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 southeastern side. The outer slopes of the seamount have a step-like appearance and feature radial grabens formed presumably by subsidence. At their foot, sediments descending from the seamount have formed talus deposits. The seamount has several rift zones crosscut by dykes and sills and features an "L"-shaped ridge to the west with a width of . South of the "L"-shaped ridge lies another seamount which is also considered to be part of Ita Mai Tai; it is uneroded and features parasitic vents. The ridge that connects the two may be the western edge of a collapse caldera. This wide and