During the initial collision of the Asia and Indian plates, a granitic batholith was buried to depths of about 20 kilometres (12 mi) or more, highly metamorphosed, highly deformed, and partially remelted during the Eocene Period to form gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes and finally exhumed and uplifted along major breakback thrust faults during post-Miocene time. The K2 Gneiss was exposed as the entire K2-Broad Peak-Gasherbrum range experienced rapid uplift with which erosion rates have been unable to keep pace.
when two cars collided
when 2 plates collided
K2 and the Himalayas were formed when the Indian plate onverged with the Eurasian plate. the Indian plate is still moving northward, subducting the Eurasian plate and the mountain range continues to rise a few millimeters each year.
like any mountain when TWO earth plates move together
Mount K2, also known as the Savage Mountain, was formed during the uplift of the Karakoram Range in the geologically recent past, likely within the last few million years. However, the specific time of its formation cannot be determined with precision.
K2 is in Pakistan.
K2 is located on the Asian continent.
K2 Is Located In Pakistan..
K2 has 1 peak
K2 is humid hope that helped
k2 by far
On K2 mountain, temperatures can drop as low as -60°C (-76°F) during the winter months. The average temperature on the summit ranges between -36°C (-32°F) and -27°C (-17°F) throughout the year.