Sea Floor Spreading Diagram
Ocean floor diagram worksheet.
Sea floor spreading diagram. Lower mantle semi rigid the deepest parts of the mantle just above the core. Schematic diagram showing the mechanism of seafloor spreading. This diagram provides evidence of seafloor spreading by showing the ages of ocean floor in the atlantic and eastern pacific oceans. Start studying sea floor spreading 3 2.
Lithosphere the crust plus the rigid upper mantle. The rising convectional currents continuously bang thick but strong oceanic sima crust and the hammering effect leads to the development of cracks joints fractures and disintegration of oceanic ridges. Start studying section 4. Learn vocabulary terms and more with flashcards games and other study tools.
Figure showing sea floor spreading the intense heat generated by radioactive substances in the mantle beneath the lithosphere seeks a path to escape and forms convection currents. Learn vocabulary terms and more with flashcards games and other study tools. The mid ocean ridge was mapped by sonar b. The rifting processes coinciding with the onset of a new spreading centre typically start with an upwelling of hot mantle rocks under continental lithosphere the heat leading to uplift and associated erosion.
Select the letter that is true about the mid ocean ridge. Sea floor spreading in the early 1960s princeton geologist harry hess proposed the hypothesis of sea floor spreading in which basaltic magma from the mantle rises to create new ocean floor at mid ocean ridges. The red colors are the youngest parts of the seafloor where fresh new crust is formed as lava seeps up from the deep interior of the earth at spreading ridges. Seafloor spreading is a process that occurs at mid ocean ridges where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge.
History of study earlier theories by alfred wegener and alexander du toit of continental drift postulated that continents in motion plowed through the fixed and immovable seafloor. The size of an ocean is determined by how fast is created at a mid ocean ridge. Read the definitions below then label the seafloor spreading plate divergence diagram.