The gases in
         the magma, and how slowly or quickly they are released contributes to how violently a volcano erupts.
Characteristics of Magma
•         high silica content 
–        produces light-colored
         lava that is too sticky to flow very far.
–       
         when cooled produces 
•        
         rhyolite (same composition as granite)
•         Obsidian (forms by cooling very quickly)
•         pumice (forms when
         gas bubbles are trapped in cooling lava, leaving spaces in the rock.)
•         Low silica produces free-flowing,
         dark-colored lava, forming basalt.
•        
         The type of magma influences how the volcano erupts (quiet or explosive).
–         Quiet
         Eruptions
•        
         Magma flows easily (low silica content)
•         Gas dissolved in the magma bubbles out gently.
•         Magma simply oozes
         from the vents
•        
         Produces …
–       
         Pahoehoe lava = fast moving, hot lava. Looks like a solid mass of wrinkles, billows, and ropelike coils.
–        Aa lava = cooler and slower
         moving. It forms a rough surface consisting of jagged lava chunks.
•         The type of magma influences how
         the volcano erupts (quiet or explosive).
–       
         Explosive eruptions
•        
         Thick and sticky magma plugs the vents.
•         Dissolved gases cannot escape from the magma,
         so pressure builds.
•        
         When the pressure of the gases become too great, the vents explode. 
•         The expanding gases
         push the magma out of the volcano with incredible force.
             
•         The type of magma
         influences how the volcano erupts (quiet or explosive).
–        Explosive eruptions
•         The explosion breaks
         the lava into fragments that quickly cool and harden into pieces of different sizes. 
–        Ash: fine rocky particles as small
         as a grain of sand.
–       
         Cinders: pebble-sized particles.
–        Bombs: baseball to car size 
–        Pyroclastic flow occurs
         when an explosive eruption hurls out ash, cinders, and bombs as well as gases. 
Identify some hazards of volcanoes.
•         Hazards
–        Different types of eruptions
         involve different volcano hazards, but both types can cause damage far from the crater’s rim.
•         Lava flow
•         Falling cinders
         and bombs
•        
         Volcanic ash
•        
         Landslides and avalanches
•        
         Mudflows
Identify
         types of volcanic activity other than eruptions.
•        
         Other Types of Volcanic Activity
–        hot springs
•         forms when groundwater
         is heated by a nearby body of magma.
•        
         rises to the surface and collects in a natural pool.
–        geyser 
•         a fountain of water
         and steam that erupts from the ground. 
–       
         Occurs when rising hot water and steam become trapped underground in a narrow crack.
–        Pressure builds until
         the mixture suddenly sprays above the surface.