The geology of Yosemite National Park is a complex and diverse system that reflects the region's unique tectonic history. The park's landscape is shaped by millions of years of weathering, erosion, and volcanic activity.
The park's landscape is characterized by a diverse range of features, including granite peaks, waterfalls, and meadows. The Sierra Nevada mountain range dominates the park, with its highest peak being Mount Whitney at 14,505 feet.
The geology of Yosemite National Park is underpinned by a complex system of formations, including granite domes, gorges, and canyons. The park's unique geology is also influenced by the movement of tectonic plates.
The geology of Yosemite National Park provides a rich source of natural resources, including timber, minerals, and water. The park is home to many endangered species, such as the marbled murrelet and the western spotted owl.
Learn more about the geology of Yosemite National Park at https://vocal.media/earth/the-geology-of-yosemite-national-park-mount-sopris