Geothermal heat flow (GHF) is an elusive physical property, yet it can reveal past and
present plate tectonic processes. In Antarctica, GHF has further consequences in predicting …

Over the past decades, significant efforts have been made to understand the nature,
dynamics and evolution of volcanic systems. In parallel, the continuous demographic …

The geology beneath Thwaites Glacier, the Antarctic glacial catchment most vulnerable to
climate change, is unknown. Thwaites Glacier lies within the West Antarctic Rift System, but …

The dynamics of the ice sheets on glacial timescales are highly controlled by interactions
with the solid Earth, ie, the glacial isostatic adjustment (GIA). Particularly at marine ice …

Tanzania is one of the several countries intersected by the East African Rift System (EARS)
endowed by a geothermal potential that has been explored only to a limited extent. Here we …

Subglacial meltwater drainage can enhance localized melting along grounding zones and
beneath the ice shelves of marine-terminating glaciers. Efforts to constrain the evolution of …

Geothermal heat flow beneath the Greenland and Antarctic ice sheets is an important
boundary condition for ice sheet dynamics, but is rarely measured directly and therefore is …

Geothermal features in Antarctica provide favorable conditions for diverse microorganisms,
yet their genomic diversity remains poorly understood. Here, we present an integrated …

The active rift zones in Iceland provide unique insight into the geodynamic processes of
divergent plate boundaries. The geodynamics of Iceland are studied intensively, particularly …

Basal thermal conditions play an important role in ice sheet dynamics, and they are sensitive
to geothermal heat flux (GHF). Here we estimate the basal thermal conditions, including …