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PRESENTATION ON VOLCANOS BY  ANJALI PATRA ANKITA TRIPATHY
Contents 1 Introduction 2 Plate tectonics and hotspots 3 Volcanic features 4 Erupted material 5 Volcanic activity 6 Notable volcanoes 7 Effects of volcanoes 8 Volcanoes on other planetary bodies 9 Panoramas
INTRODUCTION A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, ash and gases to escape from below the surface. The word volcano is derived from the name of Vulcano island off Sicily which in turn, was named after Vulcan, the Roman god of fire.  Volcanoes are generally found where tectonic plates are diverging or converging. Volcanoes can also form where there is stretching and thinning of the Earth's crust (called "non-hotspot intraplate volcanism"). Volcanoes can be caused by mantle plumes.   The study of volcanoes is called volcanology, sometimes spelled vulcanology.
Cleveland Volcano in the Aleutian Islands of Alaska photographed from the International Space Station, May 2006
Plate tectonics and hotspots Divergent plate boundaries  ,[object Object],[object Object],[object Object]
Hotspots ,[object Object],[object Object]
Volcanic features ,[object Object]
Other types of volcano include
Cryovolcanoes - ice volcanoes
Fissure vents - Flat, linear cracks through which lava emerges.
Shield volcanoes  - broad, shield-like profiles, are formed by the eruption of low-viscosity lava that can flow a great distance from a vent.,[object Object]
Cryptodomes -viscous lava forces its way up and causes a bulge, under great pressure.
Volcanic cones (cinder cones) -erupt mostly small pieces of scoria and pyroclastics.
Stratovolcanoes (composite volcanoes)  -made of cinders, ash and lava.
Supervolcanoes-a large caldera and can potentially produce devastation on an enormous, sometimes continental, scale. ,[object Object]
Subglacialvolcanoes-develop underneath icecaps, flat lava which flows at the top of extensive pillow lavas and palagonite.
Mud volcanoes-geo-excreted liquids and gases, although there are several different processes which may cause such activity. ,[object Object]
Erupted material Lava composition   Another way of classifying volcanoes is by the composition of material erupted (lava), since this affects the shape of the volcano. Lava can be broadly classified into 4 different compositions :- If the erupted magma contains a high percentage (>63%) of silica, the lava is called felsic. If the erupted magma contains 52–63% silica, the lava is of intermediate composition. If the erupted magma contains <52% and >45% silica, the lava is called mafic or basaltic. Some erupted magmas contain <=45% silica and produce ultramafic lava.
Lava texture   Two types of lava are named according to the surface texture: ʻAʻa (pronounced [ˈʔaʔa]) and pāhoehoe ([paːˈho.eˈho.e]).ʻAʻais characterized by a rough, clinkery surface and is the typical texture of viscous lava flow.Pāhoehoeis characterized by its smooth and often ropey or wrinkly surface and is generally formed from more fluid lava flows.
Volcanicactivity Scientific classification of volcanoes Philippine Institute of Volcanology and Seismology provides a scientific classification system for volcanoes. ,[object Object]
Potentially Active - Solfataras / Fumaroles - Geologically young (possibly erupted < 10,000 years and for calderas and large systems - possibly < 25,000 years). - Young-looking geomorphology (thin soil cover/sparse vegetation; low degree of erosion and dissection.
Inactive-No record of eruption and its form is beginning to change by the agents of weathering and erosion via formation of deep and long gullies.,[object Object]
Mount Etna, Sicily, Italy
Mauna Loa, Hawaii, USA

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Presentation on volcanos

  • 1. PRESENTATION ON VOLCANOS BY ANJALI PATRA ANKITA TRIPATHY
  • 2.
  • 3. Contents 1 Introduction 2 Plate tectonics and hotspots 3 Volcanic features 4 Erupted material 5 Volcanic activity 6 Notable volcanoes 7 Effects of volcanoes 8 Volcanoes on other planetary bodies 9 Panoramas
  • 4. INTRODUCTION A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, ash and gases to escape from below the surface. The word volcano is derived from the name of Vulcano island off Sicily which in turn, was named after Vulcan, the Roman god of fire. Volcanoes are generally found where tectonic plates are diverging or converging. Volcanoes can also form where there is stretching and thinning of the Earth's crust (called "non-hotspot intraplate volcanism"). Volcanoes can be caused by mantle plumes. The study of volcanoes is called volcanology, sometimes spelled vulcanology.
  • 5. Cleveland Volcano in the Aleutian Islands of Alaska photographed from the International Space Station, May 2006
  • 6.
  • 7.
  • 8.
  • 9. Other types of volcano include
  • 11. Fissure vents - Flat, linear cracks through which lava emerges.
  • 12.
  • 13. Cryptodomes -viscous lava forces its way up and causes a bulge, under great pressure.
  • 14. Volcanic cones (cinder cones) -erupt mostly small pieces of scoria and pyroclastics.
  • 15. Stratovolcanoes (composite volcanoes) -made of cinders, ash and lava.
  • 16.
  • 17. Subglacialvolcanoes-develop underneath icecaps, flat lava which flows at the top of extensive pillow lavas and palagonite.
  • 18.
  • 19. Erupted material Lava composition Another way of classifying volcanoes is by the composition of material erupted (lava), since this affects the shape of the volcano. Lava can be broadly classified into 4 different compositions :- If the erupted magma contains a high percentage (>63%) of silica, the lava is called felsic. If the erupted magma contains 52–63% silica, the lava is of intermediate composition. If the erupted magma contains <52% and >45% silica, the lava is called mafic or basaltic. Some erupted magmas contain <=45% silica and produce ultramafic lava.
  • 20. Lava texture Two types of lava are named according to the surface texture: ʻAʻa (pronounced [ˈʔaʔa]) and pāhoehoe ([paːˈho.eˈho.e]).ʻAʻais characterized by a rough, clinkery surface and is the typical texture of viscous lava flow.Pāhoehoeis characterized by its smooth and often ropey or wrinkly surface and is generally formed from more fluid lava flows.
  • 21.
  • 22. Potentially Active - Solfataras / Fumaroles - Geologically young (possibly erupted < 10,000 years and for calderas and large systems - possibly < 25,000 years). - Young-looking geomorphology (thin soil cover/sparse vegetation; low degree of erosion and dissection.
  • 23.
  • 28.
  • 30. a decline in the average temperature
  • 31. complex chemical reactions on Earth’s surface
  • 32. visual effects such as unusually colorful sunsets and affect global climate mainly by cooling it.
  • 33. benefit of adding nutrients to soil.
  • 34. create new islands Volcanoes on other planetary bodies The Earth's Moon has no large volcanoes and no current volcanic activity. he planet Venus has a surface that is 90% basalt, indicating that volcanism played a major role in shaping its surface. There are several extinct volcanoes on Mars, four of which are vast shield volcanoes far bigger than any on Earth. Jupiter's moon Io is the most volcanically active object in the solar system
  • 35. Panoramas Mount Bromo, East Java, Indonesia.
  • 37. Vulcano island with the north coast of Sicily in the background.
  • 39. Fourpeaked volcano, Alaska, in September 2007, after being thought extinct for over 10,000 years.