The present research was carried out in the Chemoga river sub basin in the Southern direction of Debre Markos town, North Western Ethiopia. The objective of the research was to investigate and map the geological construction materials following Chemoga river sub basin. To meet out the objectives of the present study, systematic and extensive field work was conducted. To detect the different lithologic formations and the contacts, surface exploration through selected travel lines was carried out and representative rock samples were collected for visual interpretations. Meter was used to quantify stratigraphic successions and the bedding thickness of the strata. Besides of this, literature review was undertaken to have a general background on the subject matter. In this study the potential and the spatial distribution of geomaterials are investigated and revealed on the map using mostly ArcGIS software. Hence, Basalt, Sandstone and Chert are the dominant lithogical units in the study area. Basaltic, Sandstone and Chert unit have existed with an average thickness of 115 m, 45 m and 30 m respectively. Basalt exposure is easily accessible, workable and the most dominant lithologic units in the study area. Moreover, sandstone unit has well exposed in a desirable potential and quality. Geometrically it forms, mostly steep rock faces which are difficult for quarrying process. Generally, a sandstone rock unit is surrounded by three major normal faults and inaccessible as compared to basalt unit. Chert is exposed on geographically limited area and rarely observed following stream cuts. Chert and basalt units are slightly to highly weathered and showed alterations on the surface. Finally, on the basis of the findings of the present research, recommendations are forwarded.