Volcanoes from only at constructive and destructive plate boundaries
Nuees Ardentes (pyroclastic flows) are formed of hot gasses over 800 degrees and tephra (ash). After ejection from a volcano, they can flow down the side of a mountain at speeds of over 700km/h
Laval flows is when molten rock flows onto the surface. Acid lava solidifies very quickly but basic lava (basaltic) tends to flow some distance before solidifying.
Lahars occur when volcanic ash mixes with water (snow melt, heavy rainfall) flowing downhill. They are volcanic mudflows.
Magnitude is measured using the volcanic explosivity index (VEI) which is a logarithmic scale. Critics point out it doesn't take into account gas emissions.
Gases such as carbon dioxide, carbon monoxide, sulphur dioxide and chlorine can be emitted by a volcano. This can lead to acid rain
Tephra is the solid matter ejected by a volcano into the air. It ranges from volcanic bombs to ash.