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How do volcanoes form and what affect do they have on the Earth? Along Above subduction zones Magma forced upwards and forms volcanoes on surface Ring of Fire in Pacific Ocean Mediterranean belt – Mt. Vesuvius Along convergent boundaries: divergent boundaries: At mid-ocean ridges Magma fills in gaps Iceland – Mid-Atlantic Ridge Hot Spots are unusually hot regions of Earth’s mantle where plumes of magma rise to surface Located away from plate boundaries Example: Hawaii Active Erupts Regularly Lifetime can span months to millions of years Can be currently erupting or showing signs of unrest (earthquakes, emitting gas) Ex: Mt. St. Helens Extinct Unlikely to erupt again No magma/lava supply Ex: Hawaiian Islands not over hot spot Dormant Erupted in past but is now quiet Can be very dangerous It is very difficult to determine status of volcanoes Volcanoes emit water vapor, carbon dioxide, and sulfur dioxide into the air Gases are suspended in atmosphere and block radiation from sun Global temperatures can be affected Health issues for humans (Respiratory) Pyroclastic flows, tephra, lahars (hot mud flow) Volcanologists study deposits left from previous eruptions Warning Signs: earthquakes activity and gas emissions Seismometers measure EQs and correlation spectrometers measure SO2 levels Structural support – walls, supportive buildings Evacuation procedures Communication between scientists and public Volcanoes may have been present in the history of other planets Mars, Venus Volcanoes are active on Jupiter's moon, Io