Although Kīlauea’s summit and East Rift Zone magma systems are connected, with changes at one sometimes leading to changes at the other, the Puʻu ʻŌʻō vent on Kīlauea Volcano’s East Rift Zone has shown no direct response to the recent overflows. However, HVO tiltmeters, GPS, web cameras, and field observations, continue to record inflation of Puʻu ʻŌʻō and the upper portion of the Episode 61g lava tube system, which could lead to the opening of a new vent on or near Pu‘u ‘Ō‘ō. If/when that happens, it is possible, even likely, that the summit lava lake will be affected, most likely by a significant drop in the lake level.