What makes Diamond Head worth the trip?
Diamond Head is the defining silhouette of Honolulu, a 760-foot volcanic tuff cone that rises from the southeastern edge of Waikiki Beach and has served as a navigational landmark for Polynesian voyagers, a coastal fortress for the U.S. Army, and the backdrop of virtually every photograph ever taken of Honolulu's coastline. Hawaiians called it Le'ahi — most often read as "brow of the tuna," because the ridgeline resembled the dorsal fin of an ahi tuna when viewed from the sea. British sailors in the 19th century renamed it Diamond Head after mistaking calcite crystals glinting in the tuff for diamonds, a story preserved on the interpretive signage at the official Diamond Head State Monument. Today the crater is one of the most recognisable natural landmarks in the United States and the single most-hiked summit in Hawaii.
The crater formed roughly 300,000 years ago during a single explosive eruption that lasted only a few days, and it has been extinct ever since, its interior now a dry, scrubby basin crisscrossed by the trail that leads to one of the most photographed viewpoints in the Pacific. The hike follows a 1.6-mile round-trip route originally constructed by the U.S. Army in 1908 as part of Oahu's coastal defence system. Hikers pass through a tunnel bored into the crater wall and climb a 99-step staircase inside a former military observation post before emerging onto the summit platform. From the top the view sweeps from the high-rises of downtown Honolulu — where the royal Iolani Palace stands — across the towers of Waikiki and the turquoise arc of Hanauma Bay to the open Pacific and, on clear days, the outline of Molokai across the channel.