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Paul's first letter to the Corinthians contains both emphatic warnings and strong statements of assurance, and the relationship between them has often puzzled interpreters. At times, it sounds as if Paul is warning the Corinthians lest they forfeit their eschatological salvation; at others, it sounds like he is assuring them that they will not. Attempts to harmonise the two stances have often ended up nullifying the warnings, or the assurances, or both. In this fresh analysis of all the relevant texts, Andrew J. Wilson demonstrates that Paul's warnings and assurances stand in tension with each other, and suggests that this tension is both coherent, and, in actual fact, deliberate on Paul's part. Discussions of perseverance and apostasy in Paul, grace and works, and the relationship between divine and human agency, will all now need to reckon with this important contribution.
This updated edition will help IT managers and assets protection professionals to assure the protection and availability of vital digital information and related information systems assets. It contains major updates and three new chapters. The book uniquely bridges the gap between information security, information systems security and information warfare. It re-examines why organizations need to take information assurance seriously.
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Perennially-frozen Angiussaq Lake, Greenland was examined in 1957 to determine the strength of its midsummer ice cover and the causes of its perennially-frozen conditions. The lake, largest within a 100-mi radius of Thule Air Base, is formed by ice-cap damming of a valley 200 m deep, and has an elevation of 590 m. Water temperatures ranged from 0.1 to 0.7 C and showed that summertime mixing is sufficient to maintain nearly isothermal conditions. Fish, phytoplankton, AND CHIRONOMID LIFE WERE FOUND IN THE LAKE WATER. At the end of the 1957 summer, more than 90% of the lake surface was covered by ice averaging 1.5 m in thickness. Variations in melting rate have caused a gently rolling surface that might be smoothed by flooding or scraping. In-place cantilever beam tests showed that the upper half meter of ice had almost no strength but that the lower portion maintained sufficient strength to support heavy loads throughout the summer. A tongue of glacier ice floating in the lake has a thickness of about 100 m and a length of about 3 km. Five smaller ice islands have thicknesses of more than 5 m and are believed to form where snow accumulation exceeds ablation. (Author).