section 13-2 review

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Section 13-2 Review Page #330:1-8

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Section 13-2 Review. Page #330:1-8. #1. Summarize the difference between mafic and felsic magma. Mafic Magma magnesium & iron dark less viscous. Felsic Magma silica & feldspars light more viscous. #2. Explain how the composition of magma affects the force of volcanic eruptions. - PowerPoint PPT Presentation

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Page 1: Section 13-2 Review

Section 13-2 ReviewPage #330:1-8

Page 2: Section 13-2 Review

#1

Summarize the difference between mafic and felsic magma.

Mafic Magma magnesium & iron dark less viscous

Felsic Magma silica & feldspars light more viscous

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#2

Explain how the composition of magma affects the force of volcanic eruptions.

More viscous magma traps gases more easily than less viscous magma, which may lead to more explosive eruptions.

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#3

Compare three major types of lava flows.

• Pahoehoe – ropy • Aa – jagged • Blocky Lava – large chunks

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Pahoehoe

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Aa

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#4

Define pyroclastic material, and list three examples.

Pyroclastic material consists of fragments of rock that form during an explosive eruption.

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Pyroclastic Materialvolcanic ash/dust

lapilli

volcanic bombs

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Volcanic Ash

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Bomb

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#5Identify the three main types of volcanic cones.

shield volcanocinder conescomposite volcano

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Types of Volcanoes

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Shield Volcano

Mauna Loa - Hawaii

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Composite Volcano

http://video.google.com/videoplay?docid=3977416382972126736&q=mt+st+helens+eruption&hl=en

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#6

Describe how calderas form.

A caldera forms when the magma chamber of a volcano empties, causing the volcanic cone to collapse in upon it, or when magma is ejected violently and the cone is destroyed.

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Caldera

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Crater Lake

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#7

List three events that may precede a volcanic eruption.

earthquake activity

rock temperatures increase

volcano area bulges

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#8Why would a sudden increase of earthquake activity around a volcano indicate a possible eruption.

Sudden earthquake activity could be caused by magma moving upward through the rock around the volcano.

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The End

On “Io” a moon of Jupiter