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Physics of volcanos
An essay on volcanic eruption
Short note on volcano
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Volcanoes are conical structure built by discharge of lava. The dome- shaped structures not only have increased beauty of the nature and make it look magnificent but on the other hand they are extremely dangerous as they contribute to create huge catastrophes. As an illustration, the word volcano is originated from the name Vulcan, which means the god of fire in Roman. Centuries ago people believed that the eruption of volcanoes are a supernatural for instance, in Polynesia, there is a peak called Pele’s peak where people thought that the eruption was caused whenever, Pele the god of volcanoes were angry. All the misconception was because people were living a centuries of blindness where technologies weren’t used and people believe on what they heard but today with the advance of technology and intellectualism we know that volcanic eruptions are not super natural, but are the form due to the listen Volcanic eruptions may create lanscapes such as, mountains, plateaus, plains and fertile fields, but on the other hand it may also destroy landscapes. Moreover, volcanoe is a vent which magma divulges due to the pressure on the earth’s surface. Researches have shown that on average, for every cubic kilometer of magma erupts from a volcano as a result 3 to 10 cubic kilometers of molten rock stores in a large underground pool beneath the surface, which is called magma chamber. The molten rock in chamber is suppressed with great amount of pressure, which eventually breaches the rock because it is dense that the surrounding of the rock and makes its way up to the surface of the earth. When the magma erupts from volcano then it’s called lava.
Basically, volcanoes can be found in places where the tectonic plates are diverging or converging....
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...Seismometer can determine if earth quack are migrating toward the surface. Also, some people monitor volcanoes by constantly mentoring gases, which comes out of fumaroles. Additionally, some recent advance technologies can determine a n accurate topography fro the data satellite.
Despite of all the huge devastations caused by the volcanoes, it can directly or indirectly produce mineral such as, gold; is close companion with volcanoes and can be find in three environments: in greenstone belts, porphyry deposits and epithermal deposits. Nickel: deposits of Nickel sulphide are mined from greenstone belts in old volcanic terrenes and its ore is associated with ultra mafic lava called komatiite. After knowing about volcanoes, their structure, nature and formation we can say that they are simply fascinating and are one of the major geological aspects of out planet.
Volcanoes have always been a mysterious wonder of the world. Volcanoes have shaped the landscape and the very ground that we all live on. People have written stories of their disastrous eruptions, and painted their marvelous shapes on canvas. The essay will outline some of the more famous volcanoes and how they have impacted are history. Mount Vesuvius that destroy the great city of Pompeii, Krakatoa they spewed deadly ash on small village town, and Mount St. Helen, the only volcano in my own country to every erupt during my own time period.
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.
Volcanoes can be very deadly but the location can also determine that. Zones are what tells people how dangerous they are. In document c it explains each zone. There are five zones by one being the harshest zone and five being the safe zone. People live in all zones and that's not good at all. Documents C says " There is an area around an active event where likelihood to be killed is extremely high." Volcanoes are always capable of surprises and never up to something good.
Volcanism is a major part of the Galapagos and their formation. The island chain is positioned on the Nazca Plate, which is subducting beneath the South American Plate at a geologically rapid pace of 2.5 inches per year. In addition, this Nazca Plate is located directly on top of the Galapagos Hotspot. It is here that mantle plumes melt Earth’s crust, creating volcanoes as a product. The oldest island was first shaped by this ...
5.) Volcanic Eruptions . (n.d.). Scholastic, Helping Children Around the World to Read and Learn. Retrieved October 8, 2013, from http://www.scholastic.com/teachers/article/volcanic-eruptions
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
Myths and legends are everywhere. There are legends of people from long ago, myths of ancient Greeks. There are myths and legends of almost everything, including volcanoes. Myths of their creation, of why they erupt. Myths and legends of various gods controlling their own volcanoes. There is a story for almost every volcano. The amount of legends and myths concerning volcanoes is quite extensive, ranging from Hephaestus to Vulcan and everything in between. It's very interesting to know what people thought of volcanoes when the myths were made; myths about volcano are as captivating as other myths. Take Pele, one of the gods associated to volcanoes I'll be talking about, for example.
Super volcanoes are formed when magma rises from the mantle to create a scorching reservoir in the Earth's
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.
Convection currents deep in the mantle of the earth, begin to well up towards the surface. As the pressure increases, it sets the crustal plates in motion. There are different kinds of mountains - Volcanic, Folded, Fault-block, and Dome mountains. Volcanic mountains are formed when magma comes up through cracks in the Earth’s crust and explodes out of lava and ash. The Hawaiian volcanoes, Mt. Hood, Mt. Etna, Vesuvius, and Mt. Saint Helens is an example of volcanic mountains.
Volcano geodesists study the inner workings of a volcano, basically, its plumbing. While a physical volcanologist and geochemist can study the results of a volcanic eruption, without knowing the inner workings of a volcano, where the magma chambers are located and which direction they go, it is sometimes difficult to know whether or not an eruption will take place at all (Poland, Hamburger, & Newman, 2006). Geophysicists study the Earth and their research regarding seismology is also crucial to volcanology. Many volcanic eruptions are foreshadowed by clusters of earthquakes. The National Earthquake Hazards Reduction Program and the Volcano Hazards Program, both run by the USGS, monitor the earthquakes and other clues of volcanic activity and release information concerning it.
Our Earth was formed 4.6 Billion years ago. This formation is partly due to the colliding of tectonic plates found under the Earth’s crust. These plates have greatly impacted the way in which the Earth’s outer layer looks and the type of terrain found across its vast surface. One example of these plates at work are volcanoes. Volcanoes are formed through the process of volcanism. This process occurs when “magma- a mixture of molten rock, suspended mineral grains, and dissolved gases formed in Earth 's interior — is forced to the surface.” (Reed,2013) The concept of isostacy is the “ideal theoretical balance of all portions of Earth’s lithosphere as though they were floating on the denser underlying layer is isostacy.” (Reed, 2013) When considering
Igneous rocks are formed from the ejection of earth’s volcanoes. Deep down inside earth’s mantle there lies hot magma. Magma is molten rock that is kept below the surface. This mixture is usually made up of four parts: a hot liquid substance which is called the melt; minerals that have been crystallized by the melt; solid rocks that have made themselves tangled in the melt because of loose materials, and finally gases that have become liquid. Magma is created by an increase in temperatures, pressure change, and a alter in composition. When this magma is ejected from earth’s crust it earns a new name called lava. The lava hardens and becomes an Igneous rock.
Mount Vesuvius is a volcano located in southern Italy, near the bay of Naples and the city of Naples. It is the only active volcano on the European mainland. Vesuvius rises to a height of 1277 m (4190 ft). Vesuvio (Vesuvius) is probably the most famous volcano on earth, and is one of the most dangerous.