Greg Carling, Brigham Young University
Physical Sciences
Wyoming the second most glaciated state in the lower 48 United States has seen drastic changes in the size of its glaciers. Glaciers in high elevation ecosystems of Grand Teton National Park are not anywhere near to the size that they were 100 years ago. The glaciers continue to decrease in size every day. As the environment changes the glaciers change in size and can be affected by many factors in the environment. Deposition of particulate matter from the atmosphere into the glaciers occurs as pollution is becoming worse and more common. Studies done throughout the world have shown that glaciers can act as a source for mercury and other trace metal elements in high elevation ecosystems. Through the assistance of the UW-NPS Research Station Dr. Greg Carling of BYU and his team of graduate and undergraduate assistants retrieved 100 glacial melt water samples from the Middle Teton, and Teepee Glaciers and stream sites in Garnet Canyon, and from the Teton Glacier in the Glacier Gulch area. In the data analysis completed up until this point, concentrations of various trace elements have found in sample sites in close proximity to the Middle and Teton glaciers on the glacial moraine. We hypothesize that these glaciers act as a source for mercury and trace elements that can then be transported to lower elevation ecosystems within the Greater Yellowstone Ecosystem.