WiseDude.com
The Formation of Islands

 
     
 

 

Home

 

Animals

 

Art & Music

 

Business and Economy

 

Classic Books In Short

 

Computers

 

Expert Advice

 

Food

 

Health and Medicine

 

History

 

Inventions and Discoveries

 

Personal Finance

 

Personalities

 

Science and Engineering

 

Sports

 

Miscellaneous

   
 

Google
 

Web

WiseDude.com

How Are Islands Formed?

Without islands there would not have been a Robinson Crusoe nor would lovers dream of being marooned on them for eternal romance. Let’s see what these little pieces of romance in the sea are.

An Island is… 
There are three natural phenomena that result in the formation of islands. And the three types of islands that result from such natural events are coral islands, islands from mountains and islands resulting from volcanic eruptions. 

Coral Reefs
The chalky skeletons of billions of tiny animals that lived in the shallow tropical water get locked together to form huge coral reefs. Some coral islands, such as the Maldives in the Indian Ocean and the Great Australian Barrier Reef, are actually tips of such reefs formed during periods of warmer climate, when the polar ice caps were smaller and the sea levels higher.   

   

By studying these coral islands scientists were able arrive at the possible weather conditions prevalent centuries ago. Based on the fact that unfavorable conditions such as cold periods result in darker corals, marine biologists in Florida have identified the years when there were cold fronts, storms and radioactive fallout from nuclear weapon tests. For this, scientists studied layers in ten feet cores or coral in Florida.

Picture of a Coral Reef
A Coral Reef

Volcanic islands
Islands like the Hawaii and the Surtsey (off Iceland) are some examples of volcanic islands. Eruption of volcanoes from weak points in the Earth’s crust have created such islands. When there is a volcanic explosion, molten rock and ash are forced up from the seabed. Once out, they form a cone shaped island. These islands are surrounded by vapor from the vent of the volcano.  Gradually, sea waves eat into the island and wear down the cliffs, forming a platform on which coral grows. In due course, the main vent cools, however a lesser one remains active, which results in crumbling rocks, that form soil. Plants and animals slowly start inhabiting these cooled platforms. However, as a lesser vent remains active, erosion continues to occur now and then, resulting in offshore stacks. Over a period of time the island sinks, with only a tip of the original cone shaped island on the ocean’s surface.

Krakatoa is an Indonesian island volcano, which erupted in 1883. The ash and pumice erupted wiped out all life on the island. However, the island was re-colonized at an amazing speed. It is said that exactly nine months later, a solitary spider was seen spinning a web. Three years later, naturalists claimed that they had located eleven species of ferns and fifteen varieties of flowering plants on the island.

Forty years later, Krakatoa was covered with lush forest and was home to one thousand two hundred species of animals, including pythons and bats.

The loneliest island in the world is said to be a volcanic island called Tristan da Cunha, near Britain. The nearest land is two thousand and twenty kilometers away from Tristan.  


After a volcanic eruption in 1961, the inhabitants were moved to Britain. However, many returned to the island a few years later, unable to cope with the hectic pace of urban life.

Mountain islands
When rising temperatures marked the end of the Ice Age about ten thousand years ago and sea levels rose by more than a hundred meters, many mountains were submerged. The tips of these submerged mountains formed islands. The Hebrides off the north-west coast of Scotland is an example of mountain island.

Home  |  About Us    |   Contact Us   |   FAQs  |  Disclaimer    |    Donations

 



Copyright © 2006 WiseDude.com. All rights reserved.
No article may be republished without permission.