General geology, facies and depositional environment of Kampung Temang, Kuala Krai, Kelantan

This study focused on the geological mapping of Kg Temiang, Kuala Krai, Kelantan, facies depositional environment and geological history and evolution of that place. Facies analysis shows the finer grained of sedimentary rock with a few of sediment structure such as massive, lamina, and cross-lamination. This place shows a shallow shoreface environment. However, the geomorphology process usually because of faulting, crack and bedding. In addition, it also because of climate change that control weathering and erosional process. Kg Temiang contain one type of rock which is sedimentary rock. The lithology of the area are shale, sandstone, mudstone, limestone and siltstone. They are included in Mesozoic era.