Isle of Rum
The Isle of Rum is fascinating from a geological standpoint for four reasons:
Dr. Mike Cheadle and Dr. Bobbie John from the University of Wyoming accompanied
our MIT/WHOI group into the field, providing expert discussions
on the different aspects of Rum geology. Rum is one of the oldest
volcanoes in the west of Scotland, pre-dating the centers in
Skye and Mull. Ages close to 63 Ma link this closely to the
initation of the Icelandic hotspot, still active today. The
gabbros that form the core of the exposed volcano are divided
into three sections, two layered series in the East and West
and a chaotic central zone, which is inferred to be the feeder
zone where new melt was delivered into the chamber from the
The gabbros are inferred to represent a 1000 km3 magma chamber and are famous for their rhythmic, layered appearance whose origin has been hotly debated by geologists. One viewpoint holds that these represent precipitation of crystals in a liquid magma chamber, with each layer representing the arrival of new batch of melt. Others have argued that the chamber was originally semi-solid and relatively homogeneous, with the banding the result of the late stage injection of a series of gabbroic sills. Click here to read Joint Program student Cara Santelli's series of three haikus composed in honor of Rum's volcanic past.
On the first day, the group hiked to see the chaotic folding and slumping of the central zone, with time to see the famous long olivine crystals of the Harrisites. More Harrisites were viewed by an elite and dedicated minority on the second day in the face of an unrelenting north Atlantic downpour. On the third day, the heavens smiled on the party enough to allow an inspection of the classic eastern layered series on the slopes of Mt. Hallival.
The accompanying slide shows provide a glimpse at the geology and scenery we encountered on the Isle of Rum.
Last updated: August 22, 2007