Volcanic volumes associated with the Kenya Rift: recognition and correction of preservation biases
A. L. Guth, 2016. "Volcanic volumes associated with the Kenya Rift: recognition and correction of preservation biases", Magmatic Rifting and Active Volcanism, T. J. Wright, A. Ayele, D. J. Ferguson, T. Kidane, C. Vye-Brown
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New eruptive volume estimates have been calculated for the Kenyan segment of the East African Rift. Since the initial publications of volume estimates for the Kenyan Rift, numerous age dates have been obtained for the region allowing for temporal analysis of eruptive volumes. Additionally, more recent available datasets allow for the independent testing of map-derived volumes. Newly calculated volumes from available seismic data indicate a total volume of c. 310 000 km3, which is significantly more than map-derived volumes found here or published previously. It is suggested that the map-based estimates are likely affected by biases against recognizing small volume events in the older record. Such events have been, however, the main driver of erupted volume over the last 5 Ma. A simple ratio-adjustment technique was developed to counter these biases and results in convergence of the volume estimates from the two independent datasets examined.
Volume calculations and classifications are available at http://www.geolsoc.org.uk/SUP18800.
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Magmatic Rifting and Active Volcanism
A major rifting episode began in the Afar region of northern Ethiopia in September 2005. Over a ten-day period, c. 2.5 km3 of magma were intruded along a 60 km-long dyke separating the Arabian and Nubian plates. Over the next five years, a further 13 dyke intrusions caused continued extension, eruptions and seismicity. This activity led to a renewed international focus on the role of magmatism in rifting, with major international collaborative projects working in Afar and Ethiopia to study the ongoing activity and to place it in a broader context. This book brings together articles that explore the role of magmatism in rifting, from the initiation of continental break-up through to full seafloor spreading. We also explore the hazards related to rifting and the associated volcanism. This work has implications for our understanding of how continents break-up and the associated distribution of resources in rift basins and continental margins.