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It consists of sillimanite-K-feldspar grade schist and gneiss intruded by numerous sills and dikes of leucogranite ranging in thickness from 1 cm to 1,500 m (0.4 in to 4,900 ft). Mount Everest consists of sedimentary and metamorphic rocks that have been faulted southward over continental crust composed of Archean granulites of the Indian Plate during the Cenozoic collision of India with Asia. They formed as the results of partial melting of Paleoproterozoic to Ordovician high-grade metasedimentary rocks of the upper Himalayan Sequence about 20 to 24 million years ago in the course of the subduction of the Indian Plate. These metamorphic rocks seem like the result of the metamorphism of Middle to Early Cambrian deep sea flysch composed of interbedded, mudstone, shale, clayey sandstone, calcareous sandstone, graywacke, and sandy limestone. The air pressure at the summit is usually about one-third what it's at sea degree. The station's first information in May 2008 have been air temperature −17 °C (1 °F), relative humidity 41.3 per cent, atmospheric strain 382.1 hPa (38.21 kPa), wind route 262.8°, wind speed 12.8 m/s (28.6 mph, 46.1 km/h), world photo voltaic radiation 711.9 watts/m2, solar UVA radiation 30.Four W/m2

A thick, white-weathering thrombolite bed that is 60 m (200 ft) thick includes the foot of the "Third Step", and base of the summit pyramid of Everest. The base camp for Everest expeditions based out of Nepal is situated by Khumbu Glacier, which is quickly thinning and destabilizing because of climate change, making it unsafe for climbers. The bottom of the North Col Formation is a regional low-angle normal fault called the "Lhotse detachment". A 5-forty cm (2.0-15.7 in) thick fault breccia separates it from the overlying Qomolangma Formation. The Qomolangma Formation is damaged up by several excessive-angle faults that terminate on the low angle normal fault, the Qomolangma Detachment. The decrease 5 metres of the Qomolangma Formation overlying this detachment are very highly deformed. The Rongbuk Formation consists of a sequence of excessive-grade metamorphic and granitic rocks that were derived from the alteration of high-grade metasedimentary rocks. These leucogranites are a part of a belt of Late Oligocene-Miocene intrusive rocks referred to as the higher Himalayan leucogranite

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