A 2.9 magnitude earthquake was reported in northwest Ohio on Sunday morning, felt in parts of northeast Indiana and surrounding areas. The earthquake’s epicenter was located near Hicksville, occurring at approximately 6:45 a.m. Residents in several cities reported feeling the tremors, demonstrating the reach and impact of seismic events even outside typical earthquake zones.
On Sunday morning, a 2.9 magnitude earthquake struck in northwest Ohio, with tremors felt as far away as northeast Indiana. According to the United States Geological Survey (USGS), the earthquake occurred approximately 0.5 miles south-southeast of Hicksville at around 6:45 a.m. This seismic event, classified as mb_L, measures the amplitude of seismic waves and is frequently utilized for earthquakes in the central and eastern regions of the United States. Reports indicated that residents in Angola, Ligonier, and Bluffton in Indiana, Bryan and Lima in Ohio, as well as Sturgis in Michigan experienced noticeable shaking.
Earthquakes, though less common in the Midwest compared to other regions in the United States such as California, can occur due to geological shifts. The measurement of earthquakes, specifically the mb_L type, is tailored to gauge seismic activities in the central and eastern states based on surface wave amplitudes. Understanding the nature and impact of such geological events is important for public awareness and safety, as even minor tremors can affect everyday activities and property.
In summary, the 2.9 magnitude earthquake that occurred in northwest Ohio serves as a reminder that seismic activity can affect regions not typically associated with earthquakes. Such events are monitored closely by geological agencies like the USGS, providing valuable information to the public regarding their occurrence and effects. It is essential for residents to stay informed about the potential for such events, especially in areas that may not expect to experience them.
Original Source: www.21alivenews.com
