Abstract

Deep tunnels in mountainous terrains usually drain large amounts of warm waters. These waters are of interest for numerous reasons: they provide information about subsurface flow conditions, can be decisive or even catastrophic in underground construction, and represent a most interesting geothermal potential for direct heat applications such as space heating. Examples are given from the Swiss Alps.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call