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Tag: Crocker

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Kinabalu via Timpohon Day 2 - Low's Peak

Kinabalu Index

The Ascent


No matter how early one goes to bed, one can never get enough sleep in Laban Rata (elevation : 3272m). 'Supper', which is a simple and light meal of bread, rice or noodles, is served at 02:00, and the hike to the summit starts in darkness not too long after. I joined a long procession of hikers that were armed with headlamps and bundled in jackets, that made their way up the trail, all of them eager to make the 1.5 kilometres to 'Sayat Sayat Hut' (elevation : 3668m) before the 05:00 cut-off time. Read more
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Kinabalu via Timpohon Day 1 - To Laban Rata

Kinabalu Index

Ferns Abound!


We made our way to Timpohon Gate (elevation : 1866m) with perfect weather that morning, and sat in the shuttle van satiated after a heavy breakfast from Balsam Cafe. With both a packed lunch and our climbing permits in hand, we went to the counter to sign-in before we set off down the trail. By then, it was 09:10. The very wide 'trail' was more of a stairwell through the jungle than an actual trail. It began with a short descent to the tiny Carson Waterfall, before beginning a long ascent to Laban Rata (elevation : 3272m), which was 1350 metres higher up and 6 kilometres further along the trail. Read more
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Mount Kinabalu

Kinabalu Day 1 : Timpohon Gate to Laban Rata
Kinabalu Day 2 : Laban Rata to Low's Peak

Mount Kinabalu


UNESCO Mount Kinabalu (elevation : 4095m) is the highest mountain in Malaysia (both by prominence as well as sheer elevation), and is also the highest mountain between the Himalayas and New Guinea. Based on topographic prominence, Mount Kinabalu also happens to be the 20th highest mountain in the world, but only the third highest mountain in Southeast Asia behind Hkakabo Razi (elevation : 5881m) in Myanmar, and Puncak Jaya (elevation : 4884m), also known as Carstensz Pyramid, in Indonesia. Mount Kinabalu is basically a massive granite intrusion (or a pluton to be precise) that was formed when magma solidified underground before being thrust upwards through the Earth's crust by tectonic movements millions of years ago. Read more