Kyushu Island, situated along the volcanic front of the Ryukyu Arc, is characterized by significant volcanic activity that has persisted from the Neogene to present. Numerous large-scale calderas are found throughout Kyushu, which have experienced several major ignimbrite eruptions, such as VEI 8 class Aso-4 eruption. These caldera-forming eruptions are a result of extensive silicic magmatic activity within the island arc. Understanding the characteristics of the magmas involved in these eruptions, as well as the temporal evolution of the eruptions themselves, offers critical insights into the formation of large-scale felsic magma chambers and the processes that lead to magma evolution within them. Additionally, we can explore the triggers of these large-scale ignimbrite eruptions through geological and petrological evidence. By comparing the Late Pleistocene caldera volcanoes in Kyushu and their caldera-forming eruptions, we can develop a general model that outlines the development process of large-scale silicic volcanoes and identify the unique characteristics of individual volcanoes. This presentation will provide an overview of caldera volcano activity focused on Kyushu and introduce a general model for the development process of caldera volcanoes based on this research.