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Hawaiian Island Chain The Hawaiian Islands 1,500 miles (2,400 kilometers) form a chain that is stretched to the northwest and southeast. It has heaps of rocks from different Islands in the Hawaiian island chain that show that the islands are progressively older to the northwest: Oahu, 3.4 to 2.2 Millions of years; Molokai, 1.8 to 1.3 Millions of years; Maui, 1.3 to 0.8 Million years; and the Big Island (Hawaii which is less than 0.7 growing (Punagridge n.d) The Hawaiian Islands are volcanic in Origin. Each island is made up of at least one primary volcano, but many islands are merged to one another. (Smithsonian 2009) The Hawaiian Island Chain is a hot spot. Which is a plume of magma or molten rock that rises from within the Earth. It reaches the surface forming underwater volcanoes which may grow tall enough to rise above the sea to form islands. In the middle of the Pacific Ocean, the Hawaiian hotspot remains stationary while the Pacific plate slowly moves overhead to the northwest. Bugielski, M. (1999). The area directly over the hot spot is volcanically active. The activity decreases and eventually stops as the plate moves on. Allaby, M (2007) The Hawaiian Islands are at the southeastern end of a chain of volcanoes that began to form more than 70 million years ago. Many of the volcanoes formed islands that have decreased and eroded beneath sea level, and some of the old volcanoes probably never reached sea level. (Ken Rubin 2013) Each Hawaiian island is made of one or more volcanoes, which first erupted on the sea floor and only appeared above the ocean's surface after numerous eruptions. (Ken Rubin 2013) Figure 3: Map of Hawaiian Island Chain (Punaridge n.d)
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