Difference between revisions of "Pine Island Glacier"

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==Subglacial volcano==
==Subglacial volcano==
[[File:Pine Island Map.png|350px|thumb|Detailed map showing the features surrounding the Pine Island Glacier.]]
In January 2008 the British Antarctic Survey (BAS) scientists, Hugh Corr and David Vaughan, reported that 2,200 years ago a volcano erupted under the Antarctic ice sheet. This was the biggest Antarctic eruption in the last 10,000 years. The volcano is situated in the [[Hudson Mountains]], close to Pine Island Glacier. The eruption spread a layer of volcanic ash (or tephra) over the surface of the [[ice sheet]]. This ash was then buried under the snow and ice. Corr and Vaughan were able to map this ash layer using an airborne radar system and calculate the date of the eruption from the depth of burial of the ash. This method uses dates calculated from nearby ice cores. The presence of the volcano raises the possibility that volcanic activity could have contributed, or may contribute in the future, to increases in the flow of the [[glacier]].
In January 2008 the British Antarctic Survey (BAS) scientists, Hugh Corr and David Vaughan, reported that 2,200 years ago a volcano erupted under the Antarctic ice sheet. This was the biggest Antarctic eruption in the last 10,000 years. The volcano is situated in the [[Hudson Mountains]], close to Pine Island Glacier. The eruption spread a layer of volcanic ash (or tephra) over the surface of the [[ice sheet]]. This ash was then buried under the snow and ice. Corr and Vaughan were able to map this ash layer using an airborne radar system and calculate the date of the eruption from the depth of burial of the ash. This method uses dates calculated from nearby ice cores. The presence of the volcano raises the possibility that volcanic activity could have contributed, or may contribute in the future, to increases in the flow of the [[glacier]].