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CH 6 Prentice Hall p.178-181 CH 6 Prentice Hall p.178-181 Volcanoes & Plate Tectonics.

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Presentation on theme: "CH 6 Prentice Hall p.178-181 CH 6 Prentice Hall p.178-181 Volcanoes & Plate Tectonics."— Presentation transcript:

1 CH 6 Prentice Hall p.178-181 CH 6 Prentice Hall p.178-181 Volcanoes & Plate Tectonics

2 Characteristics of Magma The force of an eruption depends partly on the amount of gases dissolved in the magma. The temperature and the silica content are also important factors. – Temp- partially determines whether it is thick or fluid. (Hotter- the more fluid it is.)

3 Characteristics of Magma Silica- a material found in magma composed of the elements silica and oxygen. (The more silica- the thicker the magma.) High Silica- light colored lava – Rhyolite an extrusive igneous rock – Pumice spaces left in the rock by gases bubbling out. – Obsidian- cools very quickly giving a glassy texture. Low Silica- dark colored rocks – Basalt dark colored extrusive igneous rock

4 Types of Volcanic Eruptions A volcano’s magma influences how the volcano erupts. The silica content helps determine whether the volcanic eruption is quiet or explosive.

5 Quiet Eruptions Magma flows easily. Dissolved gases in the magma bubble out easily. Thin runny lava oozes from the vent and flows. Examples Iceland and Hawaii

6 aa Cooler, slow moving lava. Forms jagged chunks of lava.

7 Pahoehoe Fast moving, hot lava. Surface of lava looks like a solid mass of wrinkles, billows and ropelike coils.

8 Explosive Eruptions Magma is thick and sticky. Thick magma builds up in the pipe, plugging it like a cork in a bottle. Pressure builds up due to the gases in the magma until the volcano explodes. The gases push the magma out with incredible force.

9 Explosive Eruptions Fragments: Volcanic Ash – fine, rocky, grain of sand sized particles. Cinders- – pebble sized particles Bombs- – large pieces of rock (baseball to the size of a car) Pyroclastic Flow Occurs when an explosive eruption hurls out ash, cinders and bombs as well as gases. (400mph, 1,800˚F)

10 Other types of Volcanic Activity Hot Spring- Forms when groundwater heated by a nearby body of magma rises to the surface and collects in a natural pool.

11 Other types of Volcanic Activity Geyser- A fountain of water and steam that erupts from the ground. – Forms due to rising hot water and steam that become trapped underground in a narrow crack. – Builds up pressure until it sprays out of the ground.

12 Other types of Volcanic Activity Geothermal Energy- A clean, reliable energy source provided by water heated by magma. Hot water can be piped into homes. Used as a source of electricity – Steam is piped into a turbine that spins and generates electricity.

13 Monitoring Volcanoes Geologists are more successful with predicting a volcanic eruption. Changes around a volcano shows signs of an eruption and allow for a short warning time. – Monitor a volcano with: Tiltmeters and Laser ranging devices to see ground changes due to shifting magma. Monitor escaping gases and water level in a volcano's crater lake.

14 Monitoring Volcanoes – Monitor a volcano with: Check the temperature of the ground water to see if the magma is heating it. Monitor the many small earthquakes triggered by magma moving from the chamber to the pipe. – Unable to predict the strength of the eruption

15 Volcano Hazards Time between eruptions can span hundreds of years. (Dormant Volcano) – People may be unaware of the danger. – Mt. St Helens 123 years.

16 Volcano Hazards Quiet Eruptions: – Lava flows- set fire and bury everything in their path. Explosive Eruptions: – Hot clouds of volcanic gases, cinders and bombs Pyroclastic Flow

17 Volcano Hazards Volcanic Ash: – Bury towns, damage crops, and clog car engines. – Wet ash is heavy and can cause roofs to collapse. Plane engines can fail if pulled into the engine. Lahar: – A mud flow of caused by melted snow. Carries ash, trees and rocks.

18 Volcano Hazards Pompeii


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