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NATURE OF VOLCANIC ERUPTIONS.

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Presentation on theme: "NATURE OF VOLCANIC ERUPTIONS."— Presentation transcript:

1 NATURE OF VOLCANIC ERUPTIONS

2 VIOLENCE OF VOLCANIC ERUPTIONS
Factors That influence the Violence of Volcanic Eruptions Composition of the Magma Temperature of the Magma Amount of dissolved Gases in the Magma

3 Composition & Viscosity

4 MAGMA & LAVA VISCOSITY As silica content Decreases
Viscosity “gooeyness”- a material’s resistance to flow (how thick it is) related to Silica content of magma As silica content Increases viscosity Increases - thicker magma As silica content Decreases viscosity Decreases - runny magma

5 VISCOSITY FACTORS

6

7 VISCOSITY FACTORS (CONT.)
COMPOSITION Low % Silica content – Low Viscosity (More fluid) Basaltic lava Intermediate % Silica content Andesitic lava High % Silica content – High Viscosity (Thicker) Granitic lava

8 VISCOSITY FACTORS TEMPERATURE
Hotter the magma the Less Viscous (more fluid) Hawaiian lava: 1170° C ° C very fluid (runny) Mt. Saint Helens lava: 500° C - 700° C very viscous (stiff)

9 VISCOSITY FACTORS (CONT.)
DISSOLVED GASES H2O & CO2 Gases escape, as magma moves toward the surface and the pressure is reduced. How easily do gases escape from magma? Low Viscosity (Fluid) magma quieter the eruption Gases can escape easily Viscous (Thick) magmas produce violent eruptions Gases become trapped within cooling magma and build up pressure

10 Volcanic MATERIAL

11 MATERIALS ASSOCIATED WITH VOLCANIC ERUPTIONS

12 LAVA FLOWS Aa Lava Pahoehoe Lava Basaltic lavas are more fluid
Types of Lava Aa Lava Rough, jagged blocks Pahoehoe Lava Resembles twisted braids in ropes Aa Pahoehoe

13 GASES Magma contains 1% - 5% gas Water vapor - H2O (70%)
Carbon dioxide - CO2 (15%) N2 and nitrogen compounds (5%) Sulfur compounds (5%) minor amounts of Cl, H2 & Ar

14 PYROCLASTIC MATERIAL Pyroclastic – means “Fire Fragments”
Pyroclastic – means “Fire Fragments” Types of Pyroclasts

15 ASH - fine, glassy fragments

16 PUMICE - forms “frothy” lava

17 CINDERS -“pea-sized” with voids

18 LAPILLI - “walnut” size

19 BLOCKS hardened lava > 64mm

20 VOLCANIC BOMB ejected as semi-molten hot lava > 64 mm

21 What materials are ejected from volcanoes?
Bellringer You have 5 minutes to answer the questions on a sheet of paper and turn into the basket What materials are ejected from volcanoes? Depending on the type of eruption, volcanoes may produce lava flows or eject pyroclastic materials, or both. Also all eruptions emit large amounts of gas.

22 “A volcano is a mountain with hiccups”
VOLCANOES “A volcano is a mountain with hiccups”

23 ANATOMY OF A VOLCANO

24 Parasitic cone Lava Pyroclastic material
ANATOMY OF A VOLCANO Crater Caldera Vent, Conduit (pipe) Parasitic cone Lava Pyroclastic material

25 Sratovolcano (Composite)
VOLCANO TYPES Shield Volcano Cinder Cone Volcano Sratovolcano (Composite) Lava Dome

26 SHIELD VOLCANO Broad & slightly domed Covers large area
Broad & slightly domed Covers large area Quiet eruptions produce large volumes of Basaltic lava Dark colored lava Low viscosity (very runny or fluid)

27 STRATOVOLCANO (COMPOSITE)
Large in size Iayered - lava & pyroclastics Most adjacent to Pacific Ocean Most Violent eruptions Produce “Lahars” Type of mudflow Produce “Nuée ardente” Fiery cloud Hot gases mixed with ash Flows down sides at speeds up to 200 kph

28 CINDER CONE Built from ejected lava fragments (pyroclastics)
Built from ejected lava fragments (pyroclastics) Have Steep Slopes Small in size Frequently occur in groups

29

30 THREE VOLCANO PROFILES

31 DANGERS OF COMPOSITE CONES MOUNT St. HELENS
Before: 5/18/1980 After: 5/18/1980

32 Nuée ardente & Lahars

33 *What are the three types of volcanoes?
Bellringer You have 5 minutes to answer the question on a sheet of paper and turn into the basket *What are the three types of volcanoes? The three main types of volcanoes are shield volcanoes, cinder cones, and composite cones.

34 Other Volcanic Landforms
EXTRUSIVE IGNEOUS FEATURES

35 VOLCANIC LANDFORMS Crater Steep walled depression at summit of volcano

36 CALDERA Collapsed crater generally larger than 1 km in diameter
Collapsed crater generally larger than 1 km in diameter Formation: Collapse - drained magma chamber Proclastic Explosion - blasts out material

37 VOLCANIC VENT & Conduit
Vent (pipe) – conduit that connects crater to magma chamber

38 VOLCANIC NECKS Magma that hardened in the volcanoes pipe (vent)
Magma that hardened in the volcanoes pipe (vent) Remains standing after volcano has eroded away Devils Tower (Wyoming) Shiprock (New Mexico) Tsé Bit' A'í - Rock With Wings

39 FLOOD BASALTS Lava flows that cover many square miles of area
fissures that open up in the crust lava flow out onto the surface

40 FISSURES Fissure - crack in the crust
allows lava to flow onto the surface

41 VOLCANIC PLATEAU Fissure Eruptions
Fissure Eruptions Volcanic material flows from fractures in crust Flood Basalts Yellowstone Plateau Columbia Plateau


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