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Volcanoes and Other Igneous Activity Chapter 7 (page 207)

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Presentation on theme: "Volcanoes and Other Igneous Activity Chapter 7 (page 207)"— Presentation transcript:

1 Volcanoes and Other Igneous Activity Chapter 7 (page 207)

2 Volcanic eruptions  Factors that determine the violence of an eruption Composition of the magma (silica content) Temperature of the magma (hot or cool) Dissolved gases in the magma (volatiles) Viscosity of magma (Viscosity is a measure of a material's resistance to flow; it is determined by the amount of silica content in the magma)

3 Volcanic eruptions  Factors affecting magma viscosity Temperature (hotter magmas are less viscous) Chemical composition (silica content) - High silica – high viscosity (e.g., rhyolitic lava) - Low silica – more fluid (e.g., basaltic lava) Dissolved gases (volatiles) - Mainly water vapor and carbon dioxide - Gases expand near the surface → explosiveness

4 Controls of Volcanic eruptions  Mafic lava → low silica →low viscosity (more fluid) → hotter → less gases → less explosive → flatter cones Example: Hawaiian volcanoes, ocean floor volcanoes  Felsic andesitic lava → high silica → high viscosity (stiffer) → cooler→ more gases → more explosive → steeper cones Example: Mt St. Helen (cascade volcanoes), subduction zone volcanoes

5 Types of Hawaiian lava flows  Types of lava Pahoehoe lava (gas filled, resembles braids in ropes) Aa lava (gas free, rough, jagged blocks) Go to Youtube to watch videos

6 A Pahoehoe lava flow

7 A typical aa flow

8 A size comparison of the three types of volcanoes

9 A volcanic bomb Bomb is approximately 10 cm long

10 Types of Volcanoes  Shield volcano Broad, slightly domed Primarily made of basaltic (fluid) lava Generally large size Associated with ocean floor magmatism e.g., Mauna Loa in Hawaii

11 Types of Volcanoes  Cinder cone Built from ejected lava fragments (cinder) Steep slope angle Rather small size Frequently occur in groups Associated with subduction zones

12 Sunset Crater – a cinder cone near Flagstaff, Arizona

13 Types of Volcanoes  Composite cone (or stratovolcano) Large size Steep slope Interbedded lava flows and pyroclastic material Most violent type of eruptions Associated with subduction zones Most are adjacent to the Pacific Ocean (e.g., Cascade, Andes volcanoes)

14 A composite volcano (stratovolcano)

15 Features of Volcanoes  General features Conduit, or pipe Crater Vent Crater Fumaroles Caldera Crater Lake

16 16 What’s in a Volcano’s arsenal? Pyroclastic flow (very hot ash) Lahar (deadly mud flow) Crater Lake’s deadly gases

17 Mt. St. Helens – a typical composite volcano

18 Mt. Hood, Oregon

19 Mt. St. Helens Pyroclastic flow

20 A lahar along the Toutle River near Mt. St. Helens

21 Formation of a caldera

22 Crater Lake in Oregon

23 Formation of a volcanic neck

24 Plate Tectonics and Igneous Activity  Volcanism at Divergent plate margins: Type of magma: Basaltic Example: Mid Ocean ridge  Volcanism at Convergent plate margins Type of magma: Andesitic/felsic Example Island arcs; Andes Mountains

25 Plate Tectonics and Igneous Activity  Intraplate Volcanism (Hot Spot) not a plate margin Form over a stationary pocket of magma; type of lava: Basaltic Form a chain of volcanoes Example: Hawaiian volcanic chain The only active volcano is over the hot spot

26 Locations of some of Earth’s major volcanoes

27 Igneous Bodies Are bodies formed by the solidification of magma or lava

28 28 Intrusive igneous structures exposed by erosion

29 29 Plutons Type – I: tabular sheet like bodies  Concordant bodies (parallel): Sills (tabular) Laccoliths (irregular)  Discordant bodies (cut through): dikes

30 Plutons Type – II: Massive irregular bodies:  Batholiths  Stocks

31 31 A sill in the Salt River Canyon, Arizona

32 32 A batholith exposed by erosion

33 33 End of Chapter 7

34 Clicker test, do not talk, please.

35 35 1-Which Magma is more viscous? a.Basaltic b.Felsic/Andesitic c.Ultramafic d.None of these

36 36 2-which magma traps more gases? a.Mafic/Ultramafic b.Felsic/Andesitic c.None of these d.I am not sure

37 37 3-Which Magma is Hotter? a.Mafic/Ultramafic b.Felsic /Andesitic c.None of these d.I am not sure

38 38 4-Which magma produces more violent eruptions? a.Mafic/Ultramafic b.Felsic/Andesitic c.None of these d.I am not sure

39 39 5-Magma viscosity is a function of… a.Temperature b.Silica content c.Gases content d.All of these e.b only

40 40 6-Which volcano is over a hot spot? a.Mt St Helens (Washington State) b.Mt Rainier (Washington State) c.Mauna Loa (Hawaii) d.All of these e.a and c only

41 41 7-Which one is a Shield Volcano? a.Mt St Helens (Washington State) b.Mt Rainier (Washington State) c.Mauna Loa (Hawaii) d.All of these e.a and c only

42 42 8-Which one is a Composite cone? a.Mt St Helens (Washington State) b.Sunset Crater (Arizona) c.Mauna Loa (Hawaii) d.All of these e.a and c only

43 43 9-Which volcano type produces lava + pyroclastic flows a.Mt St Helens (Washington State) b.Kula (Hawaii) c.Mauna Loa (Hawaii) d.All of these e.a and c only

44 44 10-Volcanoes with steep cones have a.Fluid lava b.Viscous lava c.No relation whatsoever d.I am not sure

45 45 11-Volcanoes at divergent boundary erupt mainly…lava a.Felsic to Andesitic b.Mafic c.None of these d.I am not sure

46 46 12-Volcanoes at convergent margins produce mainly…lava a.Felsic to Andesitic b.Mafic c.None of these d.No relation whatsoever

47 47 13-Which volcanoes are more explosive? a.Shield volcanoes b.Composite cones c.Cinder cones d.None of these e.I am not sure

48 48 14-Volcano explosiveness is influenced by … a.Viscosity b.Temperature c.Amount of gases d.All of the above e.A and c only

49 49 15-A Pahoehoe lava is a.Gases-free with jagged surface lava b.Wrinkled, ropy, and gaseous lava c.Explosive ash and fragments flow d.None of these e.I am not sure


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