Although erosion of valleys by subglacial meltwater was first proposed more than 100years
ago, the processes that produced these valleys under past ice sheets have remained a topic …

The low permeability of clays, shales, and other argillaceous lithologies makes them key
controls of transport and deformation processes in the crust but is known for being …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Brine springs discharging from Devonian carbonates of the Western Canada Sedimentary
Basin have distinct water chemistry from brines in laterally equivalent units deeper in the …

Pleistocene glaciations and their associated dramatic climatic conditions are suspected to
have had a large impact on the groundwater flow system over the entire North American …

While the geomorphic consequences of Pleistocene megafloods have been known for some
time, it has been only in the past 2 decades that hydrogeologists and glaciologists alike …

The hydrogeochemistry of saline-meteoric water interface zones in sedimentary basins is
important in constraining the fluid migration history, chemical evolution of basinal brines …

Underground geological storage of CO2 in deep saline aquifers is considered for reducing
greenhouse gases emissions into the atmosphere. However, some issues were raised with …

Deep meteoric waters comprise a key component of the hydrologic cycle, transferring water,
energy, and life between the Earth's surface and deeper crustal environments, yet little is …

Salinity data from the Atlantic continental shelf off New England indicate that the
freshwater/saltwater interface is far out of equilibrium with modern sea-level conditions …