Plate tectonics and continental landmass changes

¶ … plate tectonics is responsible for changing continental landmasses through geological occurrences.

Thousands of years ago the earth's surface has been hypothesized as one big landmass. The Earth's surface has been constant motion. "Fragmented into giant sheets of solid rock that glide atop a layer of hotter, more pliable material, the globe's appearance is forever changing." [Cowen, 1999]. These plates are semi-rigid, floated on flow of mantle. The plates measured around 50 miles, thickness of 25 miles on land and 4 miles thick under the oceans. Their movement was categorized by an average of a few inches a year. Even today, geologists and tectonicists hypothesize the earth to continue this movement in similar slow manner, even if we do not notice it. The plates' movement is called the Plate Tectonic Theory, a theory presented in 1912 but upheld in 1960.

STATEMENT OF PURPOSE

The main controversy in the Plate tectonic theory is that whether the movement of the plates has displaced landmass across the continents or not and whether it is the sole reason for the change of the landmass or it is through atmospheric influence. This paper will help explain how Plate Tectonics has caused changes in continental landmasses through geological occurrences.

ANALYSIS

Plate Tectonics

The concept of plate tectonic is derived from moving plates or the earth crust from its original location to some other parts of the world. The dynamic system of the plate tectonic have been responsible for the huge recycling system of the earth, by spreading the centers, thrusting the crust down and melting the mantle to increase or subdue some parts of the crust to change the surface [Austin et al., 1994].

Most plate tectonics evidence is found where volcanic eruptions or earthquakes occur. The chances of the formation of crust from the earthquakes is often embedded in the ocean floor as molten rocks, rising out into the surface when the plates are separated from the crust and not as a result of deposits. For example in areas around the Mid Atlantic Ridge, the plates are seen to have drifted apart but new oceanic crust is formed when molten rocks rise from the mantle [Price, 1999]. The Western side of South American is another example of change of land surface where the boundary of two plates comes together to form a heavier crust. When this occurs, it forces the landmass to depress, under the lighter continental crust. A similar example of landmass changes is the San Andreas Fault, belonging to the North American Plate and Pacific Plate. In this case the stick slip motion of the plates is responsible for the eruption of earthquakes in California. Yet another instance of plate tectonic is the boundary in the Himalayas. The mountains are uplifted from the impact of the Asian Plate and the Indian sub-continent.

Scientists around the world however dispute the existent evidence of the hypothesis that the landmass formations of the continents are the results of plate tectonics. For instance it has been said that this theory is "A hypothesis that is appealing for its unity or simplicity acts as a filter, accepting reinforcement with ease but tending to reject evidence that does not seem to fit" (Pratt, 2000). The argument posit that although the logic flow of the plate tectonic do give convincing evidence, but it cannot "over ride and over rule all other hypothesis" (Pratt, 2000) which pose the argument that the disturbing dogmatism of atmospheric development responsible for the change, tearing and wearing of the earth's surface.

To understand the evidence one must delve into the structure, conception of plate tectonics before accepting it wholly. Hence, the following arguments attempt to present the factual evidence of the earth's change of landmass and attribute to plate tectonics.

Types of Plate Tectonics

Plate boundaries are identified and defined mainly on the basis of earthquake and volcanic activity. The close correspondence between plate edges and belts of earthquakes and volcanoes is therefore to be expected and can hardly be regarded as one of the "successes" of plate tectonics" (McGeary and Plummer, 1998 qtd. From Pratt 2000).There are three types of plate movements that are recognized at the boundaries of the plates. These are known as convergent, divergent and transform-fault.

Convergent boundaries of plates move toward each other and collide. When continental plates collide with each other, they usually form mountain chains. Take for instance the case of Himalayas, where the oceanic plates of South America and Nazca Plate boundaries collided and formed what is called subduction of the boundaries.

In the case of divergent boundaries, the continental plates move in opposite directions. For instance the Mid Atlantic Ridge whose plates "diverge" lava rocks which later cooled to add more substance to the edges of the oceanic plates [Monastersky, 1999]. This process is also known as sea floor spreading, where the ocean bed decrease its height by increasing its mass [Harish, 2001].

In some cases the plates move past each other without any kind of collision. This is known as the transform fault boundaries. An example of the transform fault is the San Andreas Fault zone where the boundary of the Pacific Plate that categorize Los Angeles move slowly northward towards the North American plate to San Francisco but it does not collide. Due to these actions, the plate tectonics is considered to be the major contributor to landmass change.

When plate tectonic occurs it is common to have different kind of results. In that the different movement of the geological layers often result in different kind of reaction in the earth's surface. The movement of convergent, divergent and transform fault are all instances of such differential geological reaction. These are divided into subduction, sea floor spreading and continental drift.

Continental Drift

However, if the above was the case then how can scientist justify the hypothesis for continental drift. According to Ann G. Metzger and Jill Stevens Johnston of Center for Earthquake Research and Information, University of Memphis [1998], plate tectonics is the basis of reasoning for the theory of continental drift. This theory believes that around 175 million years ago the surface of the earth was one large mass of land. Despite the differential in opinions among scientists regarding the formation of the landmass of today, all have conjugate in their opinion on the fact that rock formation, geological distribution of these rocks as well as the different evidence of land support like earthquake, faulting and folding and ocean floor spreading cannot be reasoned if plate tectonic is ignored. Some rock composition may have changed but the overall layers and connection of rock formation from continent to continent are similar. One explanation for difference in composition is that the plates have collided into each other several times before it came to its present state.

The earth and its contraction of the different layers of crust cannot be treated as pieces of puzzles and according to the "best fit" theory. Since it is hypothesize that the landmass had collided several times, it is not necessary that each and every puzzle corner should match the other. It is not necessary that the east coast of Brazil in South America should match those of southwestern coast of Africa, nor does it mean that the North eastern coast of American match with Western Europe. The very fact that the plates are different in its boundaries, its fossils and rock geological composition show that these boundaries have been subjected to extreme force, collision and deterioration. Using the puzzle method would not give the desired answer. Instead, the plate tectonic theory provides the best answer for the different kind of life form common to most of the plates on earth. Fossil rocks for instance is the evidence of this theory. During the paleonthic age for instance coastlines of the continents were the hubs for changing landscape. Animals living in these areas, evident from fossils, migrated to different plates for survival. These fossils show the trace of the changing landmass [Tarbuck and Lutgens, 1984]. The magnetic traces of the rocks and its minerals for instance characteristics of volcanic or molten rocks all show the how rocks cooled, their particles dispersed to various levels and areas of the plate. When the plates collided the rocks got displaced but their composition remained in tact even though they became part of different landforms like mountains, ocean floor or valleys depending on how forceful the impact of the tectonic was. In America the evidence of such changing landmass is evident in the Ouachita Mountain folds, where the ocean crust meets the continental crust. Similar evidence of continental shifts is evident by the faulted sheets of land, overriding the land of the Northern area. When this process occurs, often the rocks crack and collide with new sets of mountains, displacing sedimentary layers to another level and hence form mountains, plateaus and uplifts.

There is no doubt that weathering and atmospheric pressure act as the changing factor for the landmass. However, unless the landmass itself changes, fragments of the whole landscape cannot change so drastically. For instance in North America the ocean floor gets shallower and the South America plate gets closer to the north is not the result of weathering. A shift of the landmass of this nature could only be attributed to plate tectonics. Even though the movement is slow but it is evident that the movement have been going on since age old. The traces of sedimentary rocks, the squeezed rock walls through folds as well as the fragments resulting from faulting all contribute to change in geological change. Unless large sheets of land over ride each other, one cannot really say that the formation of such geological composition the result of some weathering or even change in mantle level. Indeed the change of such massive nature through cracks, faults and folds could only be done through tectonics.

In this regard tectonicists admit that although the velocity of the movement is slow but it nevertheless exist. Furthermore, the argument that the lithosphere is thick and the plates cannot move with such speed is baseless since the plates glide above the plastic flow of the mantle and does not depend on the depth of the earth's crust. "Plate tectonicists expected seismic tomography to provide clear evidence of a well-organized convection-cell pattern, but it has actually provided strong evidence against the existence of large, plate-propelling convection cells in the upper mantle" (Anderson, Tanimoto, and Zhang, 1992 qtd. From Pratt 2000). It is through this reasoning that one come to the conclusion that the motion of plate could only be the sole reason for the shallow and deep mantle depths when the plate move to and fro, flowing over the surface of the mantle (McGeary and Plummer, 1998 qtd. From Pratt, 2000).

CONCLUSION:

From the above discussion the author concludes that plate tectonics, its activities having survived thousands of years are responsible for the changing landmass. Their movement have resulted in collision and displacement of the earth's crust so that the geological composition of the different land area have integrated and stretch far and wide. Today one finds this changed mixture of geological composition is responsible for the different areas, landmass and rocks types. The reason why the landmass do not resemble each other in some instance is because the tectonics have often resulted forceful folds, faults and transform fault that it has mixed up the different layers of the earth. As a result of this, the earth today vaguely resemble the large plate that it once was.

ENDNOTES:

Cowen, Ron. Plate Tectonics... On Mars. Science News, May 1, 1999.

Cowen, 1999

Austin, S., Baumgardner, J., Humphreys, D., Snelling, A., Vardiman, L., Wise, K., "Catastrophic Plate Tectonics: A Global Model of Earth History," Proceedings of the Third International Conference on Creation, Edited by Robert E. Walsh, Creation Science Fellowship, Inc., Pittsburgh, 1994, pp. 609-621.

Baumgardner, J., "3-D finite element simulation of the global tectonic changes accompanying Noah" Flood," Proceedings of the Second International Conference on Creation, Edited by Robert E. Walsh, Creation Science Fellowship, Inc., Pittsburgh, Vol. 11 pp. 35-45, 1990.

Price, Jonathan G. Geology of NEVADA. Rocks & Minerals, Nov, 1999.

Monastersky, Richard. Is the Pacific plate tearing itself apart? Science News, Sept 5, 1998.

Baumgardner, 1990.

Pratt, David. Plate Tectonics: A Paradigm Under Threat. Journal of Scientific Exploration, vol. 14, no. 3, pp. 307-352, 2000.

Macdonald, G.A. Volcanoes. Englewood Cliffs, N.J.: Prentice-Hall. 1972.

Rodgers, J. Life history of a mountain range. In Mountain building processes, ed. By K.J. Hsu, 229-41. New York; Academic Press. 1982.

Harish, Nir. Ground Control. The Sciences, Spring, 2001.

Monastersky, R. A Stirring Tale from inside Earth. Science News. March 20, 1999.

Harish, 2001.

Monastersky, 1998.

Monastersky, 1999.

Austin, et al. 1994, pp. 609-621.

Zimmer, Carl, GEOPHYSICS: Ancient Continent Opens Window on the Early Earth., Science, 12-17-1999.

Blood, Peter R. Sri Lanka: Chapter 2A. Society and its Environment., Countries of the World, 01-01-1991.

Monastersky, 1998.

Baumgardner, 1990.

Austin, 1994, pp. 609-621.

Metzger, Ann G. And Stevens, Jill. Johnston Earthquake Risk in the New Madrid Seismic Zone, Rockhounding Arkansas revised October 1998 Center for Earthquake Research and Information, University of Memphis.

Wieland, C., and Batten, D., "Interview with plate tectonics expert Dr. John Baumgardner," Creation ex-nihilo 19(3)41, 1997.

Wieland, 1997.

Tarbuck, E., and Lutgens, F., The Earth: An Introduction to Physical geology, 2nd ed., Merrill Publishing Co., Columbus, based on drawings found on pp. 380 & 386, 1987.

Cowen, 1999

Blood, 1991.

Van Diver, B. Roadside geology of New York. Missoula: Mountain Press Publishing Co. 1985.

Blood, 1991.

Doolan, Barry, The geology of Vermont.. Vol. 71, Rocks & Minerals, 08-01-1996, pp 218.

Zimmer, 1999.

Pratt, 2000.

Tarbuck, 1987.

Doolan, 1996, pp 218.