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Volcanoes

Volcanoes. A Volcano is an area in the earth’s crust where molten rock, gases, and ash erupt from. Volcano also refers to the landform that develops. How Volcanoes Form. Magma Formation The following 3 conditions will allow magma to form.

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Volcanoes

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  1. Volcanoes

  2. AVolcano is an area in the earth’s crust where molten rock, gases, and ash erupt from. Volcano also refers to the landform that develops.

  3. How Volcanoes Form

  4. Magma FormationThe following 3 conditions will allow magma to form.

  5. 1. A decrease in pressure lowers the melting point of rock material. This happens along a rift valley at a mid-ocean ridge.

  6. 2. An increase in temperature can cause rock material to melt. This happens near a hot spot such as the Hawaiian Islands.

  7. 3. An increase in the amount of water in the asthenosphere can lower the melting temperature. This happens at subduction boundaries.

  8. Why water lowers the melting point of rock and forms magma in subduction zones, by Brandon Browne, former LCHS student and Ph.D. volcanologist at Cal State Fullerton“When water dissolves into the structure or rock, chemical bonds holding minerals together are shortened (reducing viscosity) and eventually broken (melting) if the rock becomes saturated, which is defined as the point where any additional water added to the rock will form a separate phase like a bubble. another way to think about it is that water saturation requires the total Pressure to equal dissolved H2O Pressure. Decompressing rock has the same effect, which is why anhydrous (dry) mantle can melt through decompression at constant T.”

  9. Parts of a Volcano

  10. Active if it has erupted in historic time. This is anywhere from 200 to 3,000 years, depending on the region.Dormant if it is not currently active, but could become so.Extinct when scientists consider it unlikely to erupt again. Volcano ActivityA volcano is considered:

  11. Where Volcanoes Form

  12. World Earthquake and Volcano Distribution

  13. Many powerful volcanoes of the world can be found in the Pacific Ring of Fire.

  14. At Subduction Boundaries Less Dense (Continental or Oceanic Crust) More Dense (Oceanic Crust)

  15. Volcanoes form on the overriding plate. The Cascades (Mt. St. Helens, Mt. Shasta, Mt. Rainier) are a good example Cascade Mountains Juan de Fuca Plate North American Plate

  16. Mt. Rainier, Washington: A composite volcano formed at a subduction boundary where the Juan De Fuca Plate is diving under the North American Plate

  17. At Divergent Boundary Rift Valleys and Mid-Ocean Ridges

  18. Magma rises to the surface at a mid-ocean ridge in pillow lava formations and/or hydrothermal vents. Most volcanoes occur here.

  19. At Hot Spots Hawaiian Islands are a good example. Oldest Islands Hot Spot Pacific Plate Movement Newest Islands

  20. Magma and Material Erupted from a Volcano

  21. What determines whether a volcano will be explosive like this?

  22. …and what determines whether a volcano will be docile like this?

  23. The answer is the type of magma that causes the eruption. Low Viscosity, gas and silica content High Viscosity, gas and silica content

  24. …but what is viscosity?Viscosity is the resistance to flow of magma/lava.

  25. Vegetable Oil Water Syrup Viscosity Ratings of Known Liquids

  26. Vegetable Oil Water Syrup Viscosity Ratings of Known Liquids Low Viscosity

  27. Vegetable Oil Water Syrup Viscosity Ratings of Known Liquids Low Viscosity Medium Viscosity

  28. Vegetable Oil Water Syrup Viscosity Ratings of Known Liquids Medium Viscosity Low Viscosity High Viscosity

  29. Vegetable Oil Water Syrup Viscosity Ratings of Known Liquids Medium Viscosity Low Viscosity Like basaltic magma High Viscosity

  30. Vegetable Oil Water Syrup Viscosity Ratings of Known Liquids Medium Viscosity Low Viscosity Like andesitic magma Like basaltic magma High Viscosity

  31. Vegetable Oil Water Syrup Viscosity Ratings of Known Liquids Medium Viscosity Low Viscosity Like andesitic magma Like basaltic magma High Viscosity Like rhyolitic magma

  32. Magmas high in silica (quartz) concentration resist flow and have high viscosity.

  33. Magmas low in silica (quartz) concentration flow more easily and have low viscosity.

  34. Higher concentrations of gas (mostly water vapor and carbon dioxide) in the magma result in explosive volcanoes.

  35. Lower concentrations of gas (mostly water vapor and carbon dioxide) in the magma result in docile volcanoes.

  36. Characteristics of Magma (see page 199 in your book)

  37. Basaltic magma forms at mid-ocean ridges and hot spots. Mid-Ocean Ridges Hot Spots

  38. Hawaii: A low viscosity lava.

  39. Hawaii: A low viscosity lava.

  40. Hawaiian Basalt

  41. Kilauea Crater

  42. Basalt eats roads!

  43. Andesitic magma forms at subduction zones. Subduction Zone

  44. Andesitic Magma found at Mt. St. Helens, WA

  45. Devastation from explosive eruption of Mt. St. Helens, WA

  46. Rhyolitic magma forms at continental hot spots such as Yellowstone Park. Continental Hot Spot

  47. Yellowstone National Park is a good example of an extremely explosive volcano with rhyolitic magma!

  48. Yellowstone National Park is a good example of an extremely explosive volcano with rhyolitic magma!

  49. Yellowstone National Park is a good example of an extremely explosive volcano with rhyolitic magma!

  50. Yellowstone National Park is a good example of an extremely explosive volcano with rhyolitic magma!

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