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Volcanoes Chapter 10. Factors affecting Volcanic Eruptions. The three main factors that determine how violent and explosive a volcanic eruption can be are magma composition , magma temperature and the amount of dissolved gases in the magma. Magma Viscosity.
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Factors affecting Volcanic Eruptions The three main factors that determine how violent and explosive a volcanic eruption can be are magma composition, magma temperature and the amount of dissolved gases in the magma.
Magma Viscosity A magma's viscosity is its resistance to flow. Pancake syrup or honey has a higher viscosity than regular tap water. If you heat syrup or honey it lowers the viscosity. In like manner, the hotter the magma, the lower the viscosity of the magma.
Magma Composition and Viscosity If we use the syrup or honey analogy, the higher the sugar content, the higher the viscosity of the syrup or honey. Similarly, the more silica a magma has, the higher its viscosity. Magma with a felsic or rhyolitic composition has a higher viscosity than magma with amafic or basaltic composition.
Dissolved Gases Magma also contains dissolved gases. Some of those dissolved gases include water vapor, carbon dioxide, and sulfur dioxide. When the viscosity is high, dissolved gases become trapped in the magma, and the volcano builds up pressure. When viscosity is low, dissolved gases escape from the magma and the pressure is low.
Dissolved Gases When dissolved gases are high, pressure is high, and volcanic eruptions are explosive. When dissolved gases are low, pressure is low, and volcanic eruptions are quiet.
Volcanic Materials When people think of volcanoes and the materials produced by them, the most common thing people think of is lava. Lava is just magma at the earth’s surface. Although lava is one type of material that is produced by volcanoes, there are also other types of volcanic materials. Volcanoes also produce hot, broken rock fragments called pyroclastics.
Volcanic Materials The speed of a lava flow depends on its magma composition. Hot mafic/basaltic lavas can move relatively fast. Flow rates for mafic/basaltic lavas vary from 10 to 300 meters per hour. Silica-rich felsic/rhyolitic lavas move so slow that an observer can not detect its movement.
Volcanic Materials When a lava flow hardens and forms a skin with a braided rope-like texture, it is called pahoehoe (pah HOH ee hoh ee). When a lava flow hardens and forms a rough surface with jagged blocks, sharp edges, and spiny projections it is called aa (AH ah).
Volcanic Materials Particles and fragments of rocks ejected from a volcanic eruption that range in size from fine dust and ash to boulders that weigh several tons are referred to as pyroclastic materials. The small particles that are pea to walnut sized are called lapilli or cinders. The bigger particles are called blocks when they are hardened lava and volcanic bombs when they are ejected as glowing molten lava.
Types of Volcanoes There are three main types of volcanoes. Shield Volcanoes – produced by low viscosity, fluid, basaltic lavas. Shield volcanoes have the shape of a broad, gentle, sloping dome-like shape that resembles a warrior's shield. A good example of shield volcanoes are the volcanoes found on Hawaii.
Types of Volcanoes Cinder Cone Volcanoes – These volcanoes are relatively small. Usually they are no bigger than 30 to 300 meters, but occasionally they can get up to 700 meters tall. Cinder Cones are steep-sided. Cinder Cones get their name from the material they produce. They eject mostly cinders or lapilli which build up steep-sided cones.
Types of Volcanoes Cinder cones are usually produced from gas-rich, mafic/basaltic lavas. Cinder cones are usually short lived and usually are made by a single eruption. Cinder cones are often found in volcanic fields surrounded by other cinder cones, or occasionally on the sides of larger volcanoes like in the case of Mount Etna.
Types of Volcanoes Composite Cones – These are some of the world's largest, most explosive, and most powerful volcanoes. They are also called stratovolcanoes. Most of these volcanoes are located along the Circum Pacific Belt or Pacific Ring of Fire. Composite cones are produced by gas-rich, intermediate/andesitic lavas.
Types of Volcanoes Composite cone volcanoes have silica-rich, viscous lavas that generate explosive eruptions of pyroclastic materials. One of the most destructive features of a composite cone volcano is when hot gas, ash, and rock fragments flow down the side of the volcano at speeds up to 200 km/hr. This is called a pyroclastic flow.
Types of Volcanoes Another dangerous aspect of composite cone volcanoes are the mudflows (lahars). Lahars are mudflows created by volcanoes when the heat from a volcano melts snow and ice on a volcano and sends torrential flows of mud, water, and debris down the volcano.
Other Volcanic Landforms Calderas – When a volcano collapses after an eruption, a deep depression called a caldera is formed. Sometimes a large lake fills in the caldera. Yellowstone National Park is a caldera where a large eruption occurred. Volcanic Necks and Pipes – These form when the magma in the conduits come to the surface and cool and harden. Sometimes the sides of the volcano weather and erode to expose the neck or pipe later on.
Shiprock, NM and Devil's Tower, Wy, (Volcanic Necks and Pipes)
Other Volcanic Landforms Lava Plateaus – When fluid, basaltic magma comes to the surface through fissures or cracks in the ground, they can form large plateaus called lava plateaus. The Columbia Plateau in the northwestern United States is an example of a lava plateau.
Plutons When magma cools and hardens under the ground, it forms intrusive igneous bodies of rock called plutons. Plutons are classified by their shape, size, and relationship to the surrounding layers of rocks. A pluton called a sill forms when magma intrudes between two horizontal sedimentary rock layers close to the surface of the earth.
Plutons Laccoliths are similar to sills because they intrude in between horizontal sedimentary layers near the surface of the earth. The shape of laccoliths is different because the magma that forms a laccolith is more viscous and this causes the sill to take on a bulging lens-shaped appearance.
Plutons Dikes – Dikes are plutons that form when magma cuts across preexisting sedimentary rock layers. Sometimes these plutons travel diagonally, vertically, or sometimes they can radiate in all directions. Batholiths – These are the largest plutons. In order to be considered a batholith, it must have a surface area exposure greater than 100 kilometers squared. (10 km x 10 km)
