Ch.3 Plate Tectonics

According to Wegener's hypothesis of continental drift,

• Earth's surface is made up of seven major landmasses

• the continents do not move

• Earth is slowly cooling and shrinking

• the continents were once joined together in a single landmass

What is Pangea?

• the name of a German scientist

• the name of the supercontinent that existed millions of years ago

• another name for continental drift

• the name of an ancient fossil

Tags

NGSS.MS-ESS1-4

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Any trace of an ancient organism that has been preserved in rock is called a

• landform

• continent

• fossil

• landmass

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What technology did scientists use in the mid-1900s to map the mid-ocean ridge?

• satellites

• deep-sea diving

• submarines

• sonar

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In sea-floor spreading, molten material rise from the mantle and erupts

• along the edges of all the continents

• along mid-ocean ridges

• in deep-ocean trenches

• at the north and south poles

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Old oceanic crust is more dense than new oceanic crust because it is

• hot

• moving toward a deep-ocean trench

• cool

• closer to the mid-ocean ridge

Tags

NGSS.MS-ESS2-3

Most geologist think that the movement of Earth's plates is caused by

• conduction

• earthquakes

• convection currents in the mantle

• Earth's magnetic field

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The geological theory that states that pieces of Earth's lithosphere are in constant, slow motion is the theory of

• subduction

• plate tectonics

• deep-ocean trenches

• sea-floor spreading

Tags

NGSS.MS-ESS2-3

A place where two plates slip past each other, moving in opposite directions, is known as a

• transform boundary

• divergent boundary

• convergent boundary

• rift valley

A collision between two pieces of continental crust at a converging boundary produces a

• mid-ocean ridge

• deep-ocean trench

• rift valley

• mountain range

Tags

NGSS.HS-ESS1-5

NGSS.HS-ESS2-1