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 Aptian-Turonian, Santonian-Maastrichtian and Paleocene-Eocene, oolithic limestones were deposited on Ita Mai Tai, presumably by reefs and living organisms in shallow water. Lifeforms that inhabited the seamount included algae, belemnites, bivalves, bryozoans, corals, decapods, echinoderms, foraminifera, gastropods, ostracods, pogonophora, rudists and sea urchins; their fossils have been recovered in the limestone from Ita Mai Tai and the rudists are the most commonly encountered reef builders on this seamount. The oolith-containing limestone was formed by a coral reef. The reef was affected by wave activity and there were lagoonal environments as well. Bioherms developed on the Gelendzhik seamount as well, where