Investigating groundwater flow paths within proglacial moraine using multiple geophysical methods

• Published in: Journal of hydrology (Amsterdam) 2011-03, Vol.399 (1), p.57-69
• Main Authors: McClymont, Alastair F., Roy, James W., Hayashi, Masaki, Bentley, Laurence R., Maurer, Hansruedi, Langston, Greg
• Format: Article
• Language: English
• Subjects: Alpine hydrology; Bedrock; Channels; Earth sciences; Earth, ocean, space; Exact sciences and technology; Flow paths; Freshwater; Geophysical methods; Geophysics; Groundwater; Hydrology. Hydrogeology; Moraine; Mountains; Seismic phenomena; Springs; Watersheds
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2010.12.036

► Groundwater stored in alpine watersheds helps sustain mountain rivers. ► Multiple geophysical methods used to characterize groundwater flow paths in vicinity of groundwater spring. ► Bedrock topography channels deep groundwater. ► Shallow flow paths controlled by shallow bedrock and/or ice. ► Most groundwater resides within ca. 5-m-thick layer at moraine/bedrock interface. Groundwater that is stored and slowly released from alpine watersheds plays an important role in sustaining mountain rivers. Yet, little is known about how groundwater flows within typical alpine geological deposits like glacial moraine, talus, and bedrock. Within the Lake O’Hara alpine watershed of the Canadian Rockies, seasonal snowmelt and rain infiltrates into a large complex of glacial moraine and talus deposits before discharging from a series of springs within a relatively confined area of a terminal moraine deposit. In order to understand the shallow subsurface processes that govern how groundwater is routed through this area, we have undertaken a geophysical study on glacial moraine and bedrock over and around the springs. From interpretations of several seismic refraction, ground-penetrating radar (GPR), and electrical resistivity tomography (ERT) profiles, we delineate the topography of bedrock beneath moraine. Although the bedrock is generally flat under central parts of the terminal moraine, we suggest that an exposed slope of bedrock on its eastern side and a ridge of shallow bedrock imaged by ERT data underneath its western margin serves to channel deep groundwater toward the largest spring. Low-electrical-resistivity anomalies identified on ERT images within shallow parts of the moraine indicate the presence of groundwater flowing over shallow bedrock and/or ice. From coincident seismic refraction, GPR and ERT profiles, we interpret an ca. 5-m-thick deep layer of saturated moraine and fractured bedrock. Despite their relatively small storage volumes, we suggest that groundwater flowing through bedrock cracks may provide an important contribution to stream runoff during low-flow periods. The distinct deep and shallow groundwater flow paths that we interpret from geophysical data reconcile with interpretations from previous analyses of hydrograph and water chemistry data from this same area.