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Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries.

Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

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Page 1: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Chapter 8 Section 2Types of Volcanoes

Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries.

Page 2: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Volcanoes

Page 3: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

How do volcanoes work?• Heat and pressure cause rocks to melt and form magma.• Magma needs to get out, too much pressure!!!!!!• Rise in temperature or drop in pressure causes magma to form

faster.

Page 4: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

How do volcanoes work?

• Magma is forced onto Earth’s surface.

• It dries and hardens, this happens many times over thousands of years.

• Eventually a mountain called a volcano is formed.

Page 5: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Parts of a Volcano• Most volcanoes share a

specific set of features.

• The magma that feeds the eruptions pools deep underground in a structure called a magma chamber.

• At Earth’s surface, lava is released through openings called vents.

• Flowing lava in the interior travels through long, pipelike structures known as lava tubes.

Page 6: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Where do most volcanoes occur?

• Volcanoes occur at both divergent and convergent boundaries and also at hot spots.

Page 7: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Why do we have different types of Volcanoes?

• The process of magma formation is different at each type of plate boundary.

• Therefore, the composition of magma differs in each tectonic setting.

• Tectonic settings determine the types of volcanoes that form and the types of eruptions that take place.

Page 8: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Volcanoes at Divergent Boundaries

• At a divergent boundary, the lithosphere becomes thinner as two plates pull away from each other.

• A set of deep cracks form in an area called a rift zone.

• Hot mantle rock rises to fill these cracks.• As the rock rises, a decrease in pressure causes hot

mantle rock to melt and form magma.

• The magma that reaches Earth’s surface is called lava.

Basaltic magma rises to Earth’s surface through these fissures and erupts nonexplosively

Page 9: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Types of volcanoes

Page 10: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Types of volcanoes

• Shield volcano: usually form at hot spots, from non explosive eruptions

• Cinder cone volcano: form from explosive eruptions, very steep.

• Composite volcano: form from both explosive and non explosive eruptions.

Page 11: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Shield volcano

• Form from many layers of “runny” lava.• Very wide, not to steep.• Biggest type of volcanoes• Tallest mountain in the world is Mauna Kea

(measures from sea floor to top)• non explosive eruptions

Page 12: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Mauna Kea, Hawaii

Page 13: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Cinder cone volcano• Smallest type of volcano

• Most common

• Made from pyroclastic material (material shot out of a volcano)

• Form a large crater

• Explosive!

Page 14: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Paricutin, Mexico

Page 15: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Composite volcano:

• Eruptions alternate between explosive and non-explosive.

• Sometimes they have runny lava layers, other times the have pyroclastic materials form layers.

• Have a wide base and steep sides.

• Have a crater

• Mount Fuji

Page 16: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Mount Fuji

Page 17: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

2 Types of eruptions

• Explosive: volcanoes that build enough pressure to blow its top, sending pyroclastic material into the air.

• Non explosive: Build only enough pressure to allow lava to run down its sides.

Page 18: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Non explosive eruption

• Mafic: refers to rocks and magma rich in iron and magnesium.

• This type of lava that is very runny.

• As magma nears the surface there is little pressure, causing gasses escape easily.

• Magma low in Silica have quiet eruptions

Page 19: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Explosive eruptions

• Felsic: means magma with high silica and feldspar content.

• Felsic magma traps water and gas bubbles, which leads to lots of pressure.

• Silica acts like a cork• Explosive eruptions are caused by a build

up of high pressure.• Convergent zones contain lots of water,

therefore have explosive eruptions.

Page 20: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Pyroclastic materials

• Material that is thrown into the air during an explosion.

• Volcanic bombs: large blobs of magma that harden in the air.

• Lapilli: pebble size rocks

• Volcanic ash: tiny powder like material

Page 21: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries
Page 22: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Four types of lava

• Aa: lava that is thick and sharp

• Pahoehoe: lava that forms thin crust and wrinkles

• Pillow lava: lava that erupts under water, has a round shape

• Blocky lava: cooler, lava that does not travel far from eruption, jagged when it dries.

Page 23: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Aa

• lava that is thick and sharp

Page 24: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Pahoehoe:

• lava that forms thin crust and wrinkles

Page 25: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Pillow lava

• lava that erupts under water, has a round shape

Page 26: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries

Blocky lava

• cooler, lava that does not travel far from eruption, jagged when it dries.

Page 27: Chapter 8 Section 2 Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries