Podcast
Questions and Answers
What are the two important layers of the Earth for volcano formation?
What are the two important layers of the Earth for volcano formation?
- Mantle and Outer Core
- Lithosphere and Asthenosphere
- Crust and Mantle (correct)
- Core and Crust
What happens when a volcano erupts?
What happens when a volcano erupts?
- The Earth’s surface cracks and splits open.
- Lava cools down and solidifies under the Earth’s surface.
- The magma chamber empties out completely.
- Magma rises through cracks and spills out unto the Earth’s surface as lava. (correct)
What is the crack in a volcano called?
What is the crack in a volcano called?
- Vent
- Crater
- Fissure (correct)
- Fault
What is a characteristic of Shield Volcanoes?
What is a characteristic of Shield Volcanoes?
What is the purpose of the Vent in a volcano?
What is the purpose of the Vent in a volcano?
What can increase the pressure in the magma chamber?
What can increase the pressure in the magma chamber?
What is the temperature that lava from a volcano can reach?
What is the temperature that lava from a volcano can reach?
What are the three types of volcanoes?
What are the three types of volcanoes?
Which type of volcano is common?
Which type of volcano is common?
Which of the following is an extinct volcano?
Which of the following is an extinct volcano?
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Study Notes
Volcano Formation
- The two important layers of the Earth for volcano formation are the mantle and the crust.
Volcano Eruption
- A volcano erupts when magma rises through cracks and spills out onto the Earth's surface as lava.
Volcano Formation Process
- A volcano is formed when magma from the Earth's interior rises through cracks in the Earth's crust, solidifies, and accumulates, resulting in a volcanic cone.
Volcano Structure
- A volcano has several key parts, including the vent (where ash, gas, and lava escape), magma chamber (where magma accumulates), crater (the depression at the top of the volcano), and cone (the outer shape of the volcano).
Types of Volcanoes
- There are three types of volcanoes: composite, shield, and cinder cone.
- Composite volcanoes are tall and conical, and typically have violent eruptions.
- Shield volcanoes are gently sloping and typically have non-violent eruptions.
Volcano Characteristics
- Lava from a volcano can reach temperatures of up to 3210°C.
- Magma can increase the pressure in the magma chamber, leading to a volcanic eruption.
- The vent is where ash, gas, and lava escape from the volcano during an eruption.
Plate Tectonics
- Destructive plate boundaries are where one plate is being subducted (pushed) under another plate, resulting in volcanic activity.
- Constructive plate boundaries are where two plates are moving apart, resulting in volcanic activity.
Volcanic Hotspots
- Hawaii is an example of a volcanic hotspot, where magma rises from the Earth's mantle to the surface, creating a chain of volcanoes.
True or False
- When volcanoes erupt violently, this can cause the top of the volcano to blow out. (True)
- Composite volcanoes do not have steep sides and usually have violent eruptions. (False, composite volcanoes have steep sides and violent eruptions)
- Shield volcanoes are steep and violent. (False, shield volcanoes are gently sloping and typically have non-violent eruptions)
Multiple Choice
- An extinct volcano is Ben Nevis in Scotland.
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