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Physical and human impacts of earthquakes
Earthquakes and their effects
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Question:
What does this type of Scientist Study? What natural phenomena are they interested in learning more about? Answer:
Volcanologists study volcanoes and all its phenomena. One of the phenomena that volcanologists study is pyroclastic flows. Pyroclastic flows are combinations of hot rocks and hot gases. These flows are dangerous because these flows can go at speeds around 50 M.P.H. and their temperatures can range from 392 Fahrenheit to 1300 Fahrenheit. These flows will destroy nearly everything in their path. Volcanologists also study the world underneath our world. They study how the magma flows up and also why it flows up to our surface. Question:
What research/investigation questions do they ask? Why do they ask these questions,
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A volcanologist might ask this question because a usual precursor to a volcano erupting is a sizeable earthquake and change in seismic activity.
Another question a volcanologist might ask is: If this volcano erupts, how will it affect it surroundings? A volcanologist might ask this question because they might have to act quickly if they need to evacuate an area or send a warning out to the local officials etc.
What tools do Volcanologists use? What is the function or purpose of each tool?
A tool a volcanologist may use is a seismometer to track a volcano which could give clues to where magma is along the fissures in the Earth near the volcano. Another tool a volcanologist might use is beakers to collect samples of gas. Change in gas contents may tell a volcanologist way more information than just by looking at the volcano. A volcanologist might learn if more magma is on its way by collect more gases that are found in magma. Carbon dioxide and Sulfur are some of the gases that are most found in magma.
Which words (vocabulary, language) are important for Volcanologists to understand and apply in their study and why?
Term Importance pertaining to
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The Ring of Fire is a region of the earth where volcanoes are very common because of the convergent boundary that resides in that region. The North American Plate and the Pacific plate collide forcing the Pacific plate to be sub ducted beneath the North American Plate. This causes the Pacific plate to melt, thus creating volcanoes along that region. This vocabulary would be important to a volcanologist because A. he would be spending a lot of time over there studying volcanoes and B. he can apply lessons that he learned in the ring of fire to over here in the U.S.
Tectonic Plates There are 7 primary plates in the world, the
African, Antarctic, Australian, North American, Pacific, South American, and Eurasian plates. They are the driving forces behind how volcanoes are formed/ sustained. Magma rushes up from cracks in the mantle formed by tectonic plate boundaries. Volcanologists need to know/ how to apply this information in everyday volcanology life.
Magma Magma is molten rock or in other words, melted rock that bubbles to the surface where there are weaknesses in the crust of the Earth. Volcanologists need to how magma can affect the world outside but also how it’s formed inside Earth to better understand volcanoes. sampling Most of a volcanologists’ work is in the lab or in their office. But on the occasion that they do go to a live volcano, good sample taking of the
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.
Although volcanoes are difficult to predict, geologists have made many efforts in order to caution the people of Orting and other surrounding towns of possible lahar slides. Residents have been made aware of emergency response plans and they know the proper precautions to take in the case of a volcanic activity emergency. Sirens have been put in place by the fire department and governing bodies of surrounding communities to detect volcanic activity and warn the community of possible slides.... ... middle of paper ...
There are many pro’s for attempting to forecast an earthquake or volcano. Forecasting an earthquake or eruption saves lives and property, mainly by preparation, as there is no way to prevent these events with today technology.
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.
Stories about volcanoes are captivating. Myths come in different versions, but all of them are capable of capturing yours, and everybody’s imagination.
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.
The way that these three components interact is one of the main focuses of petrologists and volcanologists.
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.
The ring of fire It runs along the west coast of the Americas Magma forces its way through weak points in the crust, usually at plate boundaries Stratovolcano A. Built from layer upon layer of mostly viscous magma B. Steep sides and very tall C. Mount Vesuvius D. Mount St. Helens Cinder Cone Volcano A. Built from piles of ejected rock fragments B. Steep sides and a cylindrical shape C. Stromboli- Italy Paricutin- Mexico Shield Volcanoes A. Built from layer upon layer of runny lava B. Huge with broad, gently sloping sides
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.
Understanding the plate tectonics theory is very important, especially when investigating natural disasters like earthquakes, and volcanic eruptions. It is also gives scientists the ability to understand how mountains were formed between two tectonic plates. There are three types of interactions between plate boundaries: convergent, divergent and transform. Looking back at the history of these three different interactions, earthquakes, like the one in Haiti, volcanic eruptions, like at Mount St. Helens, and the creation of mountain belts, like the Mid-Atlantic Oceanic ridge, gives information on future consequences of tectonic movement, and what can happen when the plates interact with each other.
The concurrent convective circulations in the mantle leads to some segments of the mantle moving on top of the outer core which is very hot and molten in nature. This kind of movement in different segments occurs as tectonic plates. These tectonic plates are basically seven on the earth surface as major ones, although, several small ones exist also. The plates motions are characterized by varying velocities, this variance results to sub sequential collision of two plates (leading to formation of a mountain in a convergent boundary), drift of two plates (leading to formation of rifts in a divergent boundary), or parallel movement in a transform boundary(Webcache 3).
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.