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

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Presentation on theme: "Section 13-2 Review Page #330:1-8."— Presentation transcript:

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

2 #1 Summarize the difference between mafic and felsic magma.
Mafic Magma magnesium & iron dark less viscous Felsic Magma silica & feldspars light more viscous

3 #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.

4 #3 Compare three major types of lava flows. Pahoehoe – ropy
Aa – jagged Blocky Lava – large chunks

5 Pahoehoe

6 Aa

7 #4 Define pyroclastic material, and list three examples.
Pyroclastic material consists of fragments of rock that form during an explosive eruption.

8 Pyroclastic Material volcanic ash/dust volcanic bombs lapilli

9 Volcanic Ash

10 Bomb

11 #5 Identify the three main types of volcanic cones. shield volcano
cinder cones composite volcano

12 Types of Volcanoes

13 Shield Volcano Mauna Loa - Hawaii

14 Cinder Cone

15 Composite Volcano

16 #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.

17 Caldera

18 Crater Lake

19 #7 List three events that may precede a volcanic eruption.
earthquake activity rock temperatures increase volcano area bulges

20 #8 Why 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.

21 The End On “Io” a moon of Jupiter


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