1. Original Source: sites.tenafly.k12.nj.us/~plobosco/
Volcanoes
Original Source: sites.tenafly.k12.nj.us/~plobosco/

2. Volcanoes and Earth’s Moving Plates
Objectives:
To describe how volcanoes can affect people.
To discuss the conditions that cause volcanoes.
Identify the relationship between volcanoes and Earth’s moving plates.

3. Volcanoes
A volcano is an opening in the Earth that erupts gases, ash and lava.
Kilauea is the world’s most active volcano.

4. Lava
When the magma reaches the surface, it is called lava. The place in the Earth’s surface through which magma and other materials reach the surface is called a volcano. In some places, lava can build up to form a cone-shaped mountain.
The opening from which lava erupts is the vent. Volcanoes often have more than one vent.

5. Formation of a Volcano The opening where lava flows out is a vent.
The steep walled depression around the vent is a crater.

6. Volcanoes
Volcanoes can be both destructive and constructive forces.

7. Destructive Effects of Eruptions
Lava destroys everything in its path. Ash can cause lung damage.
If ash and debris run down the side of the mountain, this is called a pyroclastic flow. Temperatures in this flow can be hot enough to ignite wood.
Sulfurous gases can mix with water vapor and form acid rain that kills plants and animals.

8. Constructive Effects of Eruptions
The soil formed from volcanoes is very fertile and will eventually lead to abundant plant growth.
The sulfur in volcanic vents along the ocean floor allow life to exist without sunlight
Volcanoes recycle earth’s minerals

9. Where do Volcanoes occur?
Volcanoes form along divergent plate boundaries, convergent boundaries and hot spots.

10. Divergent Plates
Volcanoes often form where plates are moving apart, such as the Surtsey in Iceland.
Iceland is located on the Mid Atlantic Ridge.

11. Convergent Plate Boundaries
Soufriere Hills On the Island of Monserrat is an example of a volcano that formed when one plate slide under another and melted.
The magma was forced up and formed a volcano.

12. Hot Spots Some volcanoes form over hot spots in the mantle.
These are not on a plate boundary but in the center of a plate.
The Hawaiian Islands formed over a hot spot in the Pacific Plate.

13. Types of Volcanoes Objectives:
To discuss how explosiveness of a volcano is related to the silica and water content.
To discuss the three types of volcanoes.

14. Magma
Deep within the Earth, under tremendous pressure and at great temperatures, rock exists as a hot liquid called magma. This molten rock is found in pockets called magma chambers.

15. What Controls Eruptions?
Eruptions are controlled by
1) the amount of trapped gas and the water vapor
2) how much silica is present in the magma

16. Trapped Gas
As magma reaches the surface, it is under less pressure. Gas can escape. Gas escapes easily during quiet eruptions.
If gas build up to high pressure this will cause an explosive eruption.

17. Amount of Water Vapor
The magma at some convergent boundaries contains a lot of water vapor.
This is because oceanic plate material and some of its water slide under other plate material at some convergent plate boundaries.
The trapped water vapor in the magma can cause explosive eruptions.

18. Viscosity of Magma
Magma is divided into two major types: silica rich and silica poor
The greater the silica content, the more viscous or thick the magma.

19. Basaltic Magma
Magma that is low in silica is called basaltic magma. It is fluid and produces quiet flows such as those at Kiluea.
Basaltic lava flows under water produce pillow lava formations.

20. Basaltic Lava
Pahoehoe (p-hoi-hoi) forms a smooth, billowy, ropelike surface.
Aa, flows at a lower temperature, is stiff and slow moving.

21. Andesitic Magma
Andesitic magma is more rich in silica than basaltic magma but it has less silica than granitic magma.
It forms at convergent boundaries where one plate slides under the other.
It is more explosive than basaltic magma.
Krakatau was mainly andesitic in composition. The word andesitic comes from the Andes Mountains.

22. Granitic Magma
This type of lava is light in color. This lava, has high water content and high silica content. Light-colored lava causes explosive eruptions. Silica hardens in the vents and form rocks. Steam and new lava build up under the rocks. When the pressure becomes great, a violent explosion occurs. When this type of lava cools on the surface it forms the igneous rock, rhyolite, which resembles granite.

23. Gaseous Lava
When lava that contains large amounts of gases, such as steam and carbon dioxide, hardens it forms rocks with many holes in them, due to the gas bubbles.
Pumice and scoria are igneous rocks formed from this type of lava.

24. 3 Types of Volcanoes
Different types of volcanic eruptions form different types of volcanoes.
Cinder cones
Shield volcanoes
Composite volcanoes

25. Cinder Cones
They are steep sided cones of basaltic fragments and are smaller and simpler than composite volcanoes.
Streaming gases carry liquid lava blobs into the atmosphere that fall back to earth around a single vent to form the cone.
The volcano forms when ash, cinders pile up around the vent to form
a circular or oval cone.
Most common kind of volcano

26. Tephra
Explosive eruptions throw lava and rock high into the air. Bits of rock or solidified lava dropped from the air are called tephra.
The smallest particles are called volcanic dust. (less than 0.25 mm)
Volcanic Ash ( mm) falls to the Earth and forms small rocks.
Cinder (5mm-a few cm)
Volcanic bombs (a few cm to several meters) are molten and harden as they travel through the air.

27. Paricutin Volcano in Mexico

28. Shield Volcanoes
Volcanoes composed of quiet flows are called shield volcanoes.
Because it is runny, the lava flows over a large area. After several eruptions, a dome-shaped mountain is formed such as Mauna Loa (4km over sea level) in the Hawaiian Islands.

29. Mauna Loa, Hawaii – Earth’s Largest Volcano

30. Flood Basalts
Basaltic lava can also flow onto Earth’s surface through large cracks called fissures.
This type of eruption forms flood basalts
Columbia Plateau was formed as the lava spread out over the ground.

31. Composite Volcanoes (Stratovolcano)
Most deadly
Volcanoes built up of alternating layers of rock particles and lava are called composite volcanoes.
During the formation of a composite volcano, a violent eruption first occurs, hurling volcanic bombs, cinder and ash out of the vent. Then a quiet eruption, produces lava flow that covers the rock particles.
Lower slope is gentle, but they rise steeply toward the summit

32. Composite Volcano (Stratovolcano)

33. Mount Vesuvius (near Naples, Italy)

34. Mount St Helens

35. Krakatau
One of the most violent eruptions in recent times occurred on an island in the Sunda Straits neat Indonesia in 1883.
36,000 people were killed.
The island fell into the magma chamber.

36. Igneous Rock Features Objectives To describe intrusive rock features.
To explain how a volcanic neck and a caldera form.

37. Predicting Volcanoes There are four indicators of volcanic activity:
Rising magma (increase in electric current)
Seismic activity (tremors)
Ground deformation
Changes in gases (carbon dioxide and sulfur dioxide)

38. Instruments used to Detect Volcanic Activity
Tiltmeters are sensors that use laser beams to help create map of the physical changes in the earth’s surface that rising magma causes.
Scientists also measure the levels of gases escaping, such as carbon dioxide and sulfur dioxide.
Gravimeters measure the electrical currents given off by magma. An increase indicates a rise in the level of magma
The most recent development uses satellites to detect heat from the gases released by volcanoes.
The satellite Landsat uses infrared sensors.

39. Limits of Seismography in Detecting Volcanic Activity
Seismographs cannot determine magma height, depth or how fast the magma is rising.

40. Crater
There is often a funnel-shaped pit or depression at the top of a volcanic cone. This pit is called a crater.
If the crater becomes very large as a result of the collapse of its walls, it is called a caldera. A caldera may also form when the top of a volcano explodes or collapses.

41. Volcanic Crater

42. Intrusive Igneous Rock Features
Most magma never reaches the surface.
Much of it hardens in the earth.
Sometimes the hardened magma becomes exposed at the surface.
These rock bodies are called intrusive igneous rock features.
Examples are batholiths, sill, dikes and volcanic necks.

43. Batholiths
The largest intrusive igneous rock bodies are called batholiths. They form when magma bodies that are being forced upward cool and solidify before reaching the surface.

44. Yosemite National Park
The granite domes of Yosemite National Park are exposed batholiths.

45. Sills and Dikes
Magma sometimes squeezes into cracks below the surface.
Magma that cuts across rock layers and hardens is called a dike.
Magma that is forced into a crack parallel to the rock layers and hardens is a sill.

46. Volcanic Neck
When a volcano stops erupting, magma will harden inside the vent.
Erosion wears away the outside of the volcano and the solid igneous rock in the vent remains.
Ship Rock in New Mexico was formed this way.

47. Calderas
Sometimes after an eruption, the top of a volcano can collapse. This produces a large depression called a caldera.
Crater Lake in Oregon is a caldera that filled with water and is now a lake.

48. Volcanic Activity
Volcanoes are rather unpredictable. Some erupt regularly, others have not erupted in modern history. Scientists classify them as active, dormant or extinct.

49. Active Volcanoes
An active volcano is one that erupts whether continually or periodically such as Mount Katmai in Alaska and Mount St. Helens in the Cascade Range.

50. Dormant Volcano
A volcano that has been known to erupt within modern times but is now inactive is classified as a dormant volcano. Mount Rainier in Washington state is an example of a dormant volcano in the United States.
Scientists can be wrong. Mount St. Helens was considered to be dormant but erupted after long periods of inactivity.

51. Extinct Volcano
A volcano not known to have erupted within modern history is classified as an extinct volcano. They have been worn away almost to the level of their magma chamber.

52. Volcano and Earthquake Zones
Most major earthquakes and volcanic eruptions occur in three zones of the world. Scientists believe that there is a great deal of movement and activity in the Earth’s crust in these three zones.

53. Ring of Fire
One major earthquake and volcano zone extends nearly all the way around the edge of the Pacific Ocean. This zone goes through New Zealand, the Philippines, Japan, Alaska and along the western coasts of North and South America. The San Andreas fault is part of this zone.

54. Ring of Fire

55. Mediterranean Zone
A second Major earthquake and volcano zone is located near the Mediterranean Zone and extends across Asia into India. Many countries in the zone, including Italy, Greece and Turkey, have violent earthquakes. Many volcanic eruptions also occur in this zone.

56. Mid-Atlantic Ridge Zone
The third major earthquake and volcano zone extends through Iceland and to the middle of the Atlantic Ocean.
Under the ocean, there is a long range of volcanic mountains called the Mid-Atlantic Ocean Range. Scientists believe that the volcano and earthquake activity are due to the formation of new parts of the Earth’s crust along the ridge. The volcanic island of Iceland is part of this zone.

57. Earthquake Belts

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