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 the Cretaceous. Radiometric dating has yielded ages of about 118-120 million years ago. At least during the Paleocene, Ita Mai Tai emerged above sea level. From the Aptian to the Miocene, carbonates were deposited on the seamount and reached an eventual thickness of about . Additionally, the seamount has subsided by about , albeit with time periods where this subsidence was interrupted by the growth of coral reefs. Most of the subsidence occurred during the Oligocene when sedimentation rates were depressed, but the carbonate platform drowned no later than the Eocene, with oolithes forming underwater. During three different episodes in