Vocab 1
Vocab 2
Techtonic Plates
Layers of the Earth
Volcanos
100

Any place where gas, ash, or melted rock comes out of the ground.

Volcano

100

Melted rock, less dense than solid rock so it rises up to the service

Magma

100

The three types of plate boundaries

Divergent, convergent, transform

100

The thinnest layer of the earth

Crust

100

The subduction zones that occur around the pacific ocean

Ring of Fire

200

A Volcano in which an eruption has not occurred in a long period of time.

Dormant Volcano

200

Magma that has reached the service of the Earth

Lava

200

The type of boundary occurs when two plates are moving away from one another

Divergent

200

Earth’s Physical Layers

  • Lithosphere

  • Asthenosphere

  • Mesosphere

  • Outer Core

  • Inner Core

200

Warning signs of a volcanic eruption

Earthquakes

Changes in the tilt of the ground

rising temperatures of openings

changes in volcanic gases being tested

300

the resistance of liquid material, such as lava, to flow.

Viscosity

300

Hot ash and bits of rock.

Pyroclastic materials

300

The type of plate boundary that has two plates moving parallel to one another in opposite directions

Transform

300

A layer of weak or soft mantle that is made of rock that flows slowly. Tectonic plates move on top of this layer

Asthenosphere

300

A volcano that has collapsed in on itself

Caldera

400

Volcano’s with alternating layers of hardened lava flows and pyroclastic material. These volcanoes are generally large and steep volcano mountains.

Composite Volcano

400

Volcanoes with a broad base and gently sloping sides. They cover a wide area and generally form from mild eruptions. Layers of lava flow out from the vent, harden, and slowly build up to form the cone. Example - Hawaiian Islands

Shield Volcanoes

400

The type of plate boundary that has two plates moving towards one another

Convergent

400

The strong, lower part of the mantle

Mesosphere

400

Quiet eruptions typically result in this magma type

Balastic

500

A location where a column of extremely hot mantle rock, called a mantle plume, rises through the asthenosphere. As the hot rock reaches the base of the lithosphere, it melts partially to form magma that can rise to the surface and form a volcano.

Hot Spots

500

Volcanoes with alternating layers of hardened lava flows and pyroclastic material. These volcanoes are generally large and steep volcano mountains.

Composite Volcano

500
Continent-Ociencic Crust Collision, when one plate goes underneath the other

Subduction

500

The movement of matter that results from differences in density is caused by variations in temperature. In the mantle, this takes place when cooler rock sinks and warmer rocks rise.

Convection

500

a fast-moving mixture of water, gases, and ash

pyroclastic flow

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