INTRODUCTION. This project is about volcanoes and how they form and how they function. It will also show you the different aspects of a volcano.



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Transcription:

BY RYAN O MAHONY

INTRODUCTION This project is about volcanoes and how they form and how they function. It will also show you the different aspects of a volcano.

MAP OF VOLCANOES AROUND THE WORLD

DIAGRAM OF A VOLCANO

ACIDIC AND BASIC LAVA There are two types of lava(magma that rises to the surface).these are acidic and basic lava. Acidic lava is high in silica content(70% or more).this type of lava tends to be thick and does not flow very far. Acidic lava is associated with violent volcanic eruptions due to the silica in the magma which traps the gases in the volcano increasing the pressure build up in the volcano, which adds to the power of the eruption.

ACIDIC AND BASIC LAVA Basic lava is then the opposite with low silica content(55% or less).this lava flows much faster and covers a much greater distance. Since there is less silica in basic lava. Less gas is trapped before an eruption so volcanoes with basic lava tend to have less dramatic more gentle eruptions. Knowing the type of lava a volcano contains is important to understand whether a volcano will have a gentle or violent eruption.

THE FOUR MAIN TYPES OF VOLCANOES There are four main types of volcanoes. COMPOSITE VOLCANO. SHIELD VOLCANO. VOLCANIC DOME. CINDER VOLCANO.

COMPOSITE VOLCANO Composite volcanoes tend to be the biggest volcanoes. They are mainly steep sided built of alternating lava flows, volcanic ash, cinders, blocks and bombs may rise to 8000 feet above their bases This type of volcano has acidic lava which means they tend to have violent eruptions. A common feature of this volcano would be a crater at the summit and a conduit system of vents through which magma rises from the magma chamber during an eruption An example of a composite volcano is Mt Vesuvius in Italy.

SHIELD VOLCANOES Shield volcanoes are small volcanoes with gentle slopes and a broad base. This is due to the basic lava erupting from it. This lava cools from the change in temperature it experiences and solidifies to make basalt rock. Over time these layers build up adding to the volcano. This is how these volcanoes form. These volcanoes are common at hotspots An example of this type of volcano would be Mauna Loa in Hawaii.

VOLCANIC DOMES Volcanic domes tend to have very steep sides. This is due to the acidic lava erupting from the main vent. High amounts of gas trapped in the lava leads to a violent eruption. They have steep sides because the lava does not flow very far and tends to solidify in and around the vent which contributes to the pressure build up before an eruption. This also contributes to violent eruptions. Mount Saint Helens is an example of a dome volcano.

CINDER VOLCANO Cinder volcanoes are the simplest form of volcanoes which form because of violent eruptions. They tend to have gentle slopes due to how the volcanic particles spread during an eruption. They tend to have an oval shaped summit due to the violent eruption off the other volcano. These volcanoes rarely rise above a thousand feet These volcanoes are commonly found around volcanic terrains around the planet such as North America.

HOTSPOT VOLCANOES Hotspot volcanoes are volcanoes that form over areas of the crust that have a plume of magma formed under it. As the plate on which the volcano formed moves on the volcano will lose its source of magma and eventually become extinct because the plume of magma will stay in the same place. Eventually another volcano will form over it as the other one has moved. This process will repeat itself and will produce a chain of volcanic islands. An example of these islands would be the Hawaiian islands.

ACTIVE, DORMANT AND EXTINCT VOLCANOES These are terms used to describe how often volcanoes erupt. Active volcanoes are volcanoes that erupt on a regular basis. An example of an active volcano would be Mount St Helens in the U.S.A Dormant volcanoes are volcanoes that have not erupted in a long time but may erupt again. An example of a dormant volcano would be Cotopaxi in Peru An extinct volcano is a volcano that has not erupted in recorded history. An example of an extinct volcano would be Slemish mountain in Co. Antrim Northern Ireland.

PACIFIC RING OF FIRE