Many geologists theorize that the trail of volcanic craters and cinder cones along the Snake River plain of southern Idaho was produced as the North American continent slid westward over a stationary’ «plume,» a vertical channel through which molten rock rose intermittently from the Earth’s (…)
Descubre más desde Clases particulares GMAT
Suscríbete y recibe las últimas entradas en tu correo electrónico.