Hawaiian Islands
The Hawaiian Islands, once known as the Sandwich Islands, form an archipelago of nineteen islands and atolls, numerous smaller islets, and undersea seamounts trending northwest by southeast in the North Pacific Ocean between latitudes 19° N and 29° N. The archipelago takes its name from the largest island in the group and extends some 1500 miles (2400 km) from the Island of Hawai‘i in the south to northernmost Kure Atoll. The archipelago represents the exposed peaks of a great undersea mountain range known as the Hawaiian-Emperor seamount chain, formed by volcanic activity over a hotspot in the earth's mantle. At about 3,000 km (1,860 miles) from the nearest continent, the Hawaiian Island archipelago is the most isolated grouping of islands on Earth (Macdonald, Abbott, and Peterson, 1984).
References
- Hawai‘i state government, Table 05.09 (.pdf file).
- Macdonald, G. A., A. T. Abbott, and F. L. Peterson. 1984. Volcanoes in the Sea. The Geology of Hawaii, 2nd edition. University of Hawaii Press, Honolulu. 517 pp.
- The Ocean Atlas of Hawai‘i - SOEST at University of Hawai‘i.
~ Table of Content ~
| ► | Introduction |
| ► | Islands and reefs of the Hawaiian archipelago |
| ► | Geology |
| ► | Ecology |
| ► | Climate |
| ► | Tsunamis |
| ► | References |
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