Geology professor Lonnie Thompson, left, and research associate Mary Davis take an early look at a segment of the Kilimanjaro ice core. Researcher Mary Davis examines a thick dust layer inside the ice core, signifying a major drought event that struck the region in the past. The outer margin of the Furtwangler ice field on Kilimanjaro ice sheet show that a massive retreat, or melting, has occurred in recent years.
Members of the Ohio State expedition can barely be seen at the base of the ice wall that makes up the outer margin of Kilimanjaro's dwindling Northern ice field. One of the last remnants of Kilimanjaro's Eastern ice field is a six-meter spire that was much larger when seen on earlier expeditions. It should vanish in a few years due to global warming. The lower portion of the outer margin of Kilimanjaro's northern ice field shows clearly the stratigraphic record of ancient climate trapped in the ice.
Three views of a remnant 12 meter high spire that is all that's left of one of the smaller ice fields on Africa's highest ice-capped peak, Kilimanjaro. On the right, expedition leader Lonnie Thompson surveys the rapidly vanishing clues to past climate conditions at this tropical locale.

Return to research story
Return to OSU Research News website.