What formed Mount Vinson Massif?

Mount Vinson Massif, the highest peak in Antarctica, was formed primarily through geological processes such as tectonic activity and glaciation. Its formation is linked to the movement of the Antarctic tectonic plate, which has influenced the uplift of the mountain range. Additionally, glacial erosion has sculpted its dramatic peaks and valleys, exposing the rugged terrain we see today. The combination of these processes has resulted in the massif's impressive elevation and unique geological features.