• Join over 1.2 million students every month
  • Accelerate your learning by 29%
  • Unlimited access from just £6.99 per month

Discuss the degree to which the theory of plate tectonics is supported by seismic and volcanic activity

Extracts from this document...

Introduction

Discuss the degree to which the theory of plate tectonics is supported by seismic and volcanic activity. The theory of plate tectonics suggests that the earth's lithosphere is split into plates (as shown in map 1). At their boundaries the plates submerge, diverge and slide past one another, this movement is caused by convection currents in the asthenosphere. The idea that the plates are moving is not new, as early as 1620 the English philosopher Francis Bacon was aware that the continents seemed to fit together. In 1912 Wegener suggested that the continents were once joined as the super continent Pangaea (as seen in image 4) and that they had drifted apart, he gathered a large amount of evidence to support this theory. Continents appear to fit together, more significantly so if continental shelves are taken to be the true edges of the land mass. There is a vast array of geological evidence that includes similar glacial deposits being found in Antarctica, S. America and India. Antarctica, Svalbard, N. America and the UK all contain coal deposits of a similar age that were formed in tropical conditions, they are no longer in tropical climate zones. Biological evidence is also available, Marsupials are only found in Australia because the predator that wiped them out elsewhere had not migrated there before it drifted away from the main super continent. ...read more.

Middle

On the other hand, not all volcanoes are found at plate boundaries (as can be seen in map 2 above). For example, Hawaiian islands which are completely volcanic in their origin, were formed in the middle of the Pacific Ocean, at least 3,200 km from the nearest plate boundary. It is believed that these islands were created as the plate moved over a hot spot. Hot spots seem to be stationary and are thought, by some geologists, to be caused by plumes of magma originating deep within the mantle, others believe they occur at much less depth, and are moving slowly. Another hypothesis suggests that the volcanic activity is not caused by the temperature but by a certain level of thinning in the lithosphere due to its extension, that allows the rising of melt from shallow depths. As volcanic material erupts through the oceanic crust, over time it may build up to form an island. These islands will however, become part of the plate and gradually move away from the heat source. New volcanoes will form over the hot spot, and a new island is created, this can lead to an island chain, if the plate is moving in one direction over the hot spot such as the Hawaiian chain (an illustration of how such a chain might occur can be found above in figure 6). ...read more.

Conclusion

Like volcanoes, it is also possible for earthquakes to occur away from plate boundaries. Where plate boundaries occur within continental crust, faults are spread out over a much larger area than the plate boundary itself. In the case of the San Andreas Fault, many earthquakes occur away from the plate boundary and are related to strains developed some distance away, caused by major irregularities in the fault. Far from plate boundaries complex strata can result in deep fault zones which can result in earthquakes in apparently stable regions. Earthquakes in China and central Asia occur along lines of weakness, related to the collision of India with the Eurasian plate over 50 million years ago. Ninety percent of all earthquakes occur along plate margins and by far the greater amount of energy released as seismic waves comes from subduction zones. Furthermore, the depths of earthquakes are consistent with the idea of oceanic recycling by subduction and sea-floor spreading. The 10 percent of earthquakes that do not occur at plate boundaries are sufficiently explained by extended lines of weakness and the theory of their cause is sufficiently supported by necessary evidence. The majority of volcanoes also occur at plate boundaries, due mainly to subduction of an oceanic plate, but those that do not, are adequately explained by the presence of hot spots. In conclusion, though not strictly located at plate margins, the distribution of volcanic and seismic activity across the globe supports the theory of plate tectonics. ...read more.

The above preview is unformatted text

This student written piece of work is one of many that can be found in our AS and A Level Hazardous Environments section.

Found what you're looking for?

  • Start learning 29% faster today
  • 150,000+ documents available
  • Just £6.99 a month

Here's what a teacher thought of this essay

5 star(s)

This is an excellent answer for an A level student. The author has a sound understanding of the topic, and has an awareness of what the question requires. Use of technical terms is generally very good, and relevant examples are well-explained. In a few places a little more explanation would improve the answer. Overall worth *****

Marked by teacher Nigel Fisher 16/02/2012

Not the one? Search for your essay title...
  • Join over 1.2 million students every month
  • Accelerate your learning by 29%
  • Unlimited access from just £6.99 per month

See related essaysSee related essays

Related AS and A Level Hazardous Environments essays

  1. Describe and explain the global distribution of volcanoes and earthquakes.

    the Philippines). A series of these islands form an island arc. The global distribution of earthquakes is similar to that of volcanoes. By and large, the distribution of earthquakes divides the earth's surface into a number of areas that are aligned very well with plate boundaries.

  2. Describe the global distribution of earthquakes.

    Thus, a 7.0 earthquake is ten times more powerful than a 6.0 and 100 times more powerful than a 5.0. To allow a greater degree of precision, a decimal equivalent was provided. At one time it was believed that an earthquake with a magnitude of 8.5 was the most powerful

  1. OUTLINE THE EVIDENCE TO SUPPORT THE THEORIES OF PLATE TECTONICS & CONTINENTAL DRIFT

    evidence of glaciation in Brazil and India and also rocks which could not have been formed under current conditions have been found in Britain. All these pieces of evidence have pointed towards the continents once being joined or by having some sort of bridge between them.

  2. The hazards presented by volcanic and seismic events have the greatest impact on the ...

    The US volcanologist office warned the local authorities about the impending eruption but the authorities did not understand the seriousness of the situation and so did not warn any of the people. 28000 people died from the eruption and the secondary effects of the mudslides and lahars that formed.

  1. Free essay

    To what extent do the causes of mass movement hazards depend more on human ...

    For example, on slopes where recreational activities occur, such as walking and climbing on mountains, damage the slope over a long period of time, and the damage gradually gets worse. Farming the land also damages the land and destabilises the slope as the ground is constantly being tampered with.

  2. Seismic waves.

    An S wave is slower than a P wave and can only move through solid rock. This wave moves rock up and down, or side-to-side. The arrow shows the direction that the wave is moving. Surface Waves Love Waves The first kind of surface wave is called a Love wave, named after A.E.H.

  1. Evaluate how plate tectonics theory helps our understanding of the distribution of seismic and ...

    This means that plate tectonic theory can therefore explain the prevalence of earthquakes along the San Andreas fault line where the Pacific and North American plates move past each other, most notably the San Francisco earthquake in 1989. Additionally, the theory can help us to understand why volcanic activity does not occur in this area, but seismic activity does.

  2. To what extent has the management of volcanic activity on Montserrat been successful?

    Despite the success in certain aspects of short term and long term management, there were particular areas which were not so successful. After the prompt evacuation in August and December 1995 the residents of the South were allowed to return putting their lives in danger in January 1996 as two

  • Over 160,000 pieces
    of student written work
  • Annotated by
    experienced teachers
  • Ideas and feedback to
    improve your own work