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Alaea salt, alternatively referred to as Hawaiian red salt, is an unrefined sea salt that has been mixed with an iron oxide rich volcanic clay called ʻalaea, which gives the seasoning its characteristic brick red color.
Beeke, Joel, and Randall Pederson, Meet the Puritans: With a Guide to Modern Reprints, (Reformation Heritage Books, 2006) ISBN 978-1-60178-000-3; Cross, Claire, The Puritan Earl, The Life of Henry Hastings, Third Earl of Huntingdon, 1536-1595, New York: St. Martin's Press, 1966.
The umbrella term Pacific Islands has taken on several meanings. [1] Sometimes it is used to refer only to the islands defined as lying within Oceania. [2] [3] [4] At other times, it is used to refer to the islands of the Pacific Ocean that were previously colonized by the British, French, Spaniards, Portuguese, Dutch, or Japanese, or by the United States.
Name Elevation Location Last eruption meters feet Coordinates; Bowie Seamount-24-79: 18,000 BC Adams Seamount-59-194: 50 BCE Axial Seamount-1410: 4626: 1998
Likelep may be part of a seamount trail [58] and is part of the Ujlān volcanic complex. [59] A sediment cap and volcanic structures are found on its top, with a volcanic cone protruding through the sediment. Slumps occur on its flanks and a seamount farther north is connected to Likelep. [57] Lalibjet [6] A sea god [8
A list of active and extinct submarine volcanoes and seamounts located under the world's oceans. There are estimated to be 40,000 to 55,000 seamounts in the global oceans. [ 1 ] Almost all are not well-mapped and many may not have been identified at all.
Today the term South Seas, or South Sea, most commonly refers to the portion of the Pacific Ocean south of the equator. [1] [2] [3] The term South Sea may also be used synonymously for Oceania, or even more narrowly for Polynesia or the Polynesian Triangle, an area bounded by the Hawaiian Islands, New Zealand and Easter Island.
The Tasmantid hotspot is a volcanic hotspot located in the South Pacific Ocean.The northward movement of the Indo-Australian Plate over the last 60 million years coupled with volcanism of the Tasmantid hotspot has resulted in a north–south line of submarine volcanoes called the Tasmantid Seamount Chain. [3]