than the Himalayas.