Volcanic Hazards Flashcards
Constructive margins
Basaltic lava is formed here-very hot and has a low viscosity(runny). Eruptions of basaltic lava are frequent and go on for a long time.
Destructive Margins
Acidic lavas are formed here- they are cooler and more viscous(less runny), so flow less easily. Acidic lavas usually erupt every once in a while and are short lived
Because the lava is viscous, it forms blockages in volcanic vents, causing pressure to build. The blockage is cleared by a iolent eruption
Pyroclastic Flows
is a mixture of super heated gas, ash and volcanic rock that flows down the sides of a volcano. Travels high speeds(more than 80km/h) and flow long way(10-15km)
Volcanic Gases
Lava contains gases such as carbon dioxide and sulfur dioxide, which are released into the atmosphere when a volcano erupts.
Harmful if breathed in
Pyroclastic and Ash fallout
is material that has been ejected from a volcano during an eruption
Fallout consists of material of a range of sizes, from large pieces of rock weighing several tonnes to microscopic ash particles. Can travel thousands of kilometres from the volcano
Fine material can form a layer up to several metres in thickness.
Mudflows(lahars)
Occur when volcanic material mixes with large amounts of water(from rainfall or from ice melted by eruption).Flows move very quickly(over 80km/h) can travel tens of kilometres.
Acid Rain
Volcanic gases can react with water vapour in the atmosphere, which then falls as acid rain
Primary Impacts
Direct results of the eruption(people can be killed by falling tephra)