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46 Cards in this Set

  • Front
  • Back

Continental drift theory

Continents have not always been in their current locations but have drifted here over millions of years

What details support the continental drift theory?

1. Geological structures match from continents


2. fossils are found of the same species in different continents


3. All continents used to have glaciers

Paleoglaciation

The extent of ancient glaciers and the rock markings they leave behind

Tectonic plates

The surface of Earth is broken into large, movable slabs of rocks called tectonic plates

Volcanoes

openings in Earth's surface that when active spew out gases, chunks of rocks, and melted rocks

Earthquake

A sudden ground shaking release of built up energy at or under Earth's surface

Mid-Atlantic Ridge

A long mountain range running down the middle of the Atlantic Ocean

Magnetic Reversal

The process in which Earth's magnetic field reverses its direction

Paleomagnetism

The study of the magnetic properties of ancient rocks.

Magma

Molten rocks from beneath Earth's surface

Why does magma rise?

It is less dense than materials around it

What happens when magma breaks through Earth's surface?

Magma cools and hardens at a spreading ridge

Spreading ridge

The region where magma breaks through Earth's surface, forming new sea floor

Sea floor spreading

The process in which magma rises to Earth's surface at spreading ridges and pushes older rocks aside

Plate tectonic theory

The movement of tectonic plates

Hot spot

An area where molten rock rises to Earth's surface

Lithosphere

The crust and upper portion of the upper mantle

Crust

Earths outer most layer made up of light materials

Mantle

Earth's thickest layer

Outer core

A liquid layer under the mantle

Inner core

Earth's centre

Asthenosphere

Molten layer of the upper mantle

Ridge push

When magma cools when it reaches the surface, solidifies, and is pushed aside as new magma pushes from below

Rift valley

When currents of magma rises on land and forms a steep sided valley

Subduction

The action of one tectonic plate pushing underneath another

Slab pull

When the denser oceanic plate subducts under the lighter continental plate, and the rest of the plates follow

Plate boundary

An area where two plates are in contact

Divergent plate boundaries

Areas where plates are spreading apart

Convergent plate boundaries

Areas where plates meet

Transform plate boundaries

Areas where plates move past each other

Trench

A deep underwater valley that forms when an oceanic plate collides with a continental plate and is forced to slide beneath it

volcanic belt

A long chain of volcanoes

Volcanic arc

A long chain of volcanic islands

faults

Large breaks in rock layers

Transform fault

A fault that occurs at a transform plate boundary

Focus

Where an earthquake starts

epicentre

The point on the Earth's surface directly above the focus

Seismology

The study of earthquakes and seismic waves

Surface waves (L-waves)

Seismic waves that ripple along Earth's surface

Primary waves (Waves (P-waves)

A type of seismic wave that travels at 6km/s through Earth's crust, causing the ground to move in the direction of the waves motion

Composite volcanoes

Cone shaped, near subduction zones, explosive reuptions, thick lava

Rift eruptions

Occurs at ridges where plates separate, not very explosive but lots of magma

Shield volcanoes

Flat shield shaped, near hot spots, less explosive, thinner fast lava

Ocean-continental plate convergence

Oceanic plate subducts under the continental plat, forming a trench and mountain ranges



Volcanoes can form and earthquakes can occur

Oceanic-oceanic plate convergence

Cooler denser plate subducts under the less dense plate. May produce a volcanic island arc

Continental-Continental plate convergence

Edges fold and crumple, forming mountain ranges