Inside a Volcano: Magma Chamber and Eruptions

1. Volcanic Eruptions ch. 6 section 2

2. Inside a Volcano Beneath a volcano, magma collects in a pocket called a magmachamber. The magma moves upward through a pipe, which is a long tube in the ground that connects the magma chamber to the Earth’s surface. Molten rock and gas leave the volcano through an opening called a vent.

5. A volcanic eruption Dissolvedgasesare trapped in magma and are under great pressure. As magma reaches the surface, the dissolved gases begin to expand and exert an enormous force. When a volcano erupts, the force of the expanding gases pushes magma from the magma chamber through the pipe until it flows or explodes from the vent.

7. What do you think? What might happen if more magma is injected into the chamber from below?

8. Kinds of volcanic eruptions Geologists classify volcanic eruptions as quiet or explosive. The properties of magma determine how the volcano erupts. The type of eruption depends on the magma’s silica content. Silica is the material found in magma that is formed from the elements oxygen and silicon

9. Quiet eruptions A volcano erupts quietly if its magma is low in silica. Low silica magma is thin, runny and flows easily. The gases in the magma bubble out gently.

10. Quiet eruptions Quiet eruptions can produce two types of lava. Pahoehoe is fast moving, hot lava that is thin and runny. It looks like wrinkles when it hardens. Aa is cooler and slower moving. It is also thicker and has a rough surface when it hardens.

12. A volcano erupts explosively if its magma is high in silica. High silica magma is thick and sticky. The gases cannot escape the thick magma so they build up pressure until they explode! Explosive eruptions

13. Explosive eruptions An explosive volcano breaks lava into pieces that cool and harden in all different sizes. A pyroclastic flow is a type of explosive eruption that hurls out a mixture of hot gases, ash and cinders.

14. What do you think Identify if each of the following is an example of a high silica or low silica lava. • A lava river flowing away from a volcano • A plug of lava covering a volcano’s vent • Small pieces of lava being blasted high into the air.

15. Volcano hazards. Both types of eruptions can cause damage far from the volcano’s location. During a quiet eruption lava flows from vents setting fire to, and then burying everything in its path..

16. Volcano hazards During an explosive eruption, a volcano can release deadly gases, as well as ash and cinders

17. Life cycle of a volcano The activity of a volcano may last from less than a decade to more than 10 million years. Geologists use the terms active, dormant and extinct to describe a volcano’s stage of activity.

18. Life cycle of a volcano An active, or live volcano, is one that is erupting or showing signs to erupt in the future. A dormant, or sleeping volcano is expected to awaken and become active in the future. An extinct, or dead volcano is unlikely to erupt again.

20. Hot Springs and geysers are found in areas of present or past volcanic activity. A hot spring forms when water deep underground is heated by magma or hot rock. The hot water rises to the surface and collects in a pool. Hot Springs and Geysers

21. Hot springs and geysers Sometimes, the rising water and steam become trapped in a narrow crack. The pressure builds until it sprays above the surface as a geyser. A geyser is a fountain of steam and water that erupts from the ground.

22. Monitoring volcanoes Geologists use tiltmeters and other instruments to detect changes in or around a volcano. The changes may give warning a short time before an eruption. Scientists cannot predict the type of eruption or how powerful it may be.