Divergent Plate Boundaries

Froggy Jumps

(11)

Mid Atlantic Ridge and the formation of new ocean floor.

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geology

k13

divergent boundaries

Edad recomendada: 13 años

190 veces realizada

Creada por

Jaime Tres

Estados Unidos

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Froggy Jumps Divergent Plate BoundariesVersión en línea Mid Atlantic Ridge and the formation of new ocean floor. por Jaime Tres 1 land mass above sea level. a continent b rift c mountain 2 the process that causes continental crust to pull apart, breaking it into blocks. a evaporation b volcanoes c continental rifting 3 the crust that makes up the continents; thicker and less dense than oceanic crust. a mid Atlantic ridge b continental boundary c continental crust 4 ground shaking caused by the release of energy stored in the crust. a magma b earthquakes c lava 5 molten rock deep inside the Earth. a volcano b magma c lava 6 the mechanism for moving continents; the formation of new seafloor at spreading ridges pushes lithospheric plates on the Earth's surface. a seafloor spreading b earthquakes c tornadoes 7 the crust that underlies the oceans; thinner and denser than continental crust. a continental crust b oceanic crust c ridge 8 molten rock that has reached the Earth's surface. a Lava b magma c gasser 9 a divergent plate boundary that breaks up a continent. a Pacific Ring of Fire b continental rift c Mid Atlantic Ridge 10 a location where two lithospheric plates spread apart. a transverse plate boundary b divergent plate boundary c convergent plate boundary 11 a large, continuous mountain range found within an ocean basin; it is the location on the seafloor where magma upwells and forms new seafloor. a The Alps b Sierra Nevada c mid-ocean ridge

Froggy Jumps

Divergent Plate BoundariesVersión en línea

Mid Atlantic Ridge and the formation of new ocean floor.

por Jaime Tres

land mass above sea level.

continent

rift

mountain

the process that causes continental crust to pull apart, breaking it into blocks.

evaporation

volcanoes

continental rifting

the crust that makes up the continents; thicker and less dense than oceanic crust.

mid Atlantic ridge

continental boundary

continental crust

ground shaking caused by the release of energy stored in the crust.

magma

earthquakes

lava

molten rock deep inside the Earth.

volcano

magma

lava

the mechanism for moving continents; the formation of new seafloor at spreading ridges pushes lithospheric plates on the Earth's surface.

seafloor spreading

earthquakes

tornadoes

the crust that underlies the oceans; thinner and denser than continental crust.

continental crust

oceanic crust

ridge

molten rock that has reached the Earth's surface.

Lava

magma

gasser

a divergent plate boundary that breaks up a continent.

Pacific Ring of Fire

continental rift

Mid Atlantic Ridge

a location where two lithospheric plates spread apart.

transverse plate boundary

divergent plate boundary

convergent plate boundary

a large, continuous mountain range found within an ocean basin; it is the location on the seafloor where magma upwells and forms new seafloor.

The Alps

Sierra Nevada

mid-ocean ridge

Divergent Plate Boundaries

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Divergent Plate Boundaries

Froggy Jumps

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Froggy Jumps

Divergent Plate BoundariesVersión en línea

por Jaime Tres

land mass above sea level.

the process that causes continental crust to pull apart, breaking it into blocks.

the crust that makes up the continents; thicker and less dense than oceanic crust.

ground shaking caused by the release of energy stored in the crust.

molten rock deep inside the Earth.

the mechanism for moving continents; the formation of new seafloor at spreading ridges pushes lithospheric plates on the Earth's surface.

the crust that underlies the oceans; thinner and denser than continental crust.

molten rock that has reached the Earth's surface.

a divergent plate boundary that breaks up a continent.

a location where two lithospheric plates spread apart.

a large, continuous mountain range found within an ocean basin; it is the location on the seafloor where magma upwells and forms new seafloor.