A diamicton covers at least 4 km2, and is interpreted as a Quaternary mudflow. The largest boulder is estimated to weigh 4700 t. The mudflow probably originated on the Pinosok Plateau on the eastern flanks of Mount Kinabalu.
CITATION STYLE
Leong, T. K. (1970). Bouldery mud flow deposit at Ranau, Sabah, East Malaysia. Bulletin of the Geological Society of Malaysia, 3, 139–146. https://doi.org/10.7186/bgsm03197012
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