A team of researchers used airborne radar to map out an unexplored region in the deep interior of East Antarctica in search of old ice that could record clues from Earth's ancient climate. Although they haven’t found a suitable ice sample yet, their survey revealed new insights about the geologic processes happening under the Antarctic ice sheet and how ice is moving around beneath it.

Farmers handle a wide range of responsibilities to keep operations running — and a routine but often overlooked duty is safely disposing of dead livestock. Left unattended, carcasses can spread disease and jeopardize entire herds or flocks.

Remarkable changes are taking place in Greenland these years, according to new research. The vast ice masses are warming and melting at an accelerating rate. At the same time, movements in the bedrock caused by the last ice age are reshaping the island. As a result, Greenland is increasingly subjected to twisting, pressure, and tension.

Traditional geotechnical investigations provide data only at discrete borehole locations, leaving vast areas uncharacterized. This spatial gap often leads to unforeseen ground conditions during construction, causing costly delays, design modifications, and occasionally catastrophic failures. Now, a novel integrated geophysical-machine learning approach, using k-means clustering technique, by a team of researchers from Shibaura Institute of Technology provides continuous subsurface characterization, enabling evidence-based decision-making throughout project lifecycles.

Leading maritime engineering specialists, marine ecologists, and biodiversity experts, gathered in Barcelona between 7 and 9 October to officially kick start the project’s vision on climate-resilient coastal landscapes. Hosted by the Maritime Engineering Laboratory from the Polytechnic University of Catalonia, the meeting focused on setting the strategic direction of the project, aligning the scientific, technical and communication objectives and establishing synergies between project partners across Europe and beyond. 

Research led by a University of Utah geoscientist shows O₂ in sulfate deposits, coupled with geochemical clues, could help identify microbial activity in Earth’s rock record and even in Martian sediments.