introduction volcano, mountain or hill formed by the accumulation of materials erupted through one...
TRANSCRIPT
Introduction
• Volcano, mountain or hill formed by the accumulation of materials erupted through one or more openings (called volcanic vents) in the earth's surface.
• They are usually found along diverging plate or constructive plate.
Introduction
• Volcanoes are active, dormant or extinct.
• There are 3 types of volcanoes: composite, cinder and shield.
– Lava Basic or acidic lava– Gas Carbon Dioxide, Sulphur dioxide
– Pyroclasts Ash, dust, volcanic bombs
Eruptive Styles
Composition • Silica Content- Amount of SiO2 that lava contains
– The higher the amount of SiO2 the more explosive the eruption
• Gas & Water Content-Amount of volatiles (C02, Water, Sulfur, etc) – The higher the amount of volatiles dissolved in magma the more
explosive the eruption
ViscosityMeasure of how easily material can flow; Low viscosity, lava
flows easily; high viscosity, it does not; The more viscous the lava the more explosive the eruption
LavaType Acid Lava Basic Lava
Production Subduction Constructive Plate
Content Rich in silica Rich in iron and magnesium
Temperature 8000C 12000C
Type Viscous Fluid
Movement Slowly Quickly
Time taken to cool
Cools, solidifies quickly
Cools, solidifies slowly
Distance Does not flow far Flows very far
Explosion Violent Quiet
Formation of Volcano
• Formed along along diverging plate or constructive plate.
• Magma rises from the mantle through fractures due to the immense gas pressure in the magma chamber.
• Volcanic material spills or shots out from the vent and piles up on the ground around the vent.
• Forms a volcano.• Volcano can be formed through hot spots.
Composite Volcano
• Alternate layers of pyroclasts• Steep slopes and gentle base due to larger
pyroclasts fall near the summit while the finer pyroclasts fall near the base
• Acid lava solidifies in the central pipe build up tremendous pressure loud explosions
• Examples: Mt Merapi, Mt Mayon, Mt Fuji, Mt St Helens
• Also known as StratoVolcano
Ash and Cinder Volcano
• Steep sided symmetrical volcano form from red-hot cinders and ash.
• Steep slopes and gentle base due to larger pyroclasts fall near the summit while the finer pyroclasts fall near the base
• Bowl-shaped summit crater
• Grows rapidly and found in groups
• Examples: Paricutin
Shield Volcano
• Slightly domed shaped volcano
• Fluid basic lava
• Wide base
• Not explosive
• Little pyroclasts
• Example: Mauna Loa that is formed form hot spot
Hot Spots
• Rising columns of or plumes of magma that originate form a fixed position
• Magma plume melts a hole in the lithospheric plate
• Magma issues out from the vent
• As plates move, the volcano becomes extinct and anew volcano is formed
• The further the volcano is from the hot spot, the older it is.
Eruption of Kilauea crater spilled molten lava down the flanks of Mauna Loa volcano in Hawaii Volcanoes National Park