Earth is differentiated into three main layers (crust, mantle and core) due to different chemical composition. Our planet has a dense iron core, a mantle of silicates rich in iron and magnesium, and a crust with lighter silicates.
Permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this website. Digital assets without any copyright restrictions are public domain.
Modified from “Beauty from the Beast: Plate Tectonics and the Landscapes of the Pacific Northwest,” by Robert J. Lillie, Wells Creek Publishers, 92 pp., 2015, www.amazon.com/dp/1512211893.