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Sea and Land: An Illustrated History of the Wonderful and Curious Things of Nature Existing Before and Since the Deluge (Classic Reprint)

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Helgason, Guðmundur. "Finale". Uboat.net. Archived from the original on 6 February 2010 . Retrieved 13 September 2013.

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Logico, Mark G. (8 April 2006). "Navy Chief Submerges 2,000 Feet, Sets Record". America's Navy. United States Navy. Archived from the original on 13 May 2020 . Retrieved 12 September 2013. Murakami, M. (2002). "Water in Earth's Lower Mantle". Science. 295 (5561): 1885–1887. Bibcode: 2002Sci...295.1885M. doi: 10.1126/science.1065998. PMID 11884752. S2CID 21421320. a b "Ocean Acidification". National Geographic. 27 April 2017. Archived from the original on 9 October 2018 . Retrieved 9 October 2018. With regards to maps that are vital for navigation, in the second century, Ptolemy mapped the whole known world from the "Fortunatae Insulae", Cape Verde or Canary Islands, eastward to the Gulf of Thailand. This map was used in 1492 when Christopher Columbus set out on his voyages of discovery. [114] Subsequently, Gerardus Mercator made a practical map of the world in 1538, his map projection conveniently making rhumb lines straight. [3] :12–13 By the eighteenth century better maps had been made and part of the objective of James Cook on his voyages was to further map the ocean. Scientific study has continued with the depth recordings of the Tuscarora, the oceanic research of the Challenger voyages (1872–1876), the work of the Scandinavian seamen Roald Amundsen and Fridtjof Nansen, the Michael Sars expedition in 1910, the German Meteor expedition of 1925, the Antarctic survey work of Discovery II in 1932, and others since. [19] Furthermore, in 1921, the International Hydrographic Organization (IHO) was set up, and it constitutes the world authority on hydrographic surveying and nautical charting. [115] A fourth edition draft was published in 1986 but so far several naming disputes (such as the one over the Sea of Japan) have prevented its ratification.Nishri, A.; Stiller, M; Rimmer, A.; Geifman, Y.; Krom, M. (1999). "Lake Kinneret (The Sea of Galilee): the effects of diversion of external salinity sources and the probable chemical composition of the internal salinity sources". Chemical Geology. 158 (1–2): 37–52. Bibcode: 1999ChGeo.158...37N. doi: 10.1016/S0009-2541(99)00007-8. For those of us confined to living on the surface, the fact that our world is mostly covered in water is a well known fact. But how much of our planet is made up of water, exactly? Like most facts pertaining to our world, the answer is a little more complicated than you might think, and takes into account a number of different qualifications. Several nomadic indigenous groups in Maritime Southeast Asia live in boats and derive nearly all they need from the sea. The Moken people live on the coasts of Thailand and Burma and islands in the Andaman Sea. [196] Some Sea Gypsies are accomplished free-divers, able to descend to depths of 30 metres (98ft), though many are adopting a more settled, land-based way of life. [197] [198] When the valley floor warms during the day, warm air rises up the slopes of surrounding mountains and hills to create a valley breeze. At night, denser cool air slides down the slopes to settle in the valley, producing a mountain breeze. Music too has been inspired by the ocean, sometimes by composers who lived or worked near the shore and saw its many different aspects. Sea shanties, songs that were chanted by mariners to help them perform arduous tasks, have been woven into compositions and impressions in music have been created of calm waters, crashing waves and storms at sea. [208] :4–8 The Oceanids (The Naiads of the Sea), a painting by Gustave Doré ( c. 1860)

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a b "Tides and Water Levels". NOAA Oceans and Coasts. NOAA Ocean Service Education. Archived from the original on 1 November 2014 . Retrieved 20 April 2013. Norris, Gregory J. (1981). "Evolution of cruising". Cruise Travel (December): 28. [ permanent dead link]D'Amato, Raphaelo; Salimbeti, Andrea (2011). Bronze Age Greek Warrior 1600–1100 BC. Oxford: Osprey Publishing Company. p.24. ISBN 978-1-84908-195-5. Archived from the original on 30 July 2022 . Retrieved 21 November 2020. The sea holds large quantities of valuable dissolved minerals. [193] The most important, Salt for table and industrial use has been harvested by solar evaporation from shallow ponds since prehistoric times. Bromine, accumulated after being leached from the land, is economically recovered from the Dead Sea, where it occurs at 55,000 parts per million (ppm). [194] Fresh water production [ edit ]

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Muller, R. D.; Sdrolias, M.; Gaina, C.; Steinberger, B.; Heine, C. (2008). "Long-Term Sea-Level Fluctuations Driven by Ocean Basin Dynamics". Science. 319 (5868): 1357–1362. Bibcode: 2008Sci...319.1357M. doi: 10.1126/science.1151540. PMID 18323446. S2CID 23334128. a b Millero, F. J.; Feistel, R.; Wright, D. G.; McDougall, T. J. (2008). "The composition of Standard Seawater and the definition of the Reference-Composition Salinity Scale". Deep-Sea Research Part I: Oceanographic Research Papers. 55 (1): 50–72. Bibcode: 2008DSRI...55...50M. doi: 10.1016/j.dsr.2007.10.001. Committee on Biological Diversity in Marine Systems, National Research Council (1995). "Waiting for a whale: human hunting and deep-sea biodiversity". Understanding Marine Biodiversity. National Academies Press. ISBN 978-0-309-17641-5. Archived from the original on 30 July 2022 . Retrieved 21 November 2020.

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Further information: List of seas Oceans and marginal seas as defined by the International Maritime Organization Pidwirny, Michael (28 March 2013). "Plate tectonics". The Encyclopedia of Earth. Archived from the original on 21 October 2014 . Retrieved 20 September 2013.

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