
Still plenty of work for scientists to do to gain a better understanding of our rotating Earth’s electromagnetic processes.
Scientists assumed Earth’s mantle, the layer stretching from the crust to a depth of 255 miles, was magnetically dead. New research suggests they were mistaken, reports Phys.org.
Most scientists thought Earth’s magnetism was powered by materials in the crust and core, but according to a new study published this week in the journal Nature, hematite, a common iron oxide, retains its magnetic qualities at high temperatures.
“This new knowledge about the Earth’s mantle and the strongly magnetic region in the western Pacific could throw new light on any observations of the Earth’s magnetic field,” Ilya Kupenko, mineral physicist and researcher from the University of Munster in Germany, said in a news release.






From the team at CFACT ~
The Roman Empire rose and prospered during a time of beneficial global warming. The New Scientist article asserts that the empire played a role in bringing about subsequent cooling temperatures that ultimately contributed to the empire’s downfall. According to the article, soot from Roman fires blocked sunlight and cooled Europe. Deforestation as the empire expanded also cooled temperatures, according to…





