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Chapter 13 earth systems volcanoes
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Volcanoes are mountains with a large pool of magma. When pressure builds up the magma and lava spews out, this is called a volcanic eruption. So, how are volcanoes formed?
Volcanoes form in destructive and constructive areas on Earth. They form when plates in Earth’s core (tectonic plates) force molten rock, gases and ash to Earth’s upper mantle.
The magma lives in the Earth’s crust. Magma is made from rock and gases. When two tectonic plates collide they push magma to the Earth’s surface and as a result a volcanic eruption is caused.
Most volcanoes form and are active in the Pacific Ring of Fire. The Pacific Ring of Fire circles the Pacific Ocean. The tectonic plates are most active in the Pacific Ring of Fire which causes the most eruptions and volcanoes around it. There are over 420 volcanoes in the Pacific Ring of Fire.
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When the volcano is completely formed it has a magma pool at the bottom called the magma chamber.
The main vent is the hole at the top and it allows the magma to come out and cause a volcanic eruption. The secondary vent is a hole in the side therefore it allows the magma and lava to flow. The whole surface of the volcano is called the crater.
The difference between lava and magma is that magma is composed of molten rock and is stored in the Earth’s crust. Lava is magma that has reached the surface of our planet through a volcano vent.
There are many volcanoes on Earth. It takes 10,000 - 50,000 years for a volcano to form! There are 1,500, including the 218 under water. Eventually there will be volcanoes everywhere.
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Cody
Mauna Loa is located on a hot spot in the Pacific Ocean. It is not near a plate boundary, in fact it is 3,200 km from the nearest plate boundary, and is situated in the middle of the Pacific tectonic plate. This is actually a rarity, as 90% of volcanoes are along a tectonic plate boundary. A hot spot occurs where long, stationary vertical pools of magma rise up and towards the plate. Movement of the tectonic plates above the hot spot created Mauna Loa, along with the other Hawaiian volcanoes. The older Hawaiian Islands were once above this stationary hot spot, but have been carried northwest by the slowly moving Pacific plate. As the plate moves, it carries the previously formed, older, volcanoes with it, creating a trail of younger, new volcanoes behind. The islands are lined up along the Hawaiian Ridge-Emperor Seamounts chain, which is 3,750 miles and includes Kauai, Maui, Oahu and Hawai’i, from north to south, respectively. There are around 80 volcanoes in this chain; most of them underwater, consequently the term seamount refer to submarine volcanoes. Three volcanoes of Hawai’i, Mauna Loa, Kilauea and Loihi seamount, are all currently sharing the Hawaiian hot spot. Although, recent evidence has shown that all three volcanoes use have separate plumbing systems to expel the lava from the pool of magma deep below them. It has also been suggested that Loihi is slowly moving Mauna Loa from the center of the island, thus shifting directly over the hot spot. The closer to the hot spot a volcano is, the more active it will be. The Hawaiian hot spot has laid down layers of lava, building up enormous islands from the ocean floor.
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.
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.
About three-quarters of Japan is mountainous. They were formed by tectonic plates colliding. Volcanoes were formed by the land breaking, and the liquid rock built up in it. A lot of the volcanoes are active, yet no one knows when one will erupt. The
Stories about volcanoes are captivating. Myths come in different versions, but all of them are capable of capturing yours, and everybody’s imagination.
Volcanoes vary in shape, size, and type. Likewise, volcanoes have varied eruption styles, from beautiful fiery displays of explosive lava to pyroclastic flows of hot gases and ash. A volcano is an opening in the Earth’s surface where magma has erupted or poured through, generally resulting in hills or mountains (Abbott, 2014). This natural phenomenon has spawned a field of science known as volcanology. Volcanology is a branch of geological science that studies volcanoes, lava, and magma (RedOrbit.com, 2015). By studying volcanoes, volcanologists gain a better understanding of how volcanoes form and erupt.
Maunaloa last erupted in 1938 and Kilauea has been erupting since January 3,1938. The Hawaii Volcanoes National Park was named a World Biosphere site by UNESCO in 1987. Kilauea is also called the world's only drive-in volcano.
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...
Magma is a hot liquid made of melted minerals. Minerals can form crystals when they are cool. Igneous rock can form underground, where the magma cools. slowly. Or, igneous rock can form above ground, where the magma cools.
Volcanoes are one of natures most interesting and dangerous phenomenons. The way volcanoes operate can be understood, on a basic level, by just some simple physics and chemistry, this paper will investigate and explain some of the basic physics that govern the behavior of volcanoes.
Volcanoes can be one of the most destructive forces on Earth. It is estimated that some
overall there is a lot of different types of volcanoes like the cinder cone the shield and competitive they all have their own special things about them there is a lot of volcano in the world and they
Volcanoes are formed when magma is expelled from the Earth’s surface, resulting in volcanic eruptions consisting of ash and lava. Over time, the lava cools and forms into rock on the Earth’s surface. Whenever an eruption occurs, the newly-formed rock from the lava layers continuously until the volcano takes its shape. Volcanic eruptions have taken place for thousands of years, and even today, according to the U.S Geological Survey (2010), there are approximately 1500 active volcanoes located throughout the world.
A volcano is a mountain or hill built up around a vent that connects to a reservoir of molten rock from beneath the surface of the Earth. The molten rock is lighter than the surrounding hard rock and will eventually break through a weak point in the Earth’s crust. When this happens the volcano may have a violent eruption of gas, rocks, molten lava, and ash. Volcanoes are generally grouped into four categories: cinder cone, composite volcanoes, shield volcanoes, and lava domes.