Mount Kinabalu is formed from granodiorite. This is an intrusive igneous rock, very similar to granite but with a different proportion of plagioclase and feldspar.
I took the photo below on my ascent to Laban Rata. Ascent, that is, as in climbing the stairs rather than something more skillful.
This is a view of Mount Kinabalu taken from the Park HQ in the evening. The sun has already set on the Park HQ but still illuminates the mountain top.
The day after we watched the bats stream out of the Mulu caves my guide took me to Deer Cave. On the way we passed this dry riverbed. I was quite surprised
Waiting for the sun to set and the bats of Mulu to take flight, mother nature treated us to this wonderful rainbow as a shower drifted across the hills.
To the right you can see examples of the limestone cliffs that feature in this area. Up in the hills in the top left corner you can see a collapsed surface. These highlight some of the challenges of hiking in this area. The terrain makes it extremely difficult but you could be hiking along and find yourself on the edge of a cliff. Being so far from help, that's why you stay on the trails.