In March 2022, we conducted a fieldwork at the islands of San Benedicto and Socorro, two volcanoes of the Revillagigedo Archipelago that is located ~500 km west of the Mexian mainland. These are active volcanoes that have formed since the Pleistocene on a mid-oceanic ridge that has been extinct for about 2 million years. I assembled a team of 10 outstanding geologists to turn these islands inside out. The primary idea – the source of the funding – was to test the longevity of former mantle wedges, which form above subduction zones, after subduction stops. At a depth of 1500 km in the lower mantle below the Revillagigedo Islands, a slab is located that sudbucted 180 million years ago, during which time an arc formed that we believe is the Bonanza Arc of Vancouver Island. We have sampled sandstones from the Bonanza arc to test what the signature of zircons is that were transported to the trench at that time, and we sampled volcanic rocks and river and beach sands of Socorro and San Benedicto to test whether the geochemical subduction signature and the zircon signature are still detectable. If so, we obtain a surprising, and important constraint on the rate of upper mantle convection. In addition, we took samples for, and studied the explosiveness of the eruptions for volcanic and tsunami hazard assessment, as well as to study the intensity of the Earth’s magnetic field. Below you will find a picture impression of the most amazing fieldwork I have done to date – the people, the scenery, the activities, and the amazing wildlife.