Daiquiri possible that William A. Chanler, a US congressman who purchased the Santiago iron mines in 1902, introduced the daiquiri to clubs in New York in that year. Originally the drink was served in a tall glass packed with cracked ice. A teaspoon of sugar was poured over the ice and the juice of one or two limes was squeezed over the sugar. Two or three ounces of white rum completed the mixture. The glass was then frosted by stirring with a long-handled spoon. Later the daiquiri evolved to be mixed in a shaker with the same ingredients but with shaved
Ita Mai Tai gravelstone and coquina. In drill cores of the summit region the limestone reaches a thickness of and the mud of ; the mud formed in lagoonal settings. Terrigenous rocks have also been encountered within the limestones. Guyots such as Ita Mai Tai often accumulate ferromanganese crusts. These are generated by the oxidative precipitation of manganese salts which also include iron and absorb trace elements such as cobalt, copper, molybdenum, nickel, platin, rare earth elements and zinc from the water through as-yet unknown processes. In the case of Ita Mai Tai these crusts have been found all over the seamount and