
Geophysical measurements with a magnetometer being towed with RV Polarstern's board helicopter.
Unlike East Antarctica, West Antarctica is a geologically young region. In addition, it doesn't consist of a large contiguous land mass, where the Earth's crust is up to 40 kilometres thick, but instead is made up of several small and for the most part relatively thin crustal blocks that are separated from each other by a so-called trench system or rift system. In many of the trenches in this system, the Earth's crust is only 17 to 25 kilometres thick, and as a result a large portion of the ground lies one to two kilometres below sea level. On the other hand, the existence of the trenches has long led researchers to assume that comparatively large amounts of heat from Earth's interior rose to the surface in this region. With their new map of this geothermal heat flow in the hinterland of the West Antarctic Amundsen Sea, experts from the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI) and the British Antarctic Survey (BAS) have now provided confirmation.













Comment: For more fascinating insight into our world back then and the cataclysmic shifts it endured, check out Pierre Lescaudron's book: Cometary Encounters: Flash-Frozen Mammoths, Mars-Earth Discharge, Comet Venus and the 3,600-Year Cometary Cycle
The followng articles will provide a taste of what's in the book:
- Volcanoes, Earthquakes And The 3,600 Year Comet Cycle
- Did Earth 'Steal' Martian Water?
- The Seven Destructive Earth Passes of Comet Venus
Also check out SOTT radio's: