The 6.8 Mw earthquake occurred in the eastern provinces of the Democratic Republic of the Congo, primarily affecting the areas surrounding Lake Tanganyika. This tectonic event was part of the larger East African Rift system, which is characterized by a series of rift valleys resulting from the divergent movement of tectonic plates. The earthquake struck with a maximum Mercalli intensity of X, classified as 'Extreme,' indicating severe shaking and destruction. The impact was particularly pronounced in urban areas where infrastructure could not withstand the intensity of the quake. Although only six deaths were officially reported, the actual number may have been higher due to the difficulties in accessing remote areas and reporting fatalities. Emergency services were quickly mobilized to assess the damage and provide aid to the affected populations. The response highlighted both local and international efforts to assist communities faced with such natural disasters.In the aftermath of the earthquake, critical infrastructure suffered significant damage. Schools, hospitals, and homes were rendered uninhabitable, forcing many residents to seek temporary shelter. The quake aggravated pre-existing vulnerabilities, as the region was already grappling with the consequences of prolonged conflict and economic challenges. Humanitarian organizations responded urgently, providing food, medical assistance, and essential supplies. Recovery efforts were complicated by the region's political instability and the ongoing humanitarian crisis. Despite these challenges, the disaster underscored the resilience of the local communities and their capacity to rebuild with external support. The earthquake also prompted discussions on the importance of disaster preparedness in regions prone to seismic activity, leading to calls for improved building standards and early warning systems.