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Since the beginning of modern science, volcanoes have drawn the attention of scientists around the globe. However, it wasn’t until about 25 years ago that our understanding of the physical and chemical processes that drive volcanic eruptions increased drastically. Due to our advances in geochemical and petrological sciences, we have been able to more accurately conclude as to why and how a volcano erupts. As a generalization, volcanologists primarily focus on the science behind how magma forms and moves to Earth’s surface, and how the specific chemical properties of magma (and the lithosphere though which it moves) contribute to eruptive activity. Volcanic ash is also significant in the volcanology, differing slightly with each eruption. Different eruptions possess different properties, such as composition and thickness of the erupting magma, the force of the eruption, and what gases are present, that make each eruption unique (3).
Magma
In order for a volcanic eruption to occur, a substance known as magma must be present. Magma often collects in magma chambers (directly below the volcano) that feed a volcano. Magma consists 96% of molten, or liquid, rock, due to the extremely high temperatures (1300 °F to 2400 °F) located in the Earth’s mantle(4). This molten rock contains very many solids known as “rock forming silicate minerals,” such as carbon, iron, silicon, aluminum, and magnesium, as well as many others. While a large portion of magma is made up of these substances, magma also contains various volatiles that play an extremely vital role in a volcano’s eruption. Volatiles are substances with low melting points that are released as a liquid or gas when an eruption occurs, such as water, carbon dioxide, and sulfur dioxide ...
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Each aspect of a volcanic eruption plays a significant role when observing the various chemical properties of a volcano. Each phase (magma’s ascent into the magma chamber in the upper crust, migration toward Earth’s surface, eruption, and volcanic plume) requires a specific chemical balance in order to occur. However, although each volcanic eruption is chemically similar, each one is miraculously unique. These complex interactions only fuel the need for continued advances in our understanding of both the physical and chemical aspects of the entire volcanic eruption sequence. Volcanoes are destructive yet beautiful landforms beckoning to be explored by today’s and tomorrow’s volcanologists and geochemists. Although volcano science has exploded in the past 25 years, there are still vast amounts of information to be learned about the chemistry of volcanoes.
Many of us know Mount Shasta to be a beautiful mountain and a popular tourist location in California. However, this mountain is much more than that, this mountain is actually a volcano. Volcanoes come with a number of hazards and a volcano of this size is of no exception. Previous eruptions on Mount Shasta have given us an idea of the power this volcano has and the damage it may do. With this information scientists are able to predict what may happen should another explosion occur.
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...
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.
From modern examples and records we know that volcanic activity can set of a chai...
Stories about volcanoes are captivating. Myths come in different versions, but all of them are capable of capturing yours, and everybody’s imagination.
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...
4.) Volcanic Explosivity Index. (n.d.). Wikipedia, the free encyclopedia. Retrieved October 7, 2013, from http://en.wikipedia.org/wiki/Volcanic_Explosivity_Index
Super volcanoes are formed when magma rises from the mantle to create a scorching reservoir in the Earth's
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.
A geochemist can also determine the chemical makeup of these deposits. By studying deposits and lava flows from past eruptions, it can assist in the prediction of where the lava will flow, how far the debris field will be and how far the ash will scatter in new eruptions. As retired volcanologist Robert Tilling so aptly described it, "the present is the key to the past – In a sense, we’re detectives, trying to decipher clues that rocks tell us.” (What does a volcanologist do?, n.d. para. 1). The adage of the adage.
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.
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.