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Seafloor spreading-Process
Magma rises at mid-ocean ridges, cools to form new oceanic crust, and pushes older crust away
Seafloor spreading-Features
Mid-ocean ridges, rift valleys, symmetrical magnetic stripes
what causes Seafloor spreading
Convection currents in the mantle
Seafloor spreading- results
Creation of a new ocean floor.
Convection currents
Heat from earth’s core causes mantle material to raise and fall
Ridge push
Gravity pushes newly formed crust away from mid-ocean ridges
Slab pull
Sinking of a cold,dense plate pulls the rest of the plate along
Oceanic Plates
Thinner,denser,basalt composition
Continental plate
Thicker,Less dense,Granite composition
Folds
Anticline: Upward arch. Syncline: Downward trough
Faults
Normal Fault: Caused by tension, hanging wall moves down.
Reverse Fault: Caused by compression, hanging wall moves up. Strike-Slip Fault: Caused by shearing, horizontal movement.
Appalachian Mountains
Formed by continental convergence
What are volcanoes
openings in the earth’s crust where magma escapes
Where are volcanoes
Plate bounderies
Warning signs for a volcano
Earthquakes,Gas emissions and ground deformation
Dangers of volcanoes
Lave flows,ash clouds,mass movement.
Magma
Molten rock beneath earth’s surface
Lava
Magma that has reached the surface
P waves
Primary,fastest,travel through solids and liquids
S waves
Secondary,slower,travel only through solids
Which waves cause more damage?
S waves cause more ground shaking
Ring of fire
A horseshoe-shaped zone around the Pacific ocean with frequent earthquakes and volcanic activity.
What are earthquakes
Sudden releases of energy due to fault movement
Where are earthquakes
plate boundaries,especially transform and convergent
What damage can earthquakes cause
Ground shaking,surface rupture and tsunamis
Subduction definition
One tectonic plate sinks beneath another
Where is subduction located
Convergent boundaries
How are hot spots formed
Plumes of hot mantle material rise and melt through the crust
What are the results of hot spots
Volcanic islands like chains of extinct volcanoes as plates move over the hot spot