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Geology of the Ross of Mull, Iona and Staffa - Term Paper Example

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The author of the "Geology of the Ross of Mull, Iona and Staffa" paper reviews the published geologic literature of the Ross of Mull including the Islands of Iona and Staffa. This natural sight of Scotland, located in the Inner Hebrides, is the second-largest island in that region.  …
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Geology of the Ross of Mull, Iona and Staffa
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Download file to see previous pages The Ross of Mull is the main point of concentration. It is the largest peninsula on the island, filled with prehistoric geographical features that represent various geological events that took place millions of years ago. This includes steep cliffs of lava in the north and large mountainous roots in the south, which show clear proof of high volcanic activity in this region at some point in time in the past. Such is the sheer contrast of this region, that there are sandy beaches as well as hard granite deposits in this same region (Wilson 392).

The entire geography of the Ross of Mull depicts various prehistoric activities that will help geologists understand the movement of landmass, tectonic plates and volcanic activity in the European and North Atlantic region which has resulted in the current formation European geography. It has become a haven for geologists in investigating the long lost past and helps them portray and predict future movements and activities. Activities that will further change the shape of Europe and the world as we know it.

The island of Staffa has been the result of pure landmass formation due to magma. The entire island covers an area of about 33 hectares and is located north side of the Ross of Mull. It is an island that used to be part of the Isle of Mull; however, it was later separated. By looking at its geography, it looks like a huge cliff when observed from the southern side; however, the island shelves into the ocean on the northern side. The island has been the result of pure volcanic formation, as it is clearly visible in its existence (MacArthur 63).

The island has the formation of a cliff on its southern side as seen from the Ross of Mull. The cliff walls are made from fine tertiary basalt; however, underneath the basalt columned edges are basements of tuff, formed by pure volcanic ashes. However, these are not the main point of attractions of the island. The island is most famous for its caves, located on its far-east and west coast.   ...Download file to see next pagesRead More
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