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13-2 Notes There are 2 main types of magma. They are: 1. Mafic 2. Felsic Composition Color Make up Viscosity Texture Gases Produces Magnesium and Iron Feldspar and Silica Dark in Color Light in Color Oceanic Crust Continental Crust Low Viscosity High Viscosity Runny Lava Sticky Lava Easily Escapes Trapped: Water Vapor and Carbon Dioxide Quiet Eruption Explosive Eruptions sending molten and solid particles shooting into the air. Examples Lava Flow, Hawaii Pahoehoe Aa Pyroclastic Material Volcanic dust < 0.25mm Volcanic Ash < 2mm Lapilli or “Little Stones”< 64mm Volcanic Bombs = BIG Volcanic Blocks = BIGGER 3 main types of volcanoes: 1) Shield 2) Cinder Cone Slope Area Covered Type of eruption Layers Gently sloping sides Steep, close to 40o Not as steep as cinder cones Wide area Quiet eruption Mafic lava Smaller area explosive Pyroclastic material 3)Composite Larger than a Quiet and Mafic lava and cinder cone explosive Pyroclastic eruptions material Craters: The funnel-shaped pit at the top of a volcanic vent is known as a crater. Calderas: When the magma chamber below a volcano empties, the volcanic cone may collapse and leave a large, basin-shaped depression called a caldera. Predicting: Warning signals of volcanic eruptions: 1. An increase in the strength and frequency of earthquakes. 2. Temperature changes within the rock. 3. Fracturing of the rock around a volcano. Links: Pahoehoe Lava Flow: http://www.youtube.com/watch?v=HURs_JxnKdg&NR=1 http://www.youtube.com/watch?v=qiVVvQ9SVfc&feature=relate d http://www.youtube.com/watch?v=xsJn8izcKtg&feature=related http://www.youtube.com/watch?v=Ff9DpZIDWFs&NR=1 Aa Lava Flow: http://www.youtube.com/watch?v=iyIV5fd1Aww Felsic Eruption: http://www.youtube.com/watch?v=vBJ9xZws7ro&feature=PlayLis t&p=C4472E8C9A54D3CD&index=14 http://www.youtube.com/watch?v=I07WBMUH7Ns&feature=relat ed