EXPLORATION: Earthquakes and Volcanoes
2. Volcanoes
Causes
Almost all volcanoes happen near plate divisions. 
- Destructive (violent) volcanoes usually happen near subducting plates. i.e. The Pacific Ring of Fire
 - Less violent volcanoes usually happen near diverging plates.
 
Watch the short video from National Geographic below. You will need to respond to this video in your learning guide. 
- Cinder Cone
- basaltic magma ejected under high pressure from a narrow neck cools to form cinder and ash which falls back down to build the sides of the cone
 - cone can build rapidly with steep sides i.e. 30 - 40 degree angle eg the volcano Paricutin in Mexico in 1943 grew 500 m in 8 months
 - if the narrow neck of the cone becomes plugged the volcano can explode violently
 

Photograph by J.P. Lockwood on December 1, 1975 (Courtesy: USGS) - Shield Cone e.g. Kilauea in Hawaii
- often formed from basalt lava which has a low viscosity allowing the lava to move for some distance forming a broad gently sloped volcano i.e. 10 -20 degree angle
 - less explosive tendency because the magma flows freely allowing the gases to escape
 

Photograph by M. Mangan on April 16, 1992 (Courtesy: USGS) - Composite Cone (or sometimes called Stratovolcanoes) e.g. Mt. St. Helens, Mt. Baker, Mt. Rainier, and Mt. Etna in Sicily
- consists of alternating layers of lava and ash
 - shallow slopes at bottom, steep at top, looks like a "normal" mountain in many ways.
 - lava layers permit the cone to attain considerable width while the cinder/ash layers encourage vertical growth
 - as a result, some of the world's highest volcanic mountains are in this category
 - can be very explosive spewing much material (i.e. cinders, ash, and 
rock fragments) high into the atmosphere and / or rapidly down the side 
of the volcano. Such a flow sears everything their path. 
 - mud flows, known as lahars, are frequently triggered as heat from the volcano melts snow and ice
 
Note: volcanoes often occur as "complexes" with different types of volcanoes together. Cinder cones often occur on the sides of shield or composite volcanoes.