Unit 5.7 - Formation of a volcano

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Procedures of forming a volcano

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Vivian Cheang

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Unit 5.7 - Formation of a volcanoVersión en línea Procedures of forming a volcano por Vivian Cheang 1 Plate Movement - Plate movement affects the magma in the asthenosphere, adding pressure & causes magma to flow up, breaking through into the crust (line of weakness). 2 Transitional Zone - Pressure is not strong enough to allow eruption onto the Earth’s surface directly. Magma is stored at the transitional zone. 3 Building pressure - Continuous plate movement allows the upflow of magma into the magma chamber. Pressure started to build up in the magma chamber. 4 Releasing pressure - High pressure has to be released when the amount stored within the magma chamber has reached to its limit. 5 Vent eruption - Magma erupts from the magma chamber in the crust, onto the earth's surface to release the high pressure, through a main crack developed called a vent. 6 Accumulation of volcanic rocks - Magma erupts onto the Earth’s surface as lava and solidifies as lava rocks at the crater (open end of the vent of a volcano). 7 Cone shape mountainous landform - Repeated eruptions built a cone shape mountainous landform called a volcano. Explanation 1 As magma leaves the asthenosphere and flows into the crust. This is already a form of "eruption", called INTRUSION. 2 The transitional zone within the crust is called a magma chamber. Magma chamber is usually refers to the heart of a volcano. 3 When there is more magma stored within the magma chamber, the pressure within the chamber increases. 4 Abnormally strong plate movement will also destabilise the pressure within the magma chamber. Thus, pressure has to be released. 5 The eruption of magma from a vent onto the Earth's surface is known as a vent eruption. It is a type of extrusion that usually happens suddenly and violently. 6 Continuous plate movement keeps adding pressure to the magma chamber. Thus, vent eruptions happen from time to time, allowing the accumulation of volcanic rocks around the crater. 7 Volcanic eruptions might take place with this cone shape mountainous landform, called a volcano.

Unit 5.7 - Formation of a volcanoVersión en línea

Procedures of forming a volcano

por Vivian Cheang

1 Plate Movement 2 Transitional Zone 3 Building pressure 4 Releasing pressure 5 Vent eruption 6 Accumulation of volcanic rocks 7 Cone shape mountainous landform

Explanation

As magma leaves the asthenosphere and flows into the crust. This is already a form of "eruption", called INTRUSION.

The transitional zone within the crust is called a magma chamber. Magma chamber is usually refers to the heart of a volcano.

When there is more magma stored within the magma chamber, the pressure within the chamber increases.

Abnormally strong plate movement will also destabilise the pressure within the magma chamber. Thus, pressure has to be released.

The eruption of magma from a vent onto the Earth's surface is known as a vent eruption. It is a type of extrusion that usually happens suddenly and violently.

Continuous plate movement keeps adding pressure to the magma chamber. Thus, vent eruptions happen from time to time, allowing the accumulation of volcanic rocks around the crater.

Volcanic eruptions might take place with this cone shape mountainous landform, called a volcano.

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Unit 5.7 - Formation of a volcano

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Unit 5.7 - Formation of a volcanoVersión en línea

por Vivian Cheang

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