NuclearWinter
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- Apr 13, 2006
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As geoscientists probe ever more deeply into the "record in the rocks", their findings will oftentimes coincide with many Pole-Shift explanations. For example, a recent study of the conentrations of calcium and sulfate ions in the annual ice layers cored from the Greenland ice sheet provides an extensive record of explosive, high-sulfur producing volcanism that shows a strong correlation with disturbances and eruptive events within the last 50,000 years.
The sulfate-ion value in the GISP2 ice-core record is one of the largest of the 838 volcanic signals in the entire ice-layer sample series. And this signal, representing enormous volcanism somewhere in the Northern Hemisphere, is followed by around 1,000 years of calcium-ion peaks that are a primary indicator of continental dust.
In addition, a volcanic ash layer found in a different (GRIP) ice core from Greenland and believed to have originated from an area of explosive volcanism in southern Iceland, is thought to be created at a time that coincides with one of the previous two Pole-Shifts as well.
The GISP2 ice-core record is intriguing. It provides evidence of a period of significant volcanism that occurred somewhere in the Northern Hemisphere at the same time that a second period of disturbances were underway. The disturbances were so strong that "small channels" were produced through many of the lands.
The sulfate-ion value in the GISP2 ice-core record is one of the largest of the 838 volcanic signals in the entire ice-layer sample series. And this signal, representing enormous volcanism somewhere in the Northern Hemisphere, is followed by around 1,000 years of calcium-ion peaks that are a primary indicator of continental dust.
In addition, a volcanic ash layer found in a different (GRIP) ice core from Greenland and believed to have originated from an area of explosive volcanism in southern Iceland, is thought to be created at a time that coincides with one of the previous two Pole-Shifts as well.
The GISP2 ice-core record is intriguing. It provides evidence of a period of significant volcanism that occurred somewhere in the Northern Hemisphere at the same time that a second period of disturbances were underway. The disturbances were so strong that "small channels" were produced through many of the lands.