Science Lesson 2: Collide, Move Apart, and Slide and Triangulation Method Flashcards
He proposed the continental drift theory.
Alfred Wegener
It is also known as plate margins
Plate Boundaries
Used to determine the epicenter by where it intersects
Triangulation Method
Two continental crustal plates move toward one another
Continental-Continental
Move apart from each other, outwards, tensional force
Divergent Plate Boundaries
Uses seismic data collected from at least 3 different locations
Triangulation Method
Causes one plate to subduct from the other
Oceanic-Oceanic
Slide past horizontally, lateral, shearing force
Transform Plate Boundaries
The point on the Earth’s surface vertically above the focus of an earthquake
Epicenter
Produces new seafloor
Divergent Plate Boundaries
Print out/display screen
Seismogram
Relating to an earthquake vibration
Seismic
Process at which oceanic crust sinks down the continental crust and goes back to the mantle
Subduction
It is a line where large moving plates meet
Plate Boundaries
Deep, narrow depression on the ocean seafloor caused by the collision and/or subduction of plates
Trench