Geology Chapter 2 Flashcards
asthenosphere
hot and slowly flowing layer of relatively weak
lithosphere
cool,strong outermost layer of Earth
crust
variable thickness, is the outer rock layer of the
Earth
convection
causes water to become less dense and more unstable as it rises to the top
seismology
the study of earthquakes and the passage of seismic waves through earth
plate tectonics
the creation,movement, and destruction of plates
hot spots
where partly molten material are hot and buoyant enough to move up through the mantle and overlying plate tectonics
Wadati-Benioff zones
dipping planes of earthquakes of earthquakes
-the paths of descending plates at subduction zones from a shallow dip to nearly vertical
paleomagnetism
the study of the magnetism of rocks at the time their magnetic signature formed
Modern Evidence of Plate Tectonics
- morphology of the ocean floor
- age of the oceanic crust
- magnetic properties of the oceanic crust
- hot spots
- direct observation of plate movement via GPs
- seismology and location of earthquakes
Hot Spot
thermal anomaly rising from the depths of the Earth that melts the crust and causes the formation of volcanoes