Quiz 3- Ch.3/2 Flashcards
Continental Drift
large scale movement of continents across Earth’s surface driven by plate tectonic processes
Pangea
a supercontinent comprised of all the present day continents as we know them and then broke apart in the Mesozoic Era
Seafloor Spreading
the mechanism by which new crust is created at mid-ocean ridges. As continents move apart magma wells up in the rifts and creates new crust spreading laterally away from the rift continually replaced by newer crust
Number of plates and their composition
Earth is made up of 13 major plates and several smaller ones made up of rigid lithosphere all moving across the asthenosphere which is also in constant motion
divergent boundaries
plates move apart and new lithosphere is created causing volcanoes and earthquakes at mid-ocean ridges (plate area increases) i.e. continental drift
convergent boundaries
plates move together and one plate is recycled into the mantle causing deep sea trenches, earthquakes and mountains (plate area decreases) i.e. ocean-ocean convergence, ocean-continent convergence
transform faults
plates slide past each other causing earthquakes and offsets in geologic features (plate area doesn’t change) i.e. mid ocean ridges, continental transform faults
2 consequences of continental crust
- because continental crust is lighter it is not as easily recycled as oceanic crust
- because continental crust is weaker, plate boundaries involving continental crust tend to be more spread out and complicated than those involving oceanic plate boundaries
Rodinia
supercontinent before pangea formed 1.1 billion years ago and began to split 750 million years ago
mantle plumes
slender cylinders of fast rising materials less than 100km across that come from the deep mantle (i.e. Hawaii) They’re though to be the cause of mass extinctions
seismic waves
ground vibration produced by earthquakes
plate tectonics theory
theory that explains the creation and destruction of Earth’s lithospheric plates and their movement across Earth’s surface
Geodynamo
the global geosystem that produces Earth’s magnetic fields driven by convection in the outer core