Chapter 5 Flashcards
Volcanic Eruptions
Lava flows
molten rock that flows across the ground
Pyroclastic debris
solid fragments ejected during eruptions (ash, pumice, volcanic bombs)
Volcanic gases
gases such as water vapor, CO₂, and sulfur compounds released from magma.
pyroclastic flow
fast-moving avalanche of hot ash, gas, and volcanic material
lahar
a volcanic mudflow composed of water and volcanic ash/debris that moves down volcanic slopes, often triggered by heavy rain or melting snow.
Shield volcanoes
have broad, gentle slopes from low-viscosity basaltic lava flows
Stratovolcanoes
are steep and layered due to alternating lava flows and pyroclastic eruptions, often from more viscous andesitic or rhyolitic lava.
Cinder cones
small, steep hills of pyroclastic fragments, formed from gas-rich basaltic lava that erupts explosively.
Why do some volcanic eruptions consist mostly of lava flows, while others are explosive and do not produce flows?
Eruptions depend on magma viscosity and gas content. Low-viscosity, gas-poor basaltic magma results in gentle lava flows, while high-viscosity, gas-rich magma traps gas and pressure, leading to explosive eruptions with pyroclastic material.
What processes may lead to hot-spot eruptions?
Hot-spot eruptions are caused by mantle plumes, which are columns of hot material rising from deep within the mantle. These plumes create melting in the lithosphere as they reach shallow depths, leading to volcanic activity independent of tectonic boundaries.
How do continental-rift eruptions form flood basalts?
In continental rift settings, decompression melting of the mantle produces large volumes of basaltic magma. This magma can erupt through fissures, spreading out as vast, flat lava flows, forming extensive flood basalts.
island arc
a chain of volcanic islands formed above a subducting oceanic plate at an ocean-ocean convergent boundary
continental arc
forms along the edge of a continent above a subducting oceanic plate at an ocean-continent convergent boundary.
Identify some of the major volcanic hazards, and explain how they develop.
Lava flows can destroy property; pyroclastic flows and ash falls pose severe hazards to life, air quality, and buildings; lahars can bury settlements; volcanic gases can cause respiratory problems; volcanic tsunamis may occur if an eruption disturbs bodies of water.
How do geologists predict volcanic eruptions?
Geologists monitor earthquakes, gas emissions, ground deformation, and temperature changes around a volcano. Increased seismic activity or gas release often precedes eruptions, helping predict potential activity.
Explain how steps can be taken to protect people from the effects of eruptions.
Evacuation plans, hazard mapping, early warning systems, and exclusion zones around volcanoes can minimize risk. Public education and communication also ensure people know evacuation procedures and danger areas.
Accretionary Lapilli
Small, spherical pellets of volcanic ash that form when wet ash particles clump together as they fall during an eruption.
Active Volcano
A volcano that is currently erupting, showing signs of erupting soon, or has erupted in recent history.
Ash
Fine-grained volcanic material, smaller than 2 mm, expelled during explosive eruptions that can travel great distances.
Block
Large, angular fragments of solid rock ejected during a volcanic eruption, often originating from the volcano’s vent or walls.
Blocky Lava
Lava with a rough, jagged surface, formed when highly viscous lava cools and breaks into angular blocks as it flows.
Bomb
Large, rounded fragments of lava ejected during an explosive eruption, which cool in flight and take on aerodynamic shapes.