chapter 4. inside the earth crust mantle core lithosphere asthenosphere mesosphere tectonic...
TRANSCRIPT
PLATE TECTONICS
Chapter 4
SECTION 1 VOCABULARY
Inside the EarthCrustMantleCoreLithosphereAsthenosphereMesosphereTectonic Plate
THE COMPOSITION OF THE EARTH The Crust
5-100km thickThinnest layer
Two typesContinentalOceanicMade of…
THE COMPOSITION OF THE EARTH The Mantle
ThickerMost of the mass
Crust too thick Observations Ocean floor Made of…
THE COMPOSITION OF THE EARTH The Core
Mantle to the coreMade of…Not made of..
1/3 of the Earth’s mass
THE PHYSICAL STRUCTURE OF THE EARTH
Five layers Inner Core
Solid, dense Outer Core
Liquid layer Mesosphere
Strong Asthenosphere
Plastic layer Lithosphere
Tectonic plates
TECTONIC PLATES Names of the
plates Fit together Difference
OceanContinent
Plates include… Like ice cubes
MAPPING OF THE EARTH’S INTERIOR
Never drilled through the crust
Seismic waves Seismographs
SECTION 2 VOCABULARY Restless Continents
Continental DriftSea-floor Spreading
WEGENER’S CONTINENTAL DRIFT HYPOTHESIS Alfred Wegener
Continental DriftFit togetherSimilar types of
rocks and climatic conditions
THE BREAKUP OF PANGAEA
Observations Single, huge
continent (supercontinent)
245 million years ago
Laurasia and Gondwana (180 million years ago)
SECTION 3 VOCABULARY The Theory of Plate Tectonics
Plate tectonicsConvergent BoundaryDivergent BoundaryTransform Boundary
TECTONIC PLATE BOUNDARIES Plates Touch Three Types
Convergent Boundary
Divergent Boundary
Transform Boundary
How they move earthquakes
CONVERGENT BOUNDARY Collide Kind of crust Three Types
DIVERGENT BOUNDARY Separate New Sea Floor Mid-Ocean
Ridges
TRANSFORM BOUNDARIES
Slide Past Each other horizontally
San Andreas Fault
POSSIBLE CAUSES OF TECTONIC PLATE MOTION Plate Tectonic
Theory Solid Rock Flows Changes in
Density Thermal Energy Three possible
causes
THREE CAUSES OF TECTONIC PLATE MOTION
Ridge Push Convection Slab Pull
TRACKING TECTONIC PLATE MOTION Type and Shape
of the plate Interacts with
Plates So Slow and
Gradual GPS Radio Signals
SECTION 4 Deforming the Earth’s Crust Vocabulary
CompressionTensionFoldingFaultUpliftSubsidence
DEFORMATION Spaghetti
BendingBreaking
Rock Layers Stress
COMPRESSION AND TENSION
CompressionSqueezed or
CollidedConvergentMountain Ranges
TensionStretchDivergentMid-Ocean Ridge
FOLDING Bending of Rock
LayersHorizontal layers
Types of FoldsAnticlinesSynclinesMonoclineDifferent sizes
FAULTING Stress is applied Fault Blocks Hanging wall
and footwall Two Types
Normal faultReverse fault
TWO TYPES OF FAULTS Normal fault
Tension Pull Rocks Apart
Reverse FaultsCompression that
pushes rocks together
TELLING THE DIFFERENCE BETWEEN FAULTS Look at the order
of sedimentary rock layers
Compare the two dark layers
STRIKE-SLIP FAULTS Third Type of
Fault Opposing forces
cause rock to break and move horizontally
Move left or right San Andreas
Fault
PLATE TECTONICS AND MOUNTAIN BUILDING Plates Collide
Land features start as…
Can become …Mountains existAndes MountainsCompression or
tension
THREE DIFFERENT KINDS OF MOUNTAINS
Folded Mountains Highest Convergent (collide) Appalachian Mtns.
Fault-Block Mountains Tension Drop Down Tilted up
Volcanic Mountains Major (Convergent) Sinks Islands Ring of Fire
UPLIFT AND SUBSIDENCE Vertical
MovementsUplift
Higher elevations May or May Not Be
DeformedSubsidence
Sinking No Deformation
UPLIFT AND SIBSIDENCE Uplifting of
Depressed Rock Formation of Mtns. Without Deformation
Rebound Weight removed
Subsidence of Cooler Rock Hot More Space Less Volume (Subsides)
Tectonic Letdown Stretched rift zones Stress