Hawaiian Islands
From west to east, Hawaii is made up of the following Hawaiian Islands:
The chain of islands stretches 2,400 km (1500 miles) in a southeasterly direction to the southern tip of the Island of Hawaii The hot-spot which formed them moved South-East in the Pacific Ocean. The hot-spot in the Earth's crust moved to where it is now, near the island of Hawaii, or, rather, the hot spot stayed where it was, and the plates of the Earth's crust moved, so creating the islands.
Hawaii has been a U.S. state since 1959.
The Hawaiian islands, plus former islands now below sea level (guyots), make up the Hawaiian–Emperor seamount chain.
Hawaiian Islands Media
Aerial view of Lēʻahi or Diamond Head, Oʻahu
A composite satellite image from NASA of the Hawaiian Islands taken from outer space. Click on the image for a larger view that shows the main islands and the extended archipelago.
Eruptions from the Hawaii hotspot left a trail of underwater mountains across the Pacific over millions of years, called the Emperor Seamounts.
Aftermath of the 1960 Chilean tsunami in Hilo, Hawaiʻi, where the tsunami left 61 people dead and 282 seriously injured. The waves reached 35 feet (11 m) high.
Death of the first European visitor to the Hawaiian Islands, Captain James Cook, at Kealakekua Bay on February 14, 1779