We thank the USGS Hawaiian Volcano Observatory for help with accessing Kilauea seismicity data, Steven Andrews at Camborne School of Mines for help with the sedimentology and John Howell (Aberdeen) for the lend of a drone. John Still is thanked for help with the SEM at Aberdeen. DH and NF thank Katie and Dave Farrell for ‘baby-sitting’ services while the fieldwork was completed. We thank Craig Magee, Meredith Townsend and Dave Pollard for detailed and thoughtful reviews that helped us improve the manuscript. High-resolution orthomosaics can be found at https://doi.org/10.6084/m9.figshare.6849827.v2Peer reviewedPublisher PD
Most volcanic hazards depend on an injected dyke reaching the surface to form a feeder. Assessing th...
Field studies indicate that nearly all eruptions in volcanic edifices and rift zones are supplied wi...
Magma flow in a dike rising in a crack whose strike runs from a highland or a ridge to an adjacent l...
Seismological and geodetic data from modern volcanic systems strongly suggest that magma is transpor...
International audienceDuring intrusion of buoyant magma into a rift zone, it is a common belief that...
Crust at many divergent plate boundaries forms primarily by the injection of vertical sheet-like dyk...
We benefitted from discussions with many Earth scientists in different disciplines over the years; w...
gneous dykes are the main magma transport pathways through the Earth’s crust, and they are considere...
An important aspect of eruption forecasting is predicting the path of propagating dikes. We show how...
Understanding dykes is vital as they serve both as bodies that build the crust and as conduits that ...
Exposed rhyolitic dykes at eroded volcanoes arguably provide in situ records of conduit processes du...
The spatial distribution of eruptive vents around volcanoes can be complex and evolve as a volcano g...
Most volcanic hazards depend on an injected dyke reaching the surface to form a feeder. Assessing th...
Dykes are magma-driven extension fractures and the main conduits for magma in volcanic eruptions. To...
International audienceAt basaltic volcanoes, magma is transported to the surface through dikes (magm...
Most volcanic hazards depend on an injected dyke reaching the surface to form a feeder. Assessing th...
Field studies indicate that nearly all eruptions in volcanic edifices and rift zones are supplied wi...
Magma flow in a dike rising in a crack whose strike runs from a highland or a ridge to an adjacent l...
Seismological and geodetic data from modern volcanic systems strongly suggest that magma is transpor...
International audienceDuring intrusion of buoyant magma into a rift zone, it is a common belief that...
Crust at many divergent plate boundaries forms primarily by the injection of vertical sheet-like dyk...
We benefitted from discussions with many Earth scientists in different disciplines over the years; w...
gneous dykes are the main magma transport pathways through the Earth’s crust, and they are considere...
An important aspect of eruption forecasting is predicting the path of propagating dikes. We show how...
Understanding dykes is vital as they serve both as bodies that build the crust and as conduits that ...
Exposed rhyolitic dykes at eroded volcanoes arguably provide in situ records of conduit processes du...
The spatial distribution of eruptive vents around volcanoes can be complex and evolve as a volcano g...
Most volcanic hazards depend on an injected dyke reaching the surface to form a feeder. Assessing th...
Dykes are magma-driven extension fractures and the main conduits for magma in volcanic eruptions. To...
International audienceAt basaltic volcanoes, magma is transported to the surface through dikes (magm...
Most volcanic hazards depend on an injected dyke reaching the surface to form a feeder. Assessing th...
Field studies indicate that nearly all eruptions in volcanic edifices and rift zones are supplied wi...
Magma flow in a dike rising in a crack whose strike runs from a highland or a ridge to an adjacent l...