The fate of northern Krakatoa has been the subject of some dispute among geologists. It was originally proposed that the island had been blown apart by the force of the eruption. Most of the material deposited by the volcano is clearly magmatic in origin, and the caldera formed by the eruption is not extensively filled with deposits from the 1883 eruption. This indicates that the island subsided into an empty magma chamber at the end of the eruption sequence, rather than having been destroyed during the eruptions.