Geography
Enewetak Atoll formed atop a seamount. The seamount was formed in the late Cretaceous (about 75.8 million years ago). This seamount is now about 4,600 feet (1,400 m) below sea level. The seamount is made of basalt, and its depth is due to a general subsidence of the entire region and not because of erosion.
Enewetak has a mean elevation above sea level of 10 feet (3.0 m).
Read more about this topic: Enewetak Atoll
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“Where the heart is, there the muses, there the gods sojourn, and not in any geography of fame. Massachusetts, Connecticut River, and Boston Bay, you think paltry places, and the ear loves names of foreign and classic topography. But here we are; and, if we tarry a little, we may come to learn that here is best. See to it, only, that thyself is here;—and art and nature, hope and fate, friends, angels, and the Supreme Being, shall not absent from the chamber where thou sittest.”
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