Part of the Imhotep region showing the location of water ice deposits
Part of the Imhotep region showing the location of water ice deposits
Along the bottom, broken edge of this roughly semi-circular structure, which is approximately 300 metres across and located at the boundary of the Imhotep region on Comet 67P/Churyumov-Gerasimenko, is one of the areas where water ice was detected on the comet’s surface. It is assumed to have been exposed by erosion processes.
