Groundwater flow and storage processes in an inactive rock glacier

Groundwater flow through coarse blocky landforms contributes to streamflow in mountain watersheds, yet its role in the alpine hydrologic cycle has received relatively little attention. This study examines the internal structure and hydrogeological characteristics of an inactive rock glacier in the C...

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Veröffentlicht in:	Hydrological processes 2018-09, Vol.32 (20), p.3070-3088
Hauptverfasser:	Harrington, Jordan S., Mozil, Alexandra, Hayashi, Masaki, Bentley, Laurence R.
Format:	Artikel
Sprache:	eng
Schlagworte:	Alpine environments alpine hydrology Aquifers Bedrock Chemical composition Drainage basins Fish geophysical imaging Geophysics Glaciers Global warming Ground ice Groundwater Groundwater flow Headwaters Hydrogeology Hydrologic cycle Hydrological cycle Hydrology Imaging techniques Infiltration Isotope composition Landforms mountain permafrost Organic chemistry periglacial Rain Rain water Rock glaciers Rocks Sediments Snowmelt Spring Storage Stream discharge Stream flow Unconfined aquifers Water discharge Water flow Watersheds
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