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In the language of geology, a tuff cone is a wide, low-rimmed accumulation of debris around a volcanic vent. The debris, or tuff (from tofus, a Latin word meaning soft, light, porous rock), is igneous rock that forms wherever airborne volcanic pumice falls back to earth, piling up like a sooty snowdrift. The cliffs around Portlock, a residential community on the slope of Koko Head, the lodestone of O‘ahu’s craggy southeastern coast, are made of tuff from the same eruption that formed the crater now known as Hanauma Bay. In the pellucid waters of the bay, a protected marine life conservation area, moray eels slink around Pocillopora coral formations.
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