首页> 外文会议>Keck Research Symposium in Geology >GEOCHEMICAL EVIDENCE OF ANTHROPOGENIC IMPACTS ON SWIFTCURRENT LAKE, GLACIER NATIONAL PARK, MT
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GEOCHEMICAL EVIDENCE OF ANTHROPOGENIC IMPACTS ON SWIFTCURRENT LAKE, GLACIER NATIONAL PARK, MT

机译:对Swiftcurrent Lake,冰川国家公园,MT的人为影响的地球化学证据

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摘要

2010 marked the centennial anniversary of the commemoration of Glacier National Park, and since its dedication, the region has experienced increasingly severe effects of anthropogenic disturbance. As atmospheric CO_2 concentrations continue to rise, most-if not all-of the Park's remaining glaciers are projected to disappear by 2030 (Hall and Fagre, 2003), so it has become more important than ever to understand how humans impact this environment. The sediments preserved in the Park's glacially-fed alpine lakes reflect important climatic and geochemical changes in response to anthropogenic influence (MacGregor et al., 2011).
机译:2010年,纪念冰川国家公园的百年周年纪念日,而自奉献以来,该地区越来越严重对人为干扰的影响。随着大气的CO_2浓度继续上升,大多数 - 如果不是全能的公园的剩余冰川被预测到2030(大厅和Fagre,2003),所以它比以往任何时候都变得更加重要,以了解人类如何影响这种环境。在公园的冰川喂养的高山湖中保存的沉积物反映了对人为影响的重要气候和地球化学变化(MacGregor等,2011)。

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