Yesterday evening, the Awash region experienced its second earthquake of the day, marking the latest in a string of tremors affecting the area. The U.S. Geological Survey reported that this earthquake, which occurred at 6:20 p.m., registered a magnitude of 4.6 on the Richter scale. The tremor was felt by many residents in Addis Ababa, raising concerns about the recent increase in seismic activity.
The Awash Fentale area has now experienced five earthquakes over the past few days, causing widespread alarm among local residents and prompting the release of cautionary messages from various agencies. Authorities have advised residents to stay alert and follow any safety protocols issued by the Ethiopian government and relevant agencies, especially given that the quakes are being felt as far away as the capital, Addis Ababa.
In a statement from October 23, 2024, the Geophysics, Space Science, and Astronomy Institute at Addis Ababa University confirmed that a series of earthquakes of varying magnitudes had occurred in the Awash Fentale district. Professor Atalay Ayele, Head of the Sociology Department at Addis Ababa University, provided further insights into the events. He explained that the strongest earthquake of the day, which reached a magnitude of 4.6, was recorded at precisely 6:13 p.m. According to Professor Ayele, tremors from this quake were felt in different areas of Addis Ababa, although he emphasized that the lower magnitudes of these quakes meant they do not currently pose a major threat to residents.
Professor Ayele also noted that the Awash Fentale region is known for its tectonic activity, as it lies near the East African Rift, a zone where tectonic plates are gradually pulling apart. This geological context makes the area particularly susceptible to frequent, low-magnitude earthquakes, which are generally considered non-threatening but can sometimes cause alarm among residents unfamiliar with seismic activity. He highlighted the need for ongoing monitoring of the area to track any potential increases in earthquake frequency or intensity.
Gebretsadiq, Head of the Geology Department at Samara University, offered additional details on the nature of the earthquakes. Speaking to Fana Broadcasting Corporation (FBC), he explained that the recent tremors in the Awash Fentale region are likely connected to the movement of molten rock, or magma, beneath the Earth’s surface. As magma moves, it creates pressure on the surrounding rock formations, causing fractures and resulting in seismic activity. Gebretsadiq pointed out that the area’s geological characteristics, particularly its volcanic history, contribute to the likelihood of such activity.
Despite the increase in earthquakes, Gebretsadiq noted that predicting the duration or recurrence of these seismic events remains challenging due to the complex interactions of geological forces at play. However, he stressed the importance of preparing for potential future incidents by implementing public awareness campaigns to educate residents on earthquake preparedness and safety measures. He also highlighted the need for research to better understand the region’s seismic patterns, as more accurate information could help authorities and residents take appropriate precautions.
The Ethiopian government and local geological institutions have been coordinating to monitor the situation closely. Various agencies are also working on disseminating important information and guidelines to the public to ensure their safety. Residents have been advised to familiarize themselves with emergency response plans and to remain cautious, as even small-magnitude earthquakes can sometimes cause structural damage or, in rare cases, lead to larger seismic events.
In light of these developments, experts recommend that residents in Addis Ababa and surrounding areas prepare for the possibility of more earthquakes, even if they are of low magnitude. Simple safety measures, such as securing heavy furniture, identifying safe spots to take cover during a quake, and creating a basic emergency kit, can significantly increase resilience to seismic events.
The recent earthquakes in the Awash Fentale area have underscored the region’s vulnerability to tectonic activity. Geologists continue to study the area’s fault lines and volcanic structures to better understand the risks associated with living in a tectonically active zone. While there is currently no indication of an imminent threat, the frequency of recent tremors serves as a reminder of the need for preparedness and informed action.
Both local and international geologists are expected to collaborate on further studies, with a focus on evaluating the potential long-term impacts of these seismic activities on nearby communities. Until then, public vigilance and adherence to safety guidelines remain crucial for residents throughout the region.
