The aim of the study is to conduct detailed geological, petrographic, and mineralogical examinations of the basaltic scoria and lavas outcropping in Turkmen Village, Toprakkale District, Osmaniye Province. The mineralogical and petrographic compositions, as well as textural characteristics of these rocks, have been revealed, and the existing mineralogical components have been identified in the conducted studies. Basic composition rocks in the study area are generally found in three types: pyroclastic, vesicular basalt (scoria), and columnar basalt (massive). The first type of basic character pyroclastic rocks observed typically consist of volcanic scoria, tuff, and volcanic bombs with diameters of up to approximately 1 m. The second type of volcanic product in the region is the vesicular (scoria) levels. It has been determined that beneath the scoria-containing rocks, there are occasionally massive structures. Basalts (scoriamassive) generally exhibit an intergranular porphyritic texture and an ophitic texture, and it has been determined that scoria-type rocks contain abundant cooling gas voids. Conversely, massive-type basic volcanic rocks devoid of voids consist of olivine, pyroxene, and plagioclase microlites and are observed to have an average thickness of 1.5-2.2 meters over the observed volcanic rocks in scoria type.