Accessible records of past volcanic eruptions, unrest and associated geophysical signals are important for understanding new activity. The COMET Volcano Deformation Catalogue is an effort to bring together records of displacement at volcanoes, both published and unpublished. As well as providing context for signals in Sentinel-1 interferograms, we hope that the catalogue will provide a forum for the recording of observations for posterity, including those that are ambiguous or record a lack of deformation. We consider good records of ‘null’ results (i.e. where measurement uncertainty and time span of observation are documented) to be critical for any future probabilistic analyses of relationships between deformation and unrest or eruption.
This website welcomes community contributions – if you would like to add an entry please contact us for a contributor login to the website. We welcome contributions that could be referenced as ‘personal communications’, unpublished student theses, conference abstracts and observatory reports. We use the volcano names, numbers and locations as recorded in the GVP VOTW database in an effort to ensure future compatibility (GVP, Global Volcanism Program, 2013). However, unlike the VOTW database most entries recorded here are in ‘free text’ format, to allow maximum flexibility in the information that can be recorded.
The motivation of the COMET Volcano Deformation Catalogue and relationship to
the deformation entries in the Smithsonian Institution Global Volcanism Program’s
Volcanoes of the World relational database is described in more detail by Ebmeier
et al., (2018). A ‘snapshot’ of the catalogue after its last comprehensive update
showed that so far, InSAR detections of volcanic deformation characteristically last
more than a few months, but less than a decade, and extend between hundreds of metres
and hundreds of kilometres. However, short-lived, low rate and off-centre episodes of
volcano deformation are likely to be under-represented in historical InSAR and
ground-based deformation records. The abundance of deformation signals that occur
kilometres away from volcanic centres demonstrate the ubiquity of off-centre magma
storage (Ebmeier et al., 2018).