







































A long-standing question regarding the strength of olivine, the primary component of Earth’s mantle, has now been answered. This study has implications for how we understand now tectonic plates form and move. Geology News — ScienceDaily
IMG title=”” alt=”” src=”http://www.mineralfossil.com/wp-content/uploads/2014/01/wpid-e89c0186cb888a4d5856510ab5b9b2df.jpg” IMG class=”hide” alt=”Tempesta solare pi