Earthquake and Volcanic Hazards
Volcanic Hazards
Volcanic hazards are primarily found at constructive and destructive plate boundaries and near hot spots but not at conservative plate margins or collision zones. The fundamental cause of these hazards is the expulsion of magma from beneath the Earth’s crust to the surface. The type of eruption differs by location: at constructive margins, where magma rises, the lava is typically hotter and more fluid, resulting in less violent eruptions. Conversely, at destructive margins, the more acidic and viscous lava tends to create more violent eruptions, including pyroclastic flows and lava flows, potentially contributing to acid rain and climate alteration due to the greater volume of material released into the atmosphere. Lahars, or volcanic mudflows, can form when volcanic ash combines with water. Though relatively slow-moving, hot spot lava flows, such as those in Hawaii, can still incinerate structures and vegetation. It’s important to note that volcanic hazards become a concern when they threaten human populations. The severity of the impact from primary and secondary volcanic hazards is contingent upon the eruption’s magnitude and the proximity of populations at risk.
- Primary Hazard
- Lava flow
Ash
Pyroclastic flows
Gass emissions
- Secondary Hazard
- Lahars (volcanic mudflows)
Acidification
Landslides
Climate change (cooling)
Fire
Earthquake Hazards
Earthquakes frequently happen along the boundaries where tectonic plates meet. As these plates shift in diverse directions, stress accumulates. When this stress is suddenly released, it causes the ground to shake—an event known as an earthquake. Additionally, certain earthquakes can be induced by human actions, including mining operations, the construction of substantial dams, and the underground detonation of explosives.
- Primary Hazard
- Ground shaking
Liquefaction
- Secondary Hazard
- Gas leaks
Fires
Landslides
Debris flow and mudflow
Tsunamis
Summary
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