This study aims to analyze the surface deformation of Mount Marapi, West Sumatra, after the December 3, 2023 eruption as an indicator of volcanic activity to support disaster mitigation. Sentinel-1A imagery (IW-SLC mode) from October 23, 2023 to January 15, 2024 was processed using SNAP and QGIS through the stages of coregistration, interferogram generation, topographic correction (SRTM DEM 30 m), phase unwrapping, and conversion to deformation with the Differential Interferometric Synthetic Aperture Radar (DInSAR) technique. The results indicate three deformation phases: slight pre-eruption deflation, significant inflation prior to the eruption, and post-eruption deflation. Maximum inflation of +0.84 m occurred during November 28–December 10, 2023, followed by deflation reaching –0.90 m from December 10, 2023 to January 15, 2024. Convergent vector directions toward the crater center indicate pressure accumulation caused by magma or gas migration, while pressure migration toward the southwest is associated with the eruption and the subsequent cold lahar event in May 2024. These findings are consistent with seismic and visual data from PVMBG/MAGMA Indonesia. Therefore, the DInSAR method is proven effective for monitoring volcanic deformation both spatially and temporally, and has strong potential to support data-driven early warning and disaster mitigation systems.