Sea-Floor Spreading The mechanism for continental drift Theory of Continental Drift • Remember Wegner proposed that over time, continents drift apart? – Well how.
Download ReportTranscript Sea-Floor Spreading The mechanism for continental drift Theory of Continental Drift • Remember Wegner proposed that over time, continents drift apart? – Well how.
Sea-Floor Spreading The mechanism for continental drift Theory of Continental Drift • Remember Wegner proposed that over time, continents drift apart? – Well how did this happen? Mid-ocean Ridges • Scientist (Harry Hess) noticed that there are mountain ranges that exist under water in the Oceans – Ex: Mid-Atlantic Ridge • These mid-ocean ridges exist due to SEA-FLOOR SPREADING Sea-Floor Spreading • The process by which new oceanic lithosphere is created as older materials are pulled away. • As tectonic plates move away from each other the sea floor spreads apart and magma rises to fill in the gap. Sea Floor Spreading Video Sea-Floor Spreading Explained Sea-Floor Spreading • Sea-floor spreading creates new oceanic crust – Newer crust is found at the center or near the ridge – Older crust is found further away from the ridge (because it is being pushed away from the center of the ridge by new rising magma) Magnetic Reversals • Strongest evidence for sea-floor spreading: – Magnetic Reversals recorded in ocean floor • Magnetic reversals: – The switching of Earth’s north and south pole over time Magnetic Reversals and the Sea Floor • Magnetic minerals found in the magma that bubbles up at the ridge align with the Earth’s magnetic field. – Once the molten rock cools, it’s like tiny compasses set in stone • This record is carried slowly away from the center of the ridge, forming bands of alternating magnetic reversals – Every time there was a magnetic reversal, a new band was formed Magnetic Reversals • Why would Magnetic Reversal bands be evidence of sea-floor spreading? – These bands show that different parts (bands) of the crust were formed over different time periods – Because with each band, the rock patterns that form that part of the crust are different from the other bands nearby Magnetic Reversals Magnetic Reversals