Island
Types, Examples, & Facts
island, any area of land smaller than a continent and entirely surrounded by water. Islands may occur in oceans, seas, lakes, or rivers. A group of islands is called an archipelago.
Islands may be classified as either continental or oceanic. Oceanic islands are those that rise to the surface from the floors of the ocean basins. Continental islands are simply unsubmerged parts of the continental shelf that are entirely surrounded by water. Many of the larger islands of the world are of the continental type. Greenland (840,000 square miles [2,175,000 square km]), the largest island, is composed of the same materials as the adjacent North American continent, from which it is separated by a shallow and narrow sea. Likewise the world’s second largest island, New Guinea (309,000 square miles [800,000 square km]), is part of the Australian continental platform and is separated from it only by the very shallow and narrow Torres Strait. A slight warping of the sea bottom in the vicinity of Torres Strait would be sufficient to join New Guinea to Australia; conversely, a slight rise in sea level may submerge a hilly coast and leave the hilltops remaining as small islands just offshore (such as those off the coast near Boston and the islands off the Maine coast).
Learn through an animation about the formation of the volcanic island chains like Hawaii and SamoaSee all videos for this article
The islands that rise from the floors of the ocean basins are volcanic. Lava accumulates to enormous thickness until it finally protrudes above the ocean surface. The piles of lava that form Hawaii rise as high as 32,000 feet (9,700 metres) above the ocean floor.
Island life exhibits features of special interest. The sea is a barrier to some forms of life but acts as a carrier of others, which, once established in their new home, frequently develop new features in their isolated surroundings. A long-established sea barrier results in marked differences between the animal life and vegetation even of adjacent islands, and from these differences may be deduced the origin of an island. Further, any detailed map of the biological regions of the globe illustrates the importance of islands in the determination of the boundaries of animal-life and vegetational types. For example, to the west of a line (Wallace’s Line) running between Bali and Lombok and between Borneo and Celebes, the islands are biologically Asian, but to the east of the line, notwithstanding the narrowness of the Lombok Strait, the vegetation and animal life are Australian. Oceanic islands are usually colonized by only a few animal forms, chiefly seabirds and insects. They are often covered with abundant vegetation, the seeds of which have been carried there, for example, by air and water currents or by birds; but the plant variety is relatively limited.
A list of the world’s largest islands is provided in the table.
name
location
area*
sq mi
sq km
*Area given may include small adjoining islands. Conversions for rounded figures are rounded to the nearest hundred.
Greenland
North Atlantic Ocean
822,700
2,130,800
New Guinea
Papua New Guinea–Indonesia
309,000
800,000
Borneo
Indonesia–Malaysia–Brunei
283,400
734,000
Madagascar
Indian Ocean
226,658
587,041
Baffin Island
Northwest Territories, Can.
195,928
507,451
Sumatra
Indonesia
167,600
434,000
Honshu
Japan
87,805
227,414
Victoria Island
Northwest Territories, Can.
83,897
217,291
Great Britain
United Kingdom
83,698
216,777
Ellesmere Island
Northwest Territories, Can.
75,767
196,236
Celebes
Indonesia
69,100
179,000
South Island
New Zealand
58,676
151,971
Java
Indonesia
49,000
126,900
North Island
New Zealand
44,204
114,489
Newfoundland
Canada
42,031
108,860
Cuba
Caribbean Sea
40,519
104,945
Luzon
Philippines
40,420
104,688
Iceland
North Atlantic Ocean
39,699
102,819
Mindanao
Philippines
36,537
94,630
Ireland
Ireland–U.K.
32,589
84,406
Hokkaido
Japan
30,144
78,073
What's Your Reaction?