The M 7.3 Nthrn Indonesia earthquake was caused by movement along a fault line in the earth's crust. This type of earthquake is known as a "strike-slip" earthquake, where two tectonic plates slide past each other horizontally.
The M 7.3 Nthrn Indonesia earthquake was classified as a major earthquake, with a magnitude of 7.3 on the Richter scale. This means it released a significant amount of energy and could potentially cause widespread damage.
It is possible that the M 7.3 Nthrn Indonesia earthquake is related to the earlier earthquake that occurred today, as they both occurred in the same region and within a short time frame. However, further analysis and research will be needed to determine the exact relationship between the two earthquakes.
As of now, there have been no immediate reports of damage or casualties from the M 7.3 Nthrn Indonesia earthquake. However, it is important to continue monitoring the situation and assessing any potential impacts.
Yes, there is a risk of aftershocks following the M 7.3 Nthrn Indonesia earthquake. Aftershocks are smaller earthquakes that occur in the same area after a larger earthquake. It is important for residents in the affected region to be prepared for potential aftershocks and follow any evacuation or safety protocols given by local authorities.