ILST 2655 Lecture Notes - Lecture 1: Cenozoic, Paleozoic, Exogeny
Document Summary
Geographers describe the earth"s geologic history through a temporal system known as the geologic time scale: eons,eras, periods, epochs: alfred wegener. Saw that pieces of continents look like jigsaw puzzle that fits(especially. Continents are floating on ocean(think crackers on hot tomato soup). Improved his theory by adding movement of plates are caused by convection current: pangea. Slow seperation of continent because of plate movement. Same rocks in n/s america with africa. Mantle- convection current happen here(in mantle & asthenosphere) Asthenosphere(lower layer asthenosphere is at top of mantle) Lots of hot solid rocks that it makes the rocks flow like liquid. A discontinuity is a plane or surface that marks a change in physical or chemical characteristics in a soil or rock mass. World"s litosphere is broken up into plates(tectonic plates) 8 major plates, & lots of minor plates. 2 phenomena of plate tectonics(a. k. a 2 relief features of continent) Any action that causes breaking & bonding of earth"s litosphere ie. earth deformed.