Lecture 1 - Volcanic Hazards Flashcards
Pyroclasts
All solid fragments ejected from volcanoes
Tephra
All pyroclasts that fall to the ground from eruption columns.
Monogenetic and Polygenetic
Volcanoes that erupt once and volcanoes that erupt many times
What forms explosive eruptions?
Large amounts of entrapped gases and high visocsity magma
What forms effusive eruptions?
Small amounts of entrapped gases and low viscosity magma
Why do we have volcanoes?
Primordial heat and radioactive decay of K, U and Th
Volcanism at divergent plate boundaries
- Along mid-ocean ridges
- 75% of annual output of magma on Earth
Volcanism at hotspots
Characteristics: Shallow slopes, Shield volcanoes
- Usually non-explosive
- Mostly basaltic lava flows
Iceland: Where hotspot and MOR meet
-Large volumes
- Low viscosity
- Hot 1200
- Fissure volcano type and usually non-explosive
Viscosity
High viscosity - slow-moving
Low viscosity - Fast moving
Basaltic Lava
- Most common rock type in the curst 2/3 surface
- Low silica content so low viscosity
A a lava
Eruption Temperature - 1000 - 1100°c
Rough lava
Pahoehoe Lava
Eruption Temperature - 1100 - 1200°c
Smooth lava with rolls
Characteristics of shield volcanoes
Low viscosity
Low silica magma
Gentle sloping flanks
Volcanic Explosivity Index
Describes the intensity of a volcanic eruption
An increase in number represents an increase around a factor of 10