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Alfred Wegener
Father of theory of tectonic plates
Transform boundary
plates slide past
transform boundary
earthquakes
convergent boundary
plates collide, mountains and volcanoes form, new crust forms
divergent boundary
plates move away from eachother
continental drift theory
continents were once joined together and have since drifted apart
evidence of continental drift
fit of continents, fossils of same species, similar rock formations
plate tectonic theory
explains movements and interactions of earth’s lithosphere divided into tectonic plates
cause of tectonic plate movement
convection current in earth’s mantle
speed of tectonic plate movement
2 to 10 cm per year
oceanic-oceanic convergence
subduction when 1 of 2 plates is descending beneath the other
oceanic-continental convergence
subduction occurs, trench and volcanic arcs form, produces mountains and volcanoes
subduction
when 1 of 2 plates is descending beneath the other
continental-continental
collision forms fold mountains like Himalayas, shallow earthquakes but no volcanoes
transform plate boundary
occurs when two plates slide past eachother horizontally, opposite directions or same directions or different speeds