Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Pages: 45. Chapters: Canadian Shield, Messinian salinity crisis, Great Lakes tectonic zone, Yellowstone hotspot, Geology of the Himalaya, Geology of Great Britain, Anahim hotspot, Galapagos hotspot, Kaolin Deposits of Charentes Basin, France, Petroleum exploration in the Arctic, Multilayered Mapping of the Cap-Vert, Iceland hotspot, Bermuda hotspot, Messinian erosional crisis, Betic corridor, New England hotspot, Louisville hotspot, Richat Structure, Cratonic sequence, Periadriatic Seam, Neocomian, Bowie hotspot, Raton hotspot, Reunion hotspot, Geology of the English counties, Cobb hotspot, Baissa, Mediterranean Ridge, Great Meteor hotspot track, Easter hotspot, Thrace Basin, Mackenzie hotspot, Tristan hotspot, Geology of the Faroe Islands, Kazan Region, Kerguelen hotspot, Canary hotspot, Macdonald hotspot, Balleny hotspot, Juan Fernandez hotspot, Azores hotspot, Eifel hotspot, Marquesas hotspot, Jan Mayen hotspot, Messinian evaporite. Excerpt: The Messinian Salinity Crisis, also referred to as the Messinian Event, and in its latest stage as the Lago Mare event, was a geological event during which the Mediterranean Sea went into a cycle of partly or nearly complete desiccation throughout the latter part of the Messinian age of the Miocene epoch, from 5.96 to 5.33 Ma (million years ago). It ended with the so-called "Zanclean flood," when the Atlantic reclaimed the basin. Sediment samples from below the deep seafloor of the Mediterranean Sea, which include evaporite minerals, soils, and fossil plants, show that about 5.96 million years ago in the late Miocene period the precursor of the Strait of Gibraltar closed tight, and the Mediterranean Sea, for the first time and then repeatedly, partially desiccated. 5.6 Ma ago the strait closed one last, final time, and because of the generally dry climate conditions, within a millennium the Medit...