Deadly Landslide Claims 14 Lives in Ethiopia’s Amhara Region

Ethiopia Landslide Kills 14 Near Historic Tsadkane Mariam Monastery in Amhara Region

NAIROBI — At least 14 people have died following a devastating landslide in Ethiopia’s Amhara region, state-affiliated media reported late Monday. The disaster struck near a significant religious site, prompting an urgent recovery operation involving heavy machinery.

Disaster Strikes Near Tsadkane Mariam Monastery

According to the Amhara Media Corporation, the slope failure occurred in the North Shewa Zone, specifically near the historic Tsadkane Mariam Monastery. The monastery, a revered Ethiopian Orthodox Tewahedo site, sits in a mountainous area known for its rugged topography, which becomes increasingly unstable during the wet season.

Emergency response teams, supported by excavation machinery, were immediately deployed to the scene to recover victims trapped beneath the debris. As of the latest reports, 14 bodies have been retrieved, though officials have not ruled out the possibility of additional casualties as search efforts continue.

Heavy Rains Identified as Primary Trigger

While the initial state media briefing did not specify the exact geological cause, independent reports and meteorological data indicate the catastrophe was triggered by torrential rainfall. Ethiopia is currently in the midst of its primary rainy season, known locally as the Kiremt, which typically spans from June to September.

During this period, the Ethiopian Highlands receive the vast majority of their annual precipitation. The intense saturation of soil on steep slopes drastically reduces cohesion, leading to frequent mass wasting events such as mudflows and rockfalls. Climate experts note that increasingly erratic weather patterns, potentially linked to broader climate change impacts on the Horn of Africa, are exacerbating the frequency and severity of these geological hazards.

Geological Vulnerability in the Ethiopian Highlands

The Amhara region, characterized by the Ethiopian Highlands—often called the “Roof of Africa”—is inherently prone to geohazards. The combination of:

• Steep terrain and deep incision by river valleys.
• High population density farming on marginal, sloped land.
• Deforestation and loss of vegetation cover which binds soil.
• Intense seasonal rainfall exceeding soil infiltration capacity.

…creates a high-risk environment for landslide susceptibility. The North Shewa Zone, where the Tsadkane Mariam Monastery is located, has a documented history of similar events during peak rainfall months.

Ongoing Rescue and Humanitarian Response

Local authorities and community volunteers are working alongside regional disaster prevention bureaus to manage the immediate aftermath. The deployment of heavy excavation equipment suggests the debris field is substantial, likely consisting of large boulders, saturated earth, and uprooted vegetation typical of deep-seated rotational slides in the region.

Humanitarian agencies operating in Ethiopia, including the UN Office for the Coordination of Humanitarian Affairs (OCHA), frequently highlight the need for improved early warning systems and land-use planning in highland communities to mitigate future loss of life during the Kiremt season.

Seasonal Context and Historical Precedent

This incident follows a grim pattern observed in recent years. In August 2023, a similar rain-triggered landslide in the Gofa Zone of the South Ethiopia Regional State claimed dozens of lives, ranking among the deadliest in the country’s recent history. Such recurring tragedies underscore the critical intersection of geology, climate, and socio-economic vulnerability in East Africa.

As the rainy season progresses through September, geological surveys and disaster risk management officials remain on high alert for further slope instability across the Amhara, Oromia, and Southern regions.

Key Facts at a Glance