we used to be one big continent = continetal dift first established in 1858, antonio snider-pellegrini, noted similiar foosils also 1831-1914 edward suess seen fern fossils present acorss all southern continents
supercontinent - gondwana and tethys ocean land briges between continents.
edward - tries to explain oceans via cooling and sinking of materials with diff densities
Alfred wgeener 1880-1930matches continents at 200m isobath - proposes continental drift theory largely reject - lack mechanism evidence - plant fossils-animal fossils-geological formations such as coal bed - Paleoclimatological evidence from glacial deposits - s gondwana
emergence of plate tectonics - continental drift evidence -formation of mountain range via compression & folding -Collision between plate throws up mountian ranges - Rift valleys and transform fualts consistent with tension from sea floor spreading
Geomagnetism the earths magnetic field reverses approx. every 0.1 to 1 Ma this is seen in basaltic rocks - solidified magma from volcanic eruptions - they are ricj in iron = ferromagnetic material - retains orientation od magnetic field upon cooliing - terrestrial rcords also document the reverse
Vine-matthews-morley Hypothesis Independently developed in the 60- hypothesis -new ocean crust formed at ocean ridgea-magnetic orientation preserved - magnetometer records should reveal magnetic anomalies - magnetic orientation should show striped pattern parallel to ridges
volcanic chains oceanic crust moves over hot spot = hawian chain - youngest is the most active - oldest is subside. - subsudence and erosion eventually turn islands into guyots - emperor seamount chain
pacific ring of fire Earths most active volcanoes driven by friction associated with convergence/subduction these are common ocean-ocean convergence