Volcanoes and Other Igneous Activity Chapter 7 (page 207)

Post on 17-Dec-2015

214 views 0 download

Tags:

transcript

Volcanoes and Other Igneous Activity

Chapter 7 (page 207)

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)

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

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

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

A Pahoehoe lava flow

A typical aa flow

A size comparison of the three types of volcanoes

A volcanic bomb

Bomb is approximately 10 cm long

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

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

Sunset Crater – a cinder cone near Flagstaff, Arizona

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)

A composite volcano (stratovolcano)

Features of Volcanoes

General features • Conduit, or pipe• Crater • Vent• Crater• Fumaroles• Caldera• Crater Lake

16

What’s in a Volcano’s arsenal?

• Pyroclastic flow (very hot ash)

• Lahar (deadly mud flow)

• Crater Lake’s deadly gases

Mt. St. Helens – a typical composite volcano

Mt. Hood, Oregon

Mt. St. Helens Pyroclastic flow

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

Formation of a caldera

Crater Lake in Oregon

Formation of a volcanic neck

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

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

Locations of some of Earth’s major volcanoes

Igneous Bodies

Are bodies formed by the solidification of magma or lava

28

Intrusive igneous structures exposed by erosion

29

Plutons

Type – I: tabular sheet like bodies

Concordant bodies (parallel):• Sills (tabular) • Laccoliths (irregular)

Discordant bodies (cut through):• dikes

Plutons

Type – II: Massive irregular bodies:

BatholithsStocks

31

A sill in the Salt River Canyon, Arizona

32

A batholith exposed by erosion

33

End of Chapter 7

Clicker test, do not talk, please.

35

1-Which Magma is more viscous?

a. Basaltic

b. Felsic/Andesitic

c. Ultramafic

d. None of these

36

2-which magma traps more gases?

a. Mafic/Ultramafic

b. Felsic/Andesitic

c. None of these

d. I am not sure

37

3-Which Magma is Hotter?

a. Mafic/Ultramafic

b. Felsic /Andesitic

c. None of these

d. I am not sure

38

4-Which magma produces more violent eruptions?

a. Mafic/Ultramafic

b. Felsic/Andesitic

c. None of these

d. I am not sure

39

5-Magma viscosity is a function of…

a. Temperature

b. Silica content

c. Gases content

d. All of these

e. b only

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

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

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

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

10-Volcanoes with steep cones have

a. Fluid lava

b. Viscous lava

c. No relation whatsoever

d. I am not sure

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

12-Volcanoes at convergent margins produce mainly…lava

a. Felsic to Andesitic

b. Mafic

c. None of these

d. No relation whatsoever

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

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

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