Volcanic Hazards Flashcards
Vulcanicity
Vulcanicity refers to all volcanic activities related to magma being forced into the crust.
Volcanoes
Volcanoes are openings in the Earth’s crust through which lava, ash and gases erupt. They mark the presence of magma within the Earth’s crust.
Magma
Molten rock beneath the surface is referred to as magma, but once it is ejected at the surface it is called lava.
Where do volcanic hazards occur
Mostly near constructive and destructive plate margins
Effect of constructive margins on volcanic eruptions and landforms
Basaltic lava
Runny, less viscous, low in silica
Regular and continuous eruption
Mainly lava
Volcano type: Lava plateau, shield volcano, lava
Effect of destructive margin on volcanic eruption and landform
Andesitic lava
Slow flowing, viscous, high in silica
Long dormant periods: less frequent
Tephra, pyroclastic flow, ash, gases
Volcano type: acid lava dome, composite cone, layers of ash and lava
Lava flow
Lava can flow from volcanic vent down the side of a volcano
Speed and distance travelled depends on viscosity, temperature and slope steepness:
Basaltic, low viscosity, low silica, high temp can flow some distance before solidifying
Acidic, high viscosity, high silica, low temp flows slower and may solidify in vent - results in explosive unpredictable eruptions.
Most relatively slow - people can evacuate
Destroys anything in its path - burning, knocking down, burying
Pyroclastic flow
A mix of ash, gases, lava and hot rock rising from eruption and moves at rapid speeds (up to 80km/h) and flows a long way.
Travel fast and happen with little warning so can cause widespread destruction and death.
Common in eruptions of acidic lava at subduction zones.
Tephra
Solid rock fragments ejected during volcanic eruptions
Volcanic gases
Lava contains gases such as c02 and sulfur dioxide which are released into atmosphere during eruption.
Highly dangerous - if breathed in
Nuées ardentes
Means ‘glowing cloud’ and is a dense, rapidly moving cloud of hot gases, ashes and lava fragments from a volcanic eruption. It is a type of pyroclastic flow that contains more dense material and so doesn’t travel as far.
Ash fallout
Ash can be ejected high into the atmosphere and, depending on prevailing winds, can cover a large area
Range of sizes - larger, heavier particles deposited near volcano and lighter further away
Mudflows (Lahars)
Lahars are destructive mudflows formed when ash and other volcanic material are mixed with water. They flow at speeds of up to 60km/h and are highly erosive.
Acid rain
Volcanic gases can react with water vapour in atmosphere and then fall as acid rain
Can damage ecosystems
What is magnitude ?
Volcanic events range from small, slow lava to huge eruptions. Magnitude can be measured using Volcanic Explosivity Index, which grades volcanoes on a scale based on amount of material ejected and how high it is blasted.