Titlebook: Oceanic Hotspots; Intraplate Submarine Roger Hekinian,Jean-Louis Cheminée,Peter Stoffers Book 2004 Springer-Verlag Berlin Heidelberg 2004 I

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O. Thießen,M. Schmidt,R. Botz,M. Schmitt,P. Stoffers

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Introduction, construction of the Earth’s volcanic structures takes place under the sea in oceanic basins and along spreading centers. The divergent plate boundaries (Mid-Ocean Ridges) and back-arcs are relatively straight and structurally continuous features, making them easier to investigate than the more scat

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Seismicity of the Society and Austral Hotspots in the South Pacific: Seismic Detection, Monitoring monitoring of seismic activity on the ocean floor remains one of the few methods of studying submarine volcanic activity. This line of research goes back to more than fifty years ago, when based on a suggestion of (.), (.) obtained a detailed history of the 1952 eruption of the Myojin Volcano, south

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A Global Isostatic Load Model and its Application to Determine the Lithospheric Density Structure o times) modern principles of isostasy. His idea about the “wandering continents” was complemented and strengthened later on by important notions, among which were the rejuvenation of the oceanic lithosphere and its absorption in the inner Earth after subduction that later evolved as the theory of “p

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Origin of the 43 Ma Bend Along the Hawaiian-Emperor Seamount Chain: Problem and Solution,are surface manifestations of deep, fixed sources of mantle plumes (., .), then the along-track volcanic age progression away from Hawaii (e.g., .) must record the direction, absolute velocity, and possible changes of the Pacific Plate motion. This would suggest that the prominent ∼43 Ma Bend along

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