Volcanic activity and hazard in the East African Rift Zone
Abstract
Over the past two decades, multidisciplinary studies have unearthed a rich history of volcanic activity and unrest in the densely-populated East African Rift System, providing new insights into the influence of rift dynamics on magmatism, the characteristics of the volcanic plumbing systems and the foundation for hazard assessments. The raised awareness of volcanic hazards is driving a shift from crisis response to reducing disaster risks, but a lack of institutional and human capacity in sub-Saharan Africa means baseline data are sparse and mitigating geohazards remains challenging.
Citation
Biggs , J , Ayele , A , Fischer , T P , Fontijn , K , Hutchison , W , Kazimoto , E , Whaler , K & Wright , T J 2021 , ' Volcanic activity and hazard in the East African Rift Zone ' , Nature Communications , vol. 12 , 6881 . https://doi.org/10.1038/s41467-021-27166-y
Publication
Nature Communications
Status
Peer reviewed
ISSN
2041-1723Type
Journal item
Rights
Copyright © The Author(s) 2021. Open Access. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.
Description
J.B., K.F., K.W., T.W. and A.A. were supported by NERC Large Grant RiftVolc (NE/L013649/1, NE/L013932/1, NE/L013533/1, NE/L013649/1); A.A. acknowledges financial support of ISP (International Science Program) of Uppsala University. T.W., K.W. and A.A. were supported by NERC Afar Rift Consortium (NE/E007414/1, NE/E007147/1); K.F. acknowledges support from F.R.S.-FNRS MIS grant F.4515.20. W.H. acknowledges support from a UKRI Future Leaders Fellowship (MR/S033505/1). T.F. acknowledges US National Science Foundation GeoPRISMS grant 1654433.Collections
Items in the St Andrews Research Repository are protected by copyright, with all rights reserved, unless otherwise indicated.