There was recently an unexpected discovery in the overlying ice of southern Alaska’s Bench Glacier. According to an article on October 23, 2010 on ScienceNews.com, deep cracks were found extending from the ground up through the glacier. A team of researchers led by Joel Harper of the University of Montana in Missoula discovered the cracks. The team drilled holes through the Bench Glacier’s 200 meters to observe how water would drain. The goal of the research trip was to use a drill bit made of hot water—jet of snow melted to 160 degrees Celsius. The hole stayed filled with water during the drilling process until according to Harper, “But all of a sudden, boom, it drains right down. It sucked all the water out of our hole.” The team sent down a video camera and saw the huge crevasse they inadvertently struck. The beds of the glacier, as stated before are 200 meters deep, and the team hit this fissure at only 120 meters down, still 80 more meters to go until the bottom of the bed. Because hitting that fissure was such a chance occurrence, the team drilled nearly 30 holes at other spots on the glacier—“the majority of which drained prematurely, suggesting numerous cracks spike up into the ice.” According the article, “Scientists aren’t certain how widespread such cracks are, how long the fissures persist, or how glacier movement might be influenced. The cracks hold a considerable amount of water and could help scientists better predict how and when glaciers move and melt, which in turn could affect how much sea levels rise in the future.” Scientists think the cracks are produced by water pressure below the glacier and stress from the massive weight above, act as a buffer that allows “the glacier to absorb, sponge-style, a sudden inrush of water from melting or rain. This drainage may prevent the sliding and lurching that can happen with the water rushes into the bed of soil and rock under the glacier. But under certain conditions, the cracks might suddenly drain, and that could spill water into the bed and send a glacier sliding.” Scientist worry that the type of drainage cased by these fissures in the glaciers is too unstable because ice melts so easily, which could cause a lot of glacier sliding in the Alaska regions. In our class, we talked about the Missoula Flood and the effects of glacier movement to the earth’s surface and the creation and changing of landforms. The impending effect of the fissures found in the glaciers has not been determined yet because it is such a recent discovery, but scientists like Kholer say, “A little water suddenly has more of an effect than a lot of water slowly. Generally, the more water that goes through a system, the more it can handle pressure and perturbations.” The reports from this initial finding, the team simply believes that more cracks like this exist elsewhere. Though much more work needs to be done Harper’s team just wants the world to be aware of the risk.
http://www.sciencenews.org/view/generic/id/63847/title/Glacier_found_to_be_deeply_cracked