Geophysicist and geologist Tanya Atwater talks about the Deep Sea Drilling Project and the confirmation of magnetic reversals that provided strong evidence of seafloor spreading and plate tectonics.
Geophysicist and geologist Tanya Atwater talks about the correlation between plate boundaries and earthquake distribution.
Geophysicist and geologist Tanya Atwater discusses the differences between continental and oceanic crust. Continental crust tends to be much thicker and would be thicker still were it not for the forces of gravity and erosion. In addition, oceanic c...
Geophysicist and geologist Tanya Atwater talks about plate tectonics as a mechanism by which Earth's interior sheds the tremendous heat that builds up as a result of radioactive decay.
Geophysicist and geologist Tanya Atwater talks about the super continent Pangaea, thought to have broken up into the continents as we know them today beginning about 200 million years ago.
Geophysicist and geologist Tanya Atwater discusses the role of Alfred Wegener in bringing together a variety of evidence in support of the theory of continental drift.
Geophysicist and geologist Tanya Atwater discusses isostasy, which allows objects at the surface of Earth to float in equilibrium, and talks about how it helps define Earth's topography.
Geophysicist and geologist Tanya Atwater compares the relatively neat sea floor with continents, which she terms a "mess." She attributes these differences to the predictable and "tidy" process of seafloor spreading, as compared to the crashing toge...
Geophysicist and geologist Tanya Atwater notes that the line between oceans and continents, commonly known as the coast, is actually very arbitrary and subject to change over time. She also talks about implications of global warming for coastal regi...
Geophysicist and geologist Tanya Atwater talks about mistakes made by Alfred Wegener in formulating his theory of continental drift, some of which created doubt and skepticism among fellow geologists.