On January 12, 2020, Taal volcano, Philippines, erupted after 43 years of repose, affecting more than 500,000 people. Using interferometric synthetic aperture radar (InSAR) data, we present the pre- to post-eruption analyses of the deformation of Taal. We find that: (1) prior to eruption, the pressurization of its ∼5 km depth magma reservoir; (2) during the eruption, the magma reservoir lost a volcano experienced long-term deflation followed by short-term inflation, reflecting the depressurizationvolume of 0.531 ± 0.004 km3 while a 0.643 ± 0.001 km3 lateral dike was emplaced; and (3) post-eruption analyses reveal that the magma reservoir started recovery approximately 3 weeks after the main eruptive phase. We propose a conceptual analysis explaining the eruption and address why, despite the large volume of magma emplaced, the dike remained at depth. We also report the unique and significant contribution of InSAR data during the peak of the crisis. Plain Language Summary Taal volcano in the Philippines erupted on January 12, 2020. Here, we present the pre-, co-, and post-eruption data, model, and analyses using interferometric synthetic aperture radar (InSAR) data acquired by various satellite systems. We find that: (1) prior to the eruption, inflation as a result of the depressurization-pressurization of its ∼5 km depth magma reservoir; (2) the volcano experiences a sequence of long-term (>1 year) deflation followed by short-term (≤1 year) during the eruption, the magma reservoir lost a volume of 0.531 ± 0.004 km3 while a 0.643 ± 0.001 km3 starting ∼3 weeks after the main eruptive phase. We propose a conceptual analysis to explain the 2020 lateral dike was emplaced; and (3) post-eruption analyses reveal that the magma reservoir is in recovery Taal eruption and the dike emplacement. We also report the unique and significant contribution of remote sensing data, particularly InSAR during the peak of the crisis.