Geologists have confirmed that the African continent is being torn in two, forming a new ocean. An international collaboration has shown that a 35 mile long rift in the Afar region of the Ethiopian desert, which opened in 2005, is likely to be the beginning of a new sea. The recent study, published in the journal Geophysical Research Letters , brings together seismic data from the formation of the rift, showing that it is driven by similar processes to those at the bottom of oceans. African and Arabian tectonic plates meet in the desert, and have been slowly pulling apart for roughly 30 million years. The same movement has also been parting the Red Sea . But this is only at a speed of less than 1 inch per year. The sudden cracking in 2005, referred to by geologists as a "mega-dike intrusion", opened up a rift over 20 feet wide in places. The study has found that this happened over only a few days. According to Cindy Ebinger, a co-author of the study from the University of Rochester : "We know that seafloor ridges are created by a similar intrusion of magma into a rift, but we never knew that a huge length of the ridge could break open at once like this." The investigation was led by Professor Atalay Ayele of Addis Ababa University in Ethiopia. As well as Rochester, other groups involved included Eritrea Institute of Technology; National Yemen Seismological Observatory Center; University of Leeds , United Kingdom; Institut de Physique du Globe de Paris , France; and Columbia University , New York.
Geologists have confirmed that the African continent is being torn in two, forming a new ocean. An international collaboration has shown that a 35 mile long rift in the region of the Ethiopian desert, which opened in 2005, is likely to be the beginning of a new sea. The recent study, published in the journal , brings together seismic data from the formation of the rift, showing that it is driven by similar processes to those at the bottom of oceans. African and Arabian meet in the desert, and have been slowly pulling apart for roughly 30 million years. The same movement has also been parting the . But this is only at a speed of less than 1 inch per year. The sudden cracking in 2005, referred to by geologists as a "mega-dike intrusion", opened up a rift over 20 feet wide in places. The study has found that this happened over only a few days. According to Cindy Ebinger, a co-author of the study from the : "We know that seafloor ridges are created by a similar intrusion of magma into a rift, but we never knew that a huge length of the ridge could break open at once like this." The investigation was led by Professor Atalay Ayele of in Ethiopia. As well as Rochester, other groups involved included ; ; , United Kingdom; , France; and , New York.
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Afar
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Geophysical Research Letters
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tectonic plates
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Red Sea
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University of Rochester
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Addis Ababa University
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Eritrea Institute of Technology; National Yemen Seismological Observatory Center; University of Leeds
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Institut de Physique du Globe de Paris
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Columbia University