The Qinghai-Tibet Plateau (QTP) is highly affected by rainfall-induced mass-movements (i.e., landslides, debris flows, rock falls) due to its geomorphological and climatic characteristics and anthropogenic activities. However, understanding these events and their triggering characteristics remains limited due to scarce hazard inventories and rain gauge measurements. Using a well-documented dataset of mass-movements (2001–2022) and satellite rainfall estimates, this study comprehensively analyzes the temporal and spatial patterns of the events and their triggers. Results confirm rainfall as the dominant factor, accounting for most fatalities and damages, with antecedent rainfall on the day of occurrence and 7 days prior playing a key role in triggering. Empirical rainfall thresholds at different non-exceedance probabilities, calculated for the first time in QTP, exhibit high parameter robustness and detection capacity. A new methodological approach to evaluate the temporal evolution of the triggering rainfall thresholds reveals a pronounced decreasing trend over the last decade, indicating that the QTP landscape has been experiencing more favorable triggering conditions for mass-movements, particularly under prolonged rainfall. Spatial variations in rainfall triggering conditions were found in several environmental subregions, demonstrating the adaptation of the landscape to different predisposing conditions, with lower-frequency areas showing lower thresholds. This work advances the knowledge of rainfall-induced mass-movements in this peculiar high-mountain area and may lay the foundation for the implementation of operational warning systems for mass-movements in the Third Pole.