Scientists have found a brand new layer of partly molten rock beneath the Earth’s crust which may assist settle a long-standing debate about how tectonic plates transfer. The molten layer is situated about 100 miles from the floor and is a part of the asthenosphere, which is essential for plate tectonics as a result of it varieties a comparatively comfortable boundary that lets tectonic plates transfer by way of the mantle. The researchers discovered, nonetheless that the soften doesn’t seem to notably affect the movement of mantle rocks. As a substitute, they are saying, the invention confirms that the convection of warmth and rock within the mantle are the prevailing affect on the movement of the plates.