Abstract: A magnitude 7.3 earthquake occurred at 7:58 a.m. (Beijing time) on April 3, 2024, in the sea area of Hualien County, Taiwan Province, China (23.81°N, 121.74°E), which had a large seismic hazard impact and attracted widespread attention at home and abroad. This paper introduces the geological and tectonic background of the earthquake and its disaster influence, as well as the volcanic activity on Kueishantao volcano that partially collapsed as a result of the seismic effect, and focuses on a comprehensive analysis of the possibility of whether the earthquake will trigger the volcanic activity. Through the analysis of seismic and hyperspectral gas data, it can be seen that the Kueishantao volcano has not yet shown obvious anomalous responses. Then the probability of triggering is quantitatively judged by introducing the non-dimensional index of earthquake triggering potential volcanoes, and the TRIGI value is 19.8 (> 10), which indicates that the probability of earthquake-triggered eruption of Kueishantao volcano is relatively low in the short term. At present, the volcano is still in the state of dormancy from the analysis of qualitative and quantitative aspects. In the future, we will continue to collect and improve macro and micro precursor anomaly data before volcanic eruption, track and judge the state of volcanic activity, and draw more accurate and reliable conclusions about the triggering possibility.