Chapter 2: Plate Tectonics Flashcards
plate tectonics
the grand unifying theory of geology which says that the Earth’s crust is made up of about 20 plates/pieces that slowly move relative to one another
continental drift
the theory that the continents broke apart and moved away from each other into the positions we know today
evidence of continental drift
- glacial striations and till deposits
- distribution of climate belts
- distribution of fossils
- matching geologic units
mid-ocean ridges
sub-marine mountain ranges in the middle of an abyssal plain that are roughly symmetrical on either side of the ridge axis
deep sea trenches
bordering volcanic arcs, trenches are elongate, deep troughs in the ocean
fracture zones
lie at right angles to mid-ocean ridges and interrupt the continuity of the ridge axis
seamount chains
where numerous, formerly volcanic mounts of basalt poke up from the ocean floor
how does thickness of the ocean sediment layer vary further away from a mid-ocean ridge?
the ocean sediment layer become thicker further away from the mid-ocean ridge due to uplift of the oceanic crust in that part of the ocean and new crust forming around the mid-ocean ridge
seafloor spreading
the theory that says that at mid-ocean ridges, the basalt formed at the ridge moves away from the ridge axis, widening the ocean basin
paleomagnetism
the study of rocks that can preserve a record of the Earth’s magnetic field in the past.
what does paleomagnetism mean
in rocks that have magnetic field, ancient rocks may not have the same oriented dipole as the Earth today because of how the Earth’s poles switch periodically
apparent polar-wander path
successive position of dated paleo-poles trace out a curving line that shows how the continents moved relative to the Earth’s poles
normal and reverse polarity
normal: the polarity we have today
reverse: the opposite polarity of what we have today
active margins
continental boundaries that are also a plate boundaries
passive margins
continental margins that are not a plate boundaries