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Bear in mind that Nostradamus essentially says in his Epistle to Henry II, as well as several key quatrains, that we will not reach that point until AD 2242-43 (thus, either AD 2236-2243 or else AD 2243-2250).
He also raises an additional optimistic scenario that, if the end is not achieved around the time of this AD 2242-43 window of opportunity, a period of grace for humanity will extend all the way until AD 2827-28.
November 2017, Luzern (CH), Luzerner Mobilitätsgespräche 2017, 5.
Significant Discoveries, 2004, (From AAPG Explorer, January 2005), #10078 (2005). Meandering Fluvial Facies Architecture Using Ground Penetrating Radar, Ferron Sandstone (Upper Cretaceous) Emery County, Utah, Oluwasegun Abatan, Dennis Kerr, and Kumar Ramachandran, #41134 (2013). Are Scientific Honesty and "Best Practices" in Conflict? Characterization of Thinly Bedded Units and 3D Static Model Open Reserves in Sabiriyah Field Middle Burgan Reservoir, North Kuwait, Sabry Abd El-Aziz, Mariam Taqi, Saleh Al-Rashdan, and Saleh Al-Rasheedi, #20289 (2015). Abdul Baqi, #110010 (2004) (3 of 6 presentations at DEG/SEPM/EMD Forum: The Future of Global Energy: Technical, Environmental, Economics, and Policy Issues AAPG Annual Convention, Dallas, Texas, April, 2004) Mineralogical Content of Productive Series Shales of Western Portion of South Caspian (Example, Bulla-Daniz Area), Elshan Abdullayev and Yagut Muslimova, #30149 (2011). The Antarctic Peninsula Ice Sheet (sometimes written as APIS) is widely regarded as sensitive to climate change due to its small size and northerly location, and because this region is one of the most rapidly warming places in the world[2-5].This sensitivity has been manifest through the collapse of numerous ice shelves, increased ice velocities, and the retreat and thinning of glaciers and ice caps[6-10].Secondary Flow in Meandering Channels on Submarine Fans: Implications for Channel Morphodynamics and Architecture, Jorge D. Source Rocks at Svalbard: An Overview of Jurassic and Triassic Formations and Comparison with Offshore Barents Sea Time Equivalent Source Rock Formations, Tesfamariam B. Systematic Workflow for Characterizing Frac Sand: An Integrated Approach, Waseem Abdulrazzaq, Bilal Zoghbi, Walter Suzart, and Muhammad Salem, #80551 (2016). Abad, Octavio Sequeiros, Benoit Spinewine, Carlos Pirmez, Marcelo Garcia, and Gary Parker, #40480 (2010). A Tectono-Stratigraphic Development of the Albertine Graben of Uganda, Western Arm of East African Rift System Based on Sedimentary Exposures, Seismic and Well Data, Dozith Abeinomugisha and Nurudin Njabire, #30427 (2015). Organic Matter Variations Within the Bakken Shales of Saskatchewan: With Implications Upon Origin and Timing of Hydrocarbon Generation, Titi Aderoju and Stephen L. Investigating the Effect of Organic Sulphur Compounds on Oil Generation in Bakken Formation in Saskatchewan, Titi Aderoju and Stephen L. Foundation Settlement Determination: A Simplified Approach, O.