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Volcanoes Volcanoes and Plate tectonics Volcano is a mountain formed when layers of lava and volcanic ash erupt and build up Most are dormant About 600 are active What cause Volcanoes Magma is less dense then solid rock It slowly rises to the earths surface Flows out through an opening called a vent Lava cools quickly and forms igneous rock Opening at the top of the vent is called a crater Pyroclastic flow – massive avalanches of hot glowing rock and gases (complete destruction) Where do Volcanoes Form 1. Divergent Boundaries Mid Atlantic Ridge Forms long deep cracks called rifts where magma flows from 2. Convergent boundaries Cascade Mt. Range in Oregon and Washington Mt. Saint Helen Pacific Ring of Fire 3. Hot Spots Hawaiian Far Some Islands from the edge of any plate area of the mantle are hotter then others These hot spots melt rock which rise to the surface to form volcanoes Once the volcano rises above the water it becomes an island What determines how a volcano Erupts Composition of the magma plays a big role in determining the manner in how a volcano erupts Lave – more silica (silicon and oxygen) tend to be thicker and resists flow Lava containing more iron and magnesium and less silica tend to flow easier Amount of water vapor in lava influences how lava erupts More water (steam) the more pressure builds up and the more violent the eruption is Forms of Volcanoes Three basic volcanoes Shield volcanoes Cinder volcanoes Composite volcanoes 1. Shield Quiet eruption Broad volcanoes Gently sloping sides Ex. Hawaiian , rift zones like Iceland Cinder Cone Explosive Volcano Throws lava into the air, lava cools and hardens Tephra Forms – small- cinders , large – bombs steep sides Sunset crater Composite Volcano Can vary between quiet or violent Alternating layers of lava and tephra Convergent boundaries above subduction zone Mt. St. Helens Fissure Eruption Magma that is highly fluid can ooze from cracks or fissures in earths surface