The location and displacement of dyke-induced (and tectonic?) normal faults near the Ado'Ale Volcanic Centre in the Dabbahu-Manda Hararo Magmatic Segment of Afar, Ethiopia. The files include: 1) Dabbahu_fault_traces_2012_CM - this shapefile and associated files provides a map of fault traces mapped by Craig Magee (CM) using an airborne LiDAR survey acquired in November 2012 by the UK Natural Environment Research Council’s Airborne Research and Survey Facility (NERC ARSF) as part of the ET07/04: The Hararo Rift Segment in the Afar Triple Junction, and geohazards in the Afar capital, Semara project (see Hofmann, 2013 for acquisition and processing details; data available from https://catalogue.ceda.ac.uk/uuid/332dd80c62c16b42c2e87f588272b751). 2) Dabbahu_fault_data_2009 - this .csv file contains X, Y co-ordinates in the WGS 1984 UTM Zone 37N co-oridnate system that mark vertices for numerous faults. At each vertice, a measure of fault displacement (displ) in metres has been obtained. Fault mapping and displacement analysis were conducted on an airborne LiDAR survey acquired in October 2009 by the UK Natural Environment Research Council’s Airborne Research and Survey Facility (NERC ARSF) as part of the ET07/01: Earth crust grow at divergent plate boundaries project (see Hofmann, 2013 for acquisition and processing details; data available from https://catalogue.ceda.ac.uk/uuid/3e9e51d301962741d9ae32fce502dd48). The fault displacements measured constitute cumulative values of surface deformation accrued through multiple slip events since the initial breaching of breaking of the surface by the faults. This data was collected and processed by Barbara Hofmann during their PhD thesis (Hofmann, 2013), and has been quality controlled and modified by Craig Magee (2023). 3) Dabbahu_fault_data_Oct2008 - this .csv file contains X, Y co-ordinates in the WGS 1984 UTM Zone 37N co-oridnate system that mark vertices for numerous faults. At each vertice, a measure of fault displacement (displ) in metres has been obtained. These displaceemnt data were obtained by calculating surface displacement across the faults during a dyking episode in October 2008 using InSAR data (see Hofmann, 2013). This data was collected and processed by Barbara Hofmann during their PhD thesis (Hofmann, 2013), and has been quality controlled and modified by Craig Magee (2023). 4) Dabbahu_fault_data_2009-2012 - this .csv file contains X, Y co-ordinates in the WGS 1984 UTM Zone 37N co-oridnate system that mark vertices for numerous faults. At each vertice, a measure of fault displacement (displ) in metres has been obtained. Fault displacement was calculated by subtracting the two airborne LiDAR survey acquired in October 2009 and Novemer 2012 from each other to produce a differential LiDAR map detailing ground deformation accrued in the intervening 2009-2012 period (see Hofmann, 2013 for acquisition and processing details). This data was collected and processed by Barbara Hofmann during their PhD thesis (Hofmann, 2013), and has been quality controlled and modified by Craig Magee (2023). Reference: Hofmann, Barbara (2013) How do faults grow in magmatic rifts? LiDAR and InSAR observations of the Dabbahu rift segment, Afar, Ethiopia. PhD thesis, University of Leeds. https://etheses.whiterose.ac.uk/7546/
