A petrographic analysis was conducted to identify the mineral contents containing in the rock samples collected at study area located in Lojing, Gua Musang. The geology of the study area consists of metasedimentary rocks. There are six hand specimens collected and analysed using petrographic microscope. The limestone and carbonate rock is found at the study area. It has been subjected to some stress to such an extent that some of the grain boundaries have been modified by pervasive pressure solution of stylolites. Pressure solution is the process whereby this limestone has undergone selective dissolution to the extent that the grain boundaries were modified into thin dark n sutured seams. The rocks contain also microcrystalline to cryptocrystalline silica clasts which occur dispersed throughout the matrix. The petrographic analysis results show that the minerals contain in the six rock samples are micrite, bioclast, microspars, deformed quartz, K-feldspar, lithic and clayey carbonate lithic. The major minerals contained in the rocks are micrite and bioclast.

The research area was completed in the Upper Triassic and is situated in the Bentong-Raub suture zone of the Upper Permian collision zone between the Sibumasu and Indochina plates. Geoheritage must be preserved for educational reasons in order to preserve the geological processes that create different lithologies as well as the geological structures that create distinctive geomorphology. Geological features can be utilized for geotourism and have geoheritage significance. The purpose of this study is to evaluate the geoheritage component in the Malaysian Kelantan region of Lojing Gua Musang. The classification of geoheritage is based on factors related to geodiversity, scope, and scale. A minor geodiversity of lithological changes in metamorphic rocks, sediments, and volcanic rocks (as members of chert lithology) represent the structure’s position. The minor geodiversity of lithological changes in metamorphic rocks, sediments, and volcanic rocks (as members of chert lithology), with a score of 4, represents the structure’s location (good). Scientific geosite values, such as the numerous lithologies that characterize the Bentong Raub Suture Lojing region, have a rich geological history that makes them appealing to tourists and researchers.