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Earth Science

Unit 6 Plate Tectonics

QuestionAnswer
Continental Drift the theory that all of the continents were once joined together in a single landmass and have since drifted apart.
Pangaea “all Earth” or name given to the super continent that existed 200 million years ago.
Plate Tectonics the study of the formation and movements of plates
Plates section of the lithosphere that moves around.
Lithosphere Earth’s solid outer crust
Asthenosphere partially melted layer that flows slowly and is located below the lithosphere.
Convection Currents the driving force of- plate movement -Magma heats up causing it to expand and rise. -Magma cools down causing it to contract and sink -The plates (solid lithosphere) are moving on top of the asthenosphere (liquid magma) due to density differences.
Ring of Fire isolated belt around the Pacific Ocean where 90% of the world’s volcanoes exist
Earthquake Evidence -Scientist noticed that earthquakes do not occur at random location, but run throughout the world along isolated belts -When plotted on a map they outline the plate boundaries
Volcanic Evidence Occurs at plate boundaries where plates are interacting
Rock Evidence -Sedimentary deposits and igneous lava flows are usually placed down in horizontal layers -Sometimes movement along boundaries causes these layer to tilt or fold
Mountain Evidence -As plates collide, they sometimes are pushed upward -Fossilized marine organisms can be found at these high altitudes in the rock
Types of plate boundaries Divergent Transform Convergent
Convergent Boundary boundary where two lithospheric plates are coming together -Example: the India Plate pushing upward into Eurasian Plate and creating the Himalayan Mountains
Subduction the process where one plate is pushed below another and consumed in the mantle -Example: the Nazca Plate being consumed under the South American Plate
Three Types of Convergent Boundaries: Ocean - Ocean Boundary Ocean - Continental Boundary Continental - Continental Boundary
Divergent Boundary Divergent Boundary - boundary where two lithospheric plates are moving apart Example: part of the Mid-Atlantic Ridge emerges from the ocean and splits Iceland in half
Sea-Floor Spreading the process where ocean floor is extended when two plates move apart
Mid-Ocean Ridge underwater mountain range created from a divergent plate boundary
Mid-Atlantic Ridge a mid-ocean ridge that runs the length of the Atlantic Ocean Separates the North and South American Plates from the Eurasian and African Plates
Rift Valley long narrow valley that runs the entire length of a mid-ocean ridge system
Transform Boundary boundary where two lithospheric plates are sliding past one another Example: the San Andreas Fault is 800 km long and runs throughout California
Lithosphere Earth’s crust and outer most layer
Continental Crust thickest (100 km) and least dense (2.7 g/cm3) part of the lithosphere
Oceanic Crust - thinnest (2-3 km) and most dense part of the lithosphere (3.0 g/cm3)
MOHO thin interface separating the lithosphere from the asthenosphere
Asthenosphere a partially melted layer that allows for parts of the lithosphere to move
Mantle thickest part of Earth (80%) and is between the crust and the outer core
Outer Core liquid layer of Earth’s interior between the mantles and the inner core
Inner Core - the solid inner most zone of Earth’s core composed of iron (Fe) and nickel (Ni)
Earthquake a natural shaking of the lithosphere caused by a release of energy stored in rocks
Epicenter the location on Earth’s surface directly above the focus
Focus the point inside the Earth where the earthquake originates
Seismometer an instrument used to measure and record movements in the ground
Seismogram record of the seismometer
Mercalli Scale scale that measures the intensity of an earthquake based on the effects to Earth’s surface, humans, objects in nature, and other man-made structures
Richter Scale logarithmic scale that measures the amount of energy released during an earthquake
Magnitude a number to quantify the amount of seismic energy released from an earthquake
Primary Wave (P-wave) -are the fastest waves -Travels through solids, liquids, and gases
Compressional particles travel in the direction of wave movement
Secondary Wave - the slower wave -Travels through solids only
Shadow Zone area in which seismic waves are not detected due to the liquid outer core
P-waves are refracted when they reach the liquid outer core
S-waves are absorbed when they reach the outer core and are not transmitted through to the other side
hot spot thinner portions of the crust where rising convection currents bring magma to the surface.
Created by: user-1746037
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