Chapter 8 Volcanoes Volcanic Eruptions Section 1
Nonexplosive Eruptions Volcanoes with Lava flows
Explosive Eruptions Clouds of hot debris and gases shoot out from the volcanoes
Magma Hot liquid material volcanoes are created in
Vents Holes in the Earth’s crust that magma rises through
Lava Magma that erupts onto the Earth’s surface
Pyroclastic Material Magma & fragments of rock that are blasted into the air during violent earthquake eruptions
Volcano A vent or group of vents combined with a buildup of lava or pyroclastic material
Magma - High Water Content Explosive volcanoes with high water content
Magma - Silica Magma that contains a large percentage of Silica
Blocky Lava Cool stiff lava that cannot travel far from the erupting vent
Pahoehoe Lava that flows like wax dripping from a candle
Aa Lava that has a jagged surface
Pillow Lava Lava that erupts underwater
Volcanic Blocks Largest pieces of pyroclastic material
Volcanic Bombs Large blobs of magma that harden in the air
Lapilli “Little stones” pebble-like bits of pyroclastic material
Volcanic Ash Particles that are less than 2 mm in diameter
Chapter 8 Volcanoes Volcanoes’ Effects on Earth Section 2
Volcanic Flows Clouds of hot ash that flow rapidly downhill like an avalanche
Volcanic Fallout As volcanic ash falls to the ground effects may be devastating
Climatic Fluctuation Ash & gases spread around the globe & block out the sun
Shield Volcanoes Layers of lava from repeated non explosive eruptions
Cinder cone volcanoes Small volcanic cones made entirely of pyroclastic material from moderately explosive eruptions
Composite Volcanoes Explosive eruptions of pyroclastic material
Crater Funnel shaped pit at the top of the central vent
Caldera Magma chamber volcanoes empties & roof collapses
Chapter 8 Volcanoes What causes Volcanoes? Section 2
Formation of Magma Magma forms below the Earth’s surface in a region that includes the lower crust & the upper mantle
Where Volcanoes Form Tectonic plate boundaries form “ring of fire”
Rift Deep crake forms between the plates
Hot Spots Tectonic plates that are directly above columns of rising magma

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