How Lhotse is formed?

Lhotse, the fourth highest mountain in the world, was formed through the tectonic processes of the Himalayan orogeny, which began around 50 million years ago when the Indian and Eurasian tectonic plates collided. This collision caused intense folding and uplift of the Earth's crust, resulting in the dramatic peaks of the Himalayas, including Lhotse. The mountain features a combination of granite and schist rock formations shaped by glacial erosion, which carved its steep faces and sharp ridges. Lhotse's distinctive features, including its massive south face, were further sculpted by climatic factors and glacial activity over millennia.