There are two types of volcano:
Composite volcano
Shield volcano
Examples of composite volcanoes are Soufrière Hills, Montserrat and Mount Etna.
These occur in areas of destructive plate boundaries.
The eruptions are violent, ejecting thick and sticky lava.
Ash and lava are ejected into the air and descend as slow-flowing, thick lava. The process is then repeated, building up layers of ash and lava.
Pyroclastic flows (hot gas and ash) travelling more than 160 km per hour can flatten and burn everything in their path.
Lahars (melted ice or rain mixed with ash) can occur.
Thick layers of ash leave areas uninhabitable.
Examples of shield volcanoes are Iceland and Hawaii.
These occur in areas of constructive plate boundaries.
Widely, gentle-sloping volcanoes eject thin, runny lava.
The eruptions are not explosive and are less likely to result in loss of life.