Mount Kinabalu is essentially a massive pluton formed from granodiorite which is intrusive into sedimentary and ultrabasic rocks, and forms the central part, or core, of the Kinabalu massif. The granodiorite is intrusive int… See more

The climate of the mountain varies from humid tropical at its base to alpine at its summit. The temperature at the summit of Mount Kinabalu usually stands from −4 to 8 °C (25 to 46 °F) from December to January, and 3 to 1… See more