The social media age among Christians and their congregation

The social media age among Christians and their congregation.

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 “Awash is originating from Fentale area. Nothing was heard in Debre Berhan" - Atalai Ayele (Professor)

Yesterday at 10:46 pm, the website of the German Geoscience Research and Research Center released information that an earthquake of magnitude 4.9 occurred in Debre Berhan area. The same information was also reported.

Tikvah Ethiopia, on the other hand, has requested an explanation from the researcher in the field.

Is it true that there was an earthquake in Debre Berhan area? Atalai Ayele, a teacher and researcher of earthquake science in Addis Ababa, replied, "Oh, it's a lie."

"There is no Debre Berhan area. It is coming from the Awash Fentale area. Nothing has been heard from Deber Berhan," they said.

"In the information released by the institutions of the sector, they say, 'This many kilometers from Debre Berhan, or this many kilometers from Methara,' calling names. But in Meles, there is no such thing. Where is the tremor coming from Debre Berhan?"

The researcher explained to Tikvah Ethiopia that it does not mean that the location of the Awash Fentale area, which occurred 52 kilometers from Debre Sina, was prone to earthquakes.

"It is happening repeatedly in some areas, but nothing has been done," they said.

It is known that the earthquake that is happening in Awash Fentale is being felt in other cities including Addis Ababa.

On the other hand, at what level is the earthquake in the Awash Fentale area now? They responded further to what was presented to them today from Tikvah Ethiopia.

Atalai Ayele (prof.) What did you respond to?

"There's nothing different, it's still going on. It seems to change a little day by day. But it's not like it's going to stop tomorrow."

Still visible movement. In short, it doesn't look like it's raining. 

It's not that the website has been posted, but the area where about 10 happened last night is the same.

That is not the type of rain," he said.