This web application is used for generating a 3D slab model following the procedure of Hayes et al., 2018. If using models generated from this web application, please cite Hayes et al., 2018 and Haynie et al., 2020 (AGU abstract). Instructions for plotting the model results can be found in the Slab2 code documentation and GitHub repository.
To generate a slab model, please enter your email address, select a slab region (refer to the map on the right), choose if you would like to model the surface to the top of the slab or the center of the slab, and lastly choose the Slab2 database you would like to use for creating your model. Once submitted, the form will refresh and you will receive an email.
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Subduction zones are home to the most seismically active faults on the planet. The shallow megathrust interface of subduction zones host our largest earthquakes, and are the only faults capable of M9+ ruptures. Despite these facts, our knowledge of subduction zone geometry - which likely plays a key role in determining the spatial extent and ultimately the size of subduction zone earthquakes - is - Publications
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A three-dimensional compilation of global subduction geometries, separated into regional models for each major subduction zone.