A series of unusual earthquakes near the border of Germany and the Czech Republic has raised the possibility of magma movement deep beneath the surface. These earthquakes, which occurred in the Vogtland region, are typically mild and last for several weeks. However, a recent swarm exhibited unique characteristics, including a northward shift in its center and an occurrence on a near-horizontal underground structure. While the exact cause of the earthquakes is still unknown, scientists believe it may be related to carbon dioxide bubbling up from magmatic fluids deep underground. The findings suggest that the region may have the potential for future volcanic activity, although this is not imminent.