Volcanoes

How volcanoes are formed

  • Two plates collide or separate

  • Magma rises from the mantle to the vent

  • This is called an eruption

  • Magma wells from the magma chamber and reaches the surface where it cools and hardens.

  • This is known as lava.

  • After many eruptions, layers of lava and ash build up around the vent.

  • As a result, a cone-shaped mountain is formed with a crater on top from which the lava flows.

Types of volcano

Active - Erupted in the past 10,000 years. (Mt. Helen's, USA)

Dormant - Has not erupted in the past 10,000 years but may erupt again. (Kilimanjaro, Tanzania)

Extinct - Never expected to erupt again. (Mount Kenya, Kenya)

Case Study

Iceland - E15 (Eyjafjallajokull)

· 14 April 2010

· Very little lava

· Huge amounts of ash

· Blown south-easterly towards Europe

· 3-4 on VEI scale

Economic Impacts

Positive

· Visitor centre built, generating income for local community.

· Fertile soil

Negative

· 100,000 European flights cancelled over 8 days

· Cost airlines 145 million per day

· Loss of earnings

Social impacts

Positive

· Tourism

· Employment

· 2008: 500,000 visitors

· 2016: 1.8 million

Negative

· Contaminated water supply

· Evacuation of locals