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Volcanoes!!.

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Presentation on theme: "Volcanoes!!."— Presentation transcript:

1 Volcanoes!!

2 What is a Volcano?

3 Volcano - A Volcano is an opening in the Earth’s surface through which molten material or volcanic gases are erupted.

4 A volcano can either be a classic volcanic cone…..

5 Mt. St. Helens, pre-1980

6 Mount Ranier

7 a crack in the ground, through which lava erupts……

8 Or a simple volcanic vent.

9 How Magma Rises To view this animation, click “View” and then “Slide Show” on the top navigation bar.

10 Where are volcanoes located?

11 Major Volcanoes Around the World

12 Volcanic Settings

13 How and Where Volcanoes Form
Volcanic activity takes place primarily at subduction boundaries, 4. Some of the magma reaches Earth’s surface, and volcanoes form on the overriding continental plate. 1. Water in the subducted rock is released into the asthenosphere. Oceanic lithosphere Continental lithosphere Asthenosphere 3. The magma is less dense than its surroundings, so it rises. 2. The water lowers the melting temperatures of materials in the asthenosphere, leading to magma formation.

14 Ocean- Continental Subduction Pacific Northwest Volcanoes

15 Ocean- Ocean Subduction

16 Ocean- Ocean Subduction

17 Diverging Boundary Volcano

18

19 Hot Spot Volcano

20 How and Where Volcanoes Form
Magma and volcanoes also form at hot spots. Kauai Oahu Direction of Plate Movement The Hawaiian Islands formed over a hot spot. Molokai Lanai Maui Hawaii

21 Major Hotspots of the World

22 Plate Tectonics and Magma Generation
To view this animation, click “View” and then “Slide Show” on the top navigation bar.

23 Tectonic Settings and Volcanic Activity
To view this animation, click “View” and then “Slide Show” on the top navigation bar.

24 Volcanoes are classified as either Active, Extinct or Dormant

25 Active

26

27

28 Dormat Mt. Ranier

29 Vesuvius

30 Extinct

31

32 Magma and Erupted Materials
Parameters of volcanism: Viscosity Chemistry of Magma Gases within the magma Water content of magma

33 Magma and Erupted Materials
Viscosity: Viscosity is a measure of how thick (viscous) and sticky a liquid is. VOCABULARY viscosity lava pahoehoe aa pillow lava pyroclastic material pyroclastic flow

34 Types of Magma

35 Felsic Magma Characteristics: -light in color
-high viscosity: means it is very thick and flows very slowly. -Associated with composite type volcanoes and continential hotspots -Found along continental-ocean subduction boundaries.

36

37 Mafic Magma Characteristics: -dark in color
-low viscosity: means it is thinner and flows much faster -Associated with shield volcanoes, rift zones, and oceanic hotspots -Found at divergent boundaries and oceanic hotspots

38

39 Gases in Magma Water Vapor Carbon-Dioxide Carbon Monoxide
Sulfur-Dioxide Hydrogen-Sulfide

40 Types of Lava

41 Pahoehoe Lava

42

43

44 Aa Lava Aa Lava

45

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47 Pillow Lava

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49 Types of Lava Fragments

50 Ash

51 Ash Layers

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53 Pyroclastic Rock- Tephra

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55 Pyroclastic Rock- Pumice

56 Cinder

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58 Bombs

59

60 Blocks Blocks

61 Volcanic Blocks

62 Pyroclastic Flows

63 There are three types of volcanic cones:
Cinder ______ – explosive eruptions, small but steep slopes, pyroclastics. _______ – non-explosive eruptions, fluid basaltic lava, gentle broad slopes. _________ – alternating between lava and pyroclastics, explosive and non-explosive eruptions, steep and tall. Shield Composite

64 Volcano Types To view this animation, click “View” and then “Slide Show” on the top navigation bar.

65 Volcanic Landforms Volcanoes
VOCABULARY A volcano’s shape and structure depend on how it erupts and what materials are released. shield volcano cinder cone composite volcano Shield volcanoes are formed by basaltic lava that flows long distances before hardening. lahar caldera Shield Volcano lava plateau

66 Shield and Composite Volcanoes

67 Volcanic Landforms Volcanoes
Cinder cones are formed when molten lava is thrown into the air from a vent and breaks into drops. These drops harden into cinders that form a steep cone around the vent. Cinder Cone

68 Volcanic Landforms Volcanoes
Composite volcanoes are formed by layers of pyroclastic materials and lava that have erupted in the past. Composite Volcano

69 Composite volcanoes

70 Debris Avalanche and Eruption of Mount St. Helens, Washington
To view this animation, click “View” and then “Slide Show” on the top navigation bar.

71 Nuee ardente: pyroclastic flow, of searing superheated gas and incandescent volcanic ash and dust
Mount Pelee, on the Carribean island of Martinique, 1902 eruption. All but 2 of the more than 20,000 people in the town of St. Pierre were killed.

72 Lava Plateau

73 Volcanic Landforms Volcanoes
A caldera is a large crater-shaped basin that forms when the top of a volcano collapses.

74 Formation of Crater Lake
To view this animation, click “View” and then “Slide Show” on the top navigation bar.

75 EFFUSIVE ERUPTIONS Generally at hots spots, spreading centers
Mantle comes directly to surface Hot lava; low viscosity, very mafic, flows easily, gases escape easily Forms shields, flood basalts

76 EXPLOSIVE ERUPTIONS Found at subduction zones
Magma low temp (800 degrees C), high viscosity, does not flow easilty, more felsic mineralogy, gases trapped, hard to predict explosions Forms composite volcanoes, cinder cones, calderas, aerial bombs, nuee ardente gas flows, very destructive

77


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