Podcast
Questions and Answers
What happens when sulfur dioxide and nitrogen oxide released from volcanoes interact with water molecules in the air?
What happens when sulfur dioxide and nitrogen oxide released from volcanoes interact with water molecules in the air?
- It causes volcanic eruptions.
- It increases the amount of greenhouse gases in the atmosphere.
- It forms acid rain. (correct)
- It creates lahar mudflows.
What is the primary reason for the build-up of pressure that eventually leads to a violent volcanic eruption?
What is the primary reason for the build-up of pressure that eventually leads to a violent volcanic eruption?
- The difficulty of gases escaping thick, sticky magma. (correct)
- The accumulation of ash in the atmosphere.
- The slow release of volcanic gases.
- The rapid cooling of magma.
What is a lahar mudflow primarily composed of?
What is a lahar mudflow primarily composed of?
- Hot volcanic gas, ash, and fragmented rock.
- A mixture of tephra and water vapor.
- Hot volcanic material mixed with water. (correct)
- Molten rock, ash, and sulfur dioxide.
Which of these is NOT a direct consequence of volcanic eruptions?
Which of these is NOT a direct consequence of volcanic eruptions?
What is the primary characteristic of a pyroclastic flow that distinguishes it from other volcanic phenomena?
What is the primary characteristic of a pyroclastic flow that distinguishes it from other volcanic phenomena?
What is a fumarole primarily characterized by?
What is a fumarole primarily characterized by?
How do cracks and fissures on the surface of a volcano benefit scientists studying volcanoes?
How do cracks and fissures on the surface of a volcano benefit scientists studying volcanoes?
What differentiates tephra from other volcanic products?
What differentiates tephra from other volcanic products?
What is the primary factor that determines the speed at which lava travels outside the volcano?
What is the primary factor that determines the speed at which lava travels outside the volcano?
How do volcanic bombs contribute to the formation of volcanic landscapes?
How do volcanic bombs contribute to the formation of volcanic landscapes?
What is the main difference between a lava dome and a lava flow?
What is the main difference between a lava dome and a lava flow?
What is the significance of magma chambers in relation to volcanic eruptions?
What is the significance of magma chambers in relation to volcanic eruptions?
What is the primary cause of the formation of an eruption column?
What is the primary cause of the formation of an eruption column?
Which of the following is NOT a characteristic of volcanic ash?
Which of the following is NOT a characteristic of volcanic ash?
What is the primary difference between a volcanic vent and a volcanic opening?
What is the primary difference between a volcanic vent and a volcanic opening?
What is the smallest size for a volcanic bomb?
What is the smallest size for a volcanic bomb?
Flashcards
Magma
Magma
Molten rock beneath the Earth's surface that can form magma chambers.
Magma Chamber
Magma Chamber
An underground reservoir for magma, located 1 to 10 km below the surface.
Volcanic Vents
Volcanic Vents
Openings through which magma rises and erupts at the Earth's surface.
Lava
Lava
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Lava Flows
Lava Flows
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Volcanic Bombs
Volcanic Bombs
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Lava Domes
Lava Domes
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Eruption Column
Eruption Column
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Tephra
Tephra
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Pyroclastic Flow
Pyroclastic Flow
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Lahar Mudflows
Lahar Mudflows
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Acid Rain
Acid Rain
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Fumaroles
Fumaroles
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Volcanic Eruption
Volcanic Eruption
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Sulfur Dioxide
Sulfur Dioxide
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Cracks (Fissures)
Cracks (Fissures)
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Study Notes
Volcanic Parts and Processes
-
Magma Chambers:
- Reservoirs of molten rock located 1-10 km below the surface.
- Magma is lighter than surrounding rock, causing it to rise.
- Pressure buildup leads to volcanic eruptions.
-
Volcanic Vents:
- Openings or fissures that allow magma to reach the surface.
- Also known as volcanic openings.
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Lava:
- Magma that erupts onto the Earth's surface.
- Thin, runny lava allows gases to escape easily, producing lava flows.
- Different viscosity (thickness) creates various volcanic landforms.
-
Lava Flows:
- Molten rock oozing onto the surface after eruptions.
- Vary in temperature and viscosity, affecting volcanic landscape.
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Volcanic Bombs:
- Molten rocks ejected with force from volcanoes.
- Size is at least 66mm. Cool and solidify into diverse shapes after traveling significant distances.
- Contribute to volcanic landscapes.
-
Lava Domes:
- Geological features formed by accumulation of thick, sticky lava around vents.
- Potentially hazardous due to instability and explosive potential.
- Circular mounds protruding from volcanoes due to slow lava release.
-
Eruption Column:
- Towering plume of ash, gases, and other materials ejected into the atmosphere.
- Height can reach tens of miles.
- Impacts climate and aviation.
- Highly charged particles can generate thunder and lightning.
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Eruption Clouds:
- Billowing masses of gases, ash, and particles ejected in eruptions.
- create hazardous conditions.
- Ash falls like powdery snow, suffocating plants and animals.
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Tephra:
- Ejected fragments of volcanic material during explosive eruptions.
- Ranges from tiny ash particles to house-sized boulders.
- Highly destructive.
- Can range in size from tiny particles of ash to house-size boulders.
-
Acid Rain:
- Formed from sulfur dioxide and nitrogen oxides released by volcanic eruptions reacting with water.
- Impacts ecosystems, including water quality.
-
Lahars:
- Mudflows resulting from mixing of hot volcanic material with water.
- Can bury entire communities.
- Can devastate communities and ecosystems.
-
Pyroclastic Flows:
- Fast-moving mixtures of hot gas, ash, and fragmented rock.
- Travels down volcanic slopes at incredible speeds. Incorporates tephra.
- Created by collapses of lava domes.
- Significant threat to anything in its path.
-
Fumaroles:
- Vents where gases and steam escape from a volcano.
- Emit steam and gases like sulfur dioxide and carbon dioxide.
- Creates passageways for heat, gases, and magma.
- Create eerie landscapes.
-
Fissures/Fractures:
- Cracks on the surface caused by tectonic stresses. -Allow magma to rise and potentially cause eruptions.
- Act as windows for scientists to view gases inside volcanoes.
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