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Essay on volcano eruption
Essay on volcano eruption
volcanic eruption(essay)
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Why and how would Aerial Volcano erupt?
Aerial Island that you reside on is located along a convergent plate boundary between an oceanic plate and a continental plate. When the denser oceanic plate subducts beneath the less dense continental plate, solid mantle material melts at the subduction zone. This forms magma that is kept in a magma chamber. Pressure in the magma chamber builds up over time and when this pressure is released, the magma rises through the earth’s crust to cause volcanic eruptions.
The lava from the eruption cools to form new crust and the layers of ash and lava form the volcano.
Aerial Volcano is an active volcano that erupts pyroclastic flow (movement of hot rock fragments and super heated gases ejected down slopes).
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(Projected immediate physical, economic and social impacts)
• Physical
• The ash and mud from the volcano mixes with rainwater or melting ice, forming wet debris that flows down slopes. This creates lahars that can destroy human settlements and land used for agricultural purposes.
• The pyroclastic flow mainly consists of water vapor, carbon dioxide and sulfur dioxide. Sulfur dioxide released by the volcanic eruption into the air causes acid rain and the carbon dioxide released into the atmosphere would add to the greenhouse effect.
• When ash from the volcanic eruption flows into nearby rivers, it could lead to water pollution. Sources of potable water would then be contaminated, especially springs that provide 85% of the water the people use. Ash also blocks rivers, causing floods that could destroy crops and settlements.
• Fires started by the lava flow destroy forests and the gases, like carbon dioxide that is poisonous when inhaled in high concentrations, released from the eruption would kill wildlife and people.
• Social
• People are killed and injured by the fast-flowing lava and collapsing buildings. The gas from the pyroclastic flow, which can reach temperatures of 350˚C to 1000˚C, would cause skin burns and burn infrastructure and
Volcanoes are one of the most disastrous yet captivating geological land forms on earth. Many volcanic eruptions are catastrophic, but not all volcanic eruptions are as brutal. The two case studies I have chosen to compare and contrast are the 1980 Mount St. Helens eruption with the eruption of Hawaii’s Kilauea volcano which is still active today.
Alaskan volcanoes are different from Hawaii’s because they do not ooze out lava; they explode ash that can go up to 50,000 feet. If high enough, the ash can enter the Jet stream, a band of strong westerly air currents encircling
The volcano helps but when erupts can hurt surrounding area. Santa María is a major volcano in the region that has both provided and taken away resources for people. It has given crops to the land. Including “On Santa María alone, there are crops of coffee, rubber, sugarcane and cardamom.” (Ben Johrendt). These resources help Guatemala thrive. Without Santa Maria it could hurt them. When Santa Maria erupts it can also hurt the land by the lava destroying crops. “Eisen describes a “terrific hurricane” that devastated the vegetation around Santa María with five hours of powerful wind and torrential ash fall; almost every tree in the area had been burned, stripped, and felled by what he assumed were repeated lightning strikes – we now know this devastation was caused by pyroclastic flows, and probably by a directed blast.” (Jeannie A. J. Scott). Also the Lava can devastate the earth around it by burning everything around it.”A strong smell of sulfur was reported as far away as Guatemala City. The eruption column was 27 to 29 km high, and the huge, thick ash cloud kept the entire region in darkness for several days.”(Jeannie A. J. Scott). The way it helps and hurts the earth around it is interesting and help write this report.
This eruptions cause a leatral blasts ,lava flows , hot ash flows and many other disaster .
Basalt forms due to the partial melting of the layer of the mantle called the asthenosphere. The asthenosphere is the plastic zone of the mantle beneath the rigid lithosphere. Mantle plumes coming from the mesosphere can cause the asthenosphere to melt with heat or even if pressure decreases, which is called decompression melting (Richard 2011). The magma that forms from this melting is mafic magma that solidifies once it reaches the earth’s surface and cools quickly. The above process mainly occurs mainly during intraplate igneous activity which is the main explanation for volcanic activity that occurs a long distance away from a plate boundary. If the tectonic plate above the mantle plume is moving it can create a string of volcanic activity such as in Hawaii. See Fig 2.
The eruption on Mount Saint Helens has a specific cause and comes with many effects. A multifold of people would say that the “mountain looked like the site of an atomic blast” (Bredeson 30). That is a very accurate depiction as it took great power to inflict as much damage as it did. The reason for this impressive amount of force is that when magma is built up with pressure and an earthquake hits, the pressure gets magnified and the volcano explodes (Lewis). This is exactly what happened inside Mount Saint Helens. Furthermore, it has been revealed that “The earthquake that triggered the explosion was a 5.2 on the Richter scale” (Gunn 559). The earthquake to the magma can be compared as a match to gasoline. Even though the earthquake was not huge, the scale of the eruption was much greater than that of the earthquake (Gunn 560). The earthquake was only the trigger that allowed for more devastating things to occur. Thirteen hundred feet of the volcano were lost in the explosion followed by landslides, mudslides, and lava flows...
Climate Change has become a rising topic of interest and worry in Today's world. It has effected almost every aspect of modern life: Including the food industry, living conditions, as well as Volcanic activity. In recent years, Humanity has seen a steady increase in Volcanic activity, possibly due to climate change. The potential destruction from increased Volcanic Activity could potentially cause a mass extinction.
Over the centuries, the making of the Big Island as we know it today eventually entailed the growth and conjoining of six separate volcanoes, building all the way up from the seafloor, some 18,000 feet below the ocean’s surface. These volcanoes, from northwest to southeast, are named Mahukona, Kohala, Mauna Kea, Hualalai, Mauna Loa and Kilauea, and become younger as one moves north to south. Mahukona Volcano, just off the Big Island’s northwest coast, was the first volcano to start forming. Now submerged beneath the surface of the ocean because it is sinking into the Earth’s crust under its own vast weight, Mahukona is no longer visible. As the Pacific Plate slowly continued moving northwestward over the hotspot, the location of the rising magma moved relatively southeastward, and through time the rest of the Big Island volcanoes formed along that path.After Mahukona, Kohala Volcano, the precursor to today’s Kohala Mountain, erupted next. As Kohala Volcano emerged from the sea and joined with Mahukona, a much larger Big
Within a thousand kilometres falling ash, lava flows and the utter explosive force of the eruption would kill practically all life. Volcanic ash would cover places as far away as Iowa and the
The most iconic volcanic eruption in history was the eruption of Mt. Vesuvius in 79 A.D. Mt. Vesuvius is located on the west coast side of Italy. Pompeii was the ancient town five miles from Mt. Vesuvius where people would flock to the area in 79 AD to be near the Bay of Naples. Little did they know that the volcano would erupt into the most destructive volcano in history. Mt. Vesuvius has erupted about three dozen times and was the most disastrous due to the large population around the area. The volcano, which is still active today, is a stratovolcano. A stratovolcano has pyroclastic flows and erupt explosively and violently. Pyroclastic flows don't necessarily look exactly like “flowing eruptions”. These eruptions are not the “flowing” type of eruptions because they are eruptions with explosions and blowing clouds that fill the air. These clouds are usually dark clouds that are made up of ash. Pompeii had some signs of the volcano erupting, but the technology was not like the technology of today where scientists can monitor the volcanic activity.
Volcanoes can be one of the most destructive forces on Earth. It is estimated that some
Volcanoes can cause damage by spewing lava, but earthquakes before the eruption can also cause damage. These earthquakes open fissures and let magma out to the surface. When the magma exits these fissures, streams of lava up to hundreds of feet can shoot into the air. The picture below shows the lava erupting from the fissures created by the earthquakes in...
channel migration, the eruption of a volcano, the drying of a lake, or the destruction of a
When a volcano erupts, the focus is particularly on the consequences that take place near the volcano, such as weather conditions, the impact on nature, and the people who are affected. The noticeable changes that take place after a volcanic eruption includes the decrease in the temperature, natural disasters, such as tsunamis, droughts, and hurricanes, and the air pollution, which can be harmful to plants, animals, and people.