mapping

For decades, researchers have mapped the frozen continent, finding huge depressions and subglacial lakes that have left us in awe. Until now, these formations were studied as isolated pieces of a geological puzzle; However, a new study has turned this view on its head. The demonstration. This study has been published in Nature Geoscience and has just demonstrated that the great basins of East Antarctica are not independent accidents, but form part of a single, gigantic fan-shaped tectonic province. The tectonic fan. The research team, using a combination of subglacial topography, gravity and magnetism data, proposes that this entire vast region is the result of a distributed rotational extension process. To understand it, we can imagine the Earth’s crust in this area opening and stretching asymmetrically, unfolding as if it were a fan. This colossal tectonic movement makes East Antarctica one of the largest known examples of rotational extension in continental crust on the entire planet. The beginning. The origin of this continental scar is closely linked to the history of our planet, specifically to the tectonic phases linked to the fragmentation of the supercontinent Gondwana and the dramatic separation between Antarctica and Australia. As the land masses separated, the crust stretched and fractured, leaving this “bounced topography” that today lies hidden under miles of ice. Its importance. Beyond the undoubted geological and historical value, understanding this structure has a practical and urgent application, since Antarctica is the great thermostat of the Earth and its stability is key in the face of climate change. The topography beneath the Antarctic ice sheet acts as a mold that conditions absolutely everything that happens on the surface. This is seen, for example, in how the shape of bedrock controls the flow of today’s glaciers and determines how subglacial lake and basin systems are distributed. That is why, if we want to predict with mathematical precision how the Antarctic ice will respond to global warming and how it will flow towards the ocean, we need to know the tectonic “pipe” on which it rests to the millimeter. Its mystery. Although the article Nature Geoscience manages to unify structures as massive as the Wilkes and Aurora basins under the same theoretical framework, the authors maintain scientific caution. The exact age at which this fan province formed and the fine geodynamic mechanism that triggered it remain, to a large extent, open questions, and this means that work still needs to be done to find out exactly when the movements of the Antarctic crust will occur. Images | Tam Minton Nature In Xataka | Antarctica was practically the last corner of the Earth immune to touristification. That’s ending