Mt.Vesuvius and its 79 AD Eruption Essay -- essays research papers

Vol bearo A agglomerate or mountain form around and above a vent by accumulations of erupted materials, such as modify, pumice, cinders or lava-flow. The term refers both to the vent itself and to the much cone-shaped accumulation above it. (Scarth, 1994.) This definition can do Mt. Vesuvius no justice. Instead, I would describe it as one of the most hellish and population decimating volcanoes. Vesuvius livesor lived In its prime, Vesuvius covered and demolished two of Italys biggest cultural and artistic cities of its time. In this paper, I provide be discussing volcanoes in general. In addition, Mt. Vesuvius, in particular, give be thoroughly looked at, as well as its 79 AD eruption.Volcanoes have long been render as natures killer. In movies, Volcanoes are seen as mountains of fire and spitting lava their only purpose seems to be to kill and destroy ein truththing in their path. neer is the background of volcanoes discussed. How are volcanoes formed? Are in that location different types of volcanoes? What happens during an eruption? The basic questions to aid understanding of volcanoes might change the publics opinion. First, I will begin with the creation of volcanoes. Volcanoes are formed in different ways. In a short version the earths plates shift and move. aft(prenominal) the plates collide into each other, one plate is pushed master into the mantel below the crust and melts. Hot magma from the mantle breaks through a weak spot in the crust. As the Ziehm 2magma shoots out of the crust, the cooling magma called lava becomes hard. subsequently significant time, the hard lava forms a volcanic mountain. Volcanoes can form in many different sizes and shapes. They can look like a cone, have tincture looking flanks, or look as if they were long cracks in the earths crust. (Plummer et al., 2000). If the mountain is very tall, then there is a greater gamble that it was formed from past eruptions. When the lava cools, it makes the mountain bigger a nd higher. Depending on the type of volcano, layers can differ in lava/ash content. (Plu... ...pZiehm 6Mt.Vesuvius is just one of several officious volcanoes throughout the world. They have wiped out populations in the past and have the potential to decimate more in the future. Geologists are predicting that a volcanic eruption will occur that will dwarf eruptions such as Vesuvius and Mt. St. Helens. (http//www.ph_heidelburg.de/stud/EGGERTT/vesuvio.html) The only thing we can do is sit and waitnature will resume its course. List of RefrencesMorris,C. 1902 The Volcanos Deadly Work From the Fall of Pompeii to the Destruction of St. Pierre. The Dan Waugh Collection of Nature Books. Washington, D.C. 236-254.Plummer, C.C., McGeary, D. & Carlson, D.H., 2000 material Geoloy. Updated eigth ed..Mcgraw-Hill Companies, Inc., NY. 81-82,88-89. Rittman, A & L. 1976 Volcanoes. G.P. Putnams Sons, NY. 20-22Scarth, A.1994 Volcanoes An Introduction. Texas A&M University extract College Station. 5 6-57, 74, 259. http//www.volcano.und.nodak.edu http//www.harcourtschool.comhttp//www.ph_heidelburg.de/stud/EGGERTT/vesuvio.html Mt.Vesuvius and its 79 AD Eruption Essay -- essays research papers Volcano A hill or mountain formed around and above a vent by accumulations of erupted materials, such as ash, pumice, cinders or lava-flow. The term refers both to the vent itself and to the often cone-shaped accumulation above it. (Scarth, 1994.) This definition can do Mt. Vesuvius no justice. Instead, I would describe it as one of the most hellish and population decimating volcanoes. Vesuvius livesor lived In its prime, Vesuvius covered and demolished two of Italys biggest cultural and artistic cities of its time. In this paper, I will be discussing volcanoes in general. In addition, Mt. Vesuvius, in particular, will be thoroughly looked at, as well as its 79 AD eruption.Volcanoes have long been depicted as natures killer. In movies, Volcanoes are seen as mountains of fire and spitting lava their only purpose seems to be to kill and destroy everything in their path. Never is the background of volcanoes discussed. How are volcanoes formed? Are there different types of volcanoes? What happens during an eruption? The basic questions to aid understanding of volcanoes might change the publics opinion. First, I will begin with the creation of volcanoes. Volcanoes are formed in different ways. In a short version the earths plates shift and move. After the plates collide into each other, one plate is pushed down into the mantel below the crust and melts. Hot magma from the mantle breaks through a weak spot in the crust. As the Ziehm 2magma shoots out of the crust, the cooling magma called lava becomes hard. After significant time, the hard lava forms a volcanic mountain. Volcanoes can form in many different sizes and shapes. They can look like a cone, have steep looking flanks, or look as if they were long cracks in the earths crust. (Plummer et al., 2000). I f the mountain is very tall, then there is a greater chance that it was formed from past eruptions. When the lava cools, it makes the mountain bigger and higher. Depending on the type of volcano, layers can differ in lava/ash content. (Plu... ...pZiehm 6Mt.Vesuvius is just one of several active volcanoes throughout the world. They have wiped out populations in the past and have the potential to decimate more in the future. Geologists are predicting that a volcanic eruption will occur that will dwarf eruptions such as Vesuvius and Mt. St. Helens. (http//www.ph_heidelburg.de/stud/EGGERTT/vesuvio.html) The only thing we can do is sit and waitnature will take its course. List of RefrencesMorris,C. 1902 The Volcanos Deadly Work From the Fall of Pompeii to the Destruction of St. Pierre. The Dan Waugh Collection of Nature Books. Washington, D.C. 236-254.Plummer, C.C., McGeary, D. & Carlson, D.H., 2000 Physical Geoloy. Updated eigth ed..Mcgraw-Hill Companies, Inc., NY. 81-82,88-89. Rittman , A & L. 1976 Volcanoes. G.P. Putnams Sons, NY. 20-22Scarth, A.1994 Volcanoes An Introduction. Texas A&M University Press College Station. 56-57, 74, 259. http//www.volcano.und.nodak.edu http//www.harcourtschool.comhttp//www.ph_heidelburg.de/stud/EGGERTT/vesuvio.html