In June 2005, scientists used fluorescent dye to track groundwater movement in Yellowstone National Park. They discovered a rapid connection between surface water and Mammoth Crystal Springs. The findings revealed groundwater traveled 1.45 miles with a vertical drop of approximately 500 feet. The research documented how quickly groundwater moved and the effects of weather on spring discharge. This study contributed to understanding groundwater and surface water connections in Yellowstone’s hydrology.
Read more at Times of India
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