L2 vocab Exam 1 Flashcards
(22 cards)
Topography
Variations in elevation.
Bathymetry
Variation in depth.
Isostasy
The conditon that exists when the buoyancy force pushing the lithosphere up equals the gravational force pulling the lithosphere down.
Lithosphere plate
One of many pieces of the lithosphere (the Earth’s relatively riqid shell) that are sepreated from one another by breaks. (plate boundries)
Asthenosphere
The layer of the mantle that lies between 100-500 km and 350 km deep under the moho
Seismic waves
waves of energy emitted at the focus of an earthquake
Deformation
a change in space, position or orientation a material, by bending, breaking or flowing.
Heat
Thermal energy resulting from the movement of molecules.
Plate tectonics
States that tthe Earth’s. outer shell, rather than being static and consists of discrete plates that slowly more relative to one another.
Continental drift
The hypothesis that continents have moved and are still moving slowly across the Earth’s surface.
Pangea
A supercontinent that assembled at the end of the Paleozonic Era.
Gondwana Sequence
A supercontinent that consisted of today’s South America, Africa, Antartica, india and Austrillia.
Abyssal plain
A broad, relatively flat region of the ocean that lies at least 4.5 km below sea level.
Mid-ocean ridge
A 2km high submarine mountain belt that forms along a divergent oceanic plate boundary.
Fracture zone
A narrow band of vertical factures in the ocean floor
Trench
Volcanic arc
A curving chain of active volvanoes form adjacent to a convergent plate boundary.
Seamount
An isolated submarine mountain.
Heat flow
The rate at which heat rises from the Earth’s interior up to the surface.
Seafloor spreading
The gradual widening of an ocean basin as new oceanic crust forms at a mid-ocean ridge axis and then moves away from the axis
Subduction
The process by which one oceanic plate bends and sinks down into the atmosphere beneath another plate.
Lithosphere
The relatively rigid, nonflowable, outer 100-to 150- km thick layer of the Earthconstituting the crust all to the top part of the mantle.