Bogotá, the capital city of Colombia, is the largest and most populous urban center in the country. Established in a moderate seismic zone, its complex topography facilitates the occurrence of landslides and floods. The city has been subject to a massive migration process in recent years, which has generated the accelerated urbanization of the city and increased its vulnerability to various natural hazards. Bogotá is located within the Sabana de Bogotá, a tectonic-sedimentary basin consolidated after the uplifting of the northern Andes approximately 5 Ma. With TerraSAR-X radar images, a quantitative analysis of the subsidence in the Sabana de Bogotá was carried out using the interferometric synthetic aperture radar technique for the city of Bogotá. The obtained results allowed establishing subsidence values in the central region of the city on the order of 3.3 cm/y. It is important to note that the BOGT GPS Continuously Operating Reference Station, which is part of a global network, indicates a decreasing value in its vertical component on the order of 3.5 ± 0.09 cm/y.