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Mount Kinabalu

Highest mountain in Malaysia

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Panoramic view of Mount Kinabalu during sunrise, from Kampong Kundasang, near Kinabalu Park entrance
kallerna · CC BY-SA 4.0

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Through Biodiversity, Sedimentary rock and Igneous rock

In 1997, a re-survey using satellite technology was conducted. It established Mount Kinabalu had a summit (known as Low's Peak) height of 4,095 m (13,435 ft) above sea level, some 6 m (20 ft) less than the hitherto-published figure of 4,101 m (13,455 ft).

The mountain and its surroundings have high biodiversity, with 5,000 to 6,000 species of plants, 326 species of birds, and over 100 mammalian species identified. Among this rich collection of wildlife are famous species such as the Rafflesia plants and orangutans.

Low's Peak can be climbed by a person in good physical condition without mountaineering equipment on the main route. However, climbers must be accompanied by accredited guides at all times due to national park regulations and the risk of experiencing altitude sickness.

Geology

Mount Kinabalu is a massive pluton formed from granodiorite that intruded into sedimentary and ultrabasic rocks, and forms the central part, or core, of the Kinabalu massif. The granodiorite is intrusive into strongly folded strata, probably of Eocene to Miocene age, and associated ultrabasic and basic igneous rocks. It was pushed up from the Earth's crust as molten rock millions of years ago. In geological terms, it is a very young mountain, as the granodiorite cooled and hardened only about 10 million years ago.

The present landform is considered to be a mid-Pliocene peneplain, arched and deeply dissected, through which the Kinabalu granodiorite body has risen in isostatic adjustment. It is still gaining roughly 5 mm (0.20 in) of height per year.

During the Pleistocene Epoch of about 100,000 years ago, the mountain was covered by sheets of ice and glaciers. As these glaciers flowed down its slopes, they scoured the surface of Mount Kinabalu in the process and creating the 1,800-metre-deep (5,900 ft) Low's Gully (named after Hugh Low) on its north side. Its granitic composition and the glacial formative processes are readily apparent when viewing its craggy, rocky peaks.

IUGS geological heritage site

Because it is "one of the youngest granitic intrusions exposed on Earth and the site of spectacular tropical glacial landscapes", the International Union of Geological Sciences (IUGS) included the Mount Kinabalu Neogene granite in its assemblage of 100 geological heritage sites around the world in a listing published in October 2022. The organisation defines an IUGS Geological Heritage Site as "a key place with geological elements and/or processes of international scientific relevance, used as a reference, and/or with a substantial contribution to the development of geological sciences through history."

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