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This study was initiated to explore the suitability of volcanic scoria from Mount Cameroon along the Cameroon Volcanic Line (CVL) in engineering applications. The mineral composition has been obtained through thin sections observation and XRD method. The XRF analytical methods have been used to determine major element composition. The studied rocks are dark gray to reddish in color with a vacuolar structure and porphyritic microlithic texture recalling the Strombolian dynamism. They are mainly made up of pyroxene, olivine, plagioclase, opaque minerals, quartz, magnetite and iddingsite. The presence of phenocrysts of olivine and clinopyroxene is due to mantle contamination. The main chemical components of scoria of Mount Cameroon are silica, alumina, iron and calcium oxides. The abundant vitreous phases are responsible for the acidic character revealed by high SiO 2 + Al 2 O 3 contents. Fe 2 O 3 , MnO and MgO are hosted by ferromagnesian minerals while SiO 2 , Al 2 O 3 , K 2 O, NaO and P 2 O 5 are found in acidic vitreous phases. The mineral and chemical composition of the scoria of Mount Cameroun is similar to those of scoria previously studied around the world. They can be used as absorbents for metals because of their high adsorption capacity and affinity for metals. The high SiO 2 + Al 2 O 3 + Fe 2 O 3 contents and low LOI values show that the scoria from Mount Cameroon are suitable to the use in cement and concretes. They can improve the resistance to sulfate, and chlorite and alkali silica reaction. According to the chemical composition, the rocks are conforming to French standard NFP18310. Their high CaO contents are favorable to improve the quality of scoria blended cements.
