Describe the three condition under which magma can form. Explain what volcanism is. Identify three tectonic settings where volcanoes form. Describe how magma can form plutons. The cause of many volcanic eruptions is the movement of tectonic plates › The movement of these plates is driven by Earth’s internal heat Mantle is mostly solid due to high pressure, even though high temps. › Solid mantle that melts and becomes liquid rock is known as magma. Can form under 3 conditions Temp of rock rises above melting pt. Pressure is reduce and melting pt. lowers Addition of fluids may decrease melting pt. of some minerals in the rock, causing rock to melt Fig 1, p. 319 Any activity that includes the movement of magma toward or onto Earth’s surface Bodies of magma rise to the surface in 2 ways › Magma is hot enough to melts surrounding rock › Magma rises, is forced into cracks, and causes large blocks to break off and melt. This adds to the magma body Lava – magma that flows onto Earth’s surface; the rock that forms when lava cools and solidifies › May flow out of a vent, cool, and build up a cone of material that may become a mountain. Volcano – a vent or fissure in Earth’s surface through which magma and gases are expelled Fig 2 – map of active volcano locations Most occur at or near both convergent and divergent plate boundaries Pacific Ocean – Ring of Fire › Also a major earthquake zone Area where one tectonic plate moves under another › Oceanic plates are more dense than continental plates are usually subducted › A deep trench forms on ocean floor along continent boundary › Continental plate forms Mtns as it is folded and pushed back › Subducted plate is melted to form magma › May form volcano chain › 2 oceanic plates – island arc may form Divergent plate boundaries – plates are pulling away › area where largest amount of magma rises to surface › Pillow lava › Fissures – cracks through which lava flows to Earth’s surface http://images.google.com/imgres?imgurl=http://oceanservice.noaa.gov/education/yos/multimedia/oceanexplor er.noaa.gov/oceanexplorer.noaa.gov/explorations/04fire/background/volcanism/pillow_lava_220.jpg&imgrefurl=h ttp://oceanservice.noaa.gov/education/yos/multimedia/oceanexplorer.noaa.gov/oceanexplorer.noaa.gov/expl orations/06fire/background/volcanism/volcanism.html&usg=__hXQKTNkmPcCI1nilHA5oK0I0iPs=&h=165&w=220&sz= 8&hl=en&start=5&tbnid=LW1Sb8d9jRnKM:&tbnh=80&tbnw=107&prev=/images%3Fq%3Dpillow%2Blava%26gbv%3D2%26hl%3Den A volcanically active area of Earth’s surface, commonly far from a tectonic plate boundary Mantle plumes – columns of hot, solid material rise and reach the lithospere › Appear to remain stationary, even though lithospheric plates drifs above the plumes. Theory that states hot spots result from cracks in Earth’s crust. Magma is not dense, therefore it rises through or intrudes the overlaying layer of rock. › Magma may fracture or melt the surrounding rock. › Rock that is melted may cool again into igneous rock. Magma may cool and solidify within the crust, resulting in many large plutons › Dikes – small plutons that are tabular in shape › Batholiths – large plutons that cover a lot of area