New composite images made from NASA's Cassini spacecraft data are the most detailed global infrared views ever produced of Saturn's moon Enceladus. And data used to build those images provides strong evidence that the northern hemisphere of the moon has been resurfaced with ice from its interior. During Cassini's 13-year exploration of the Saturn system, the spacecraft's Visible and Infrared Mapping Spectrometer (VIMS) collected light — both visible to the human eye and infrared light — reflected off the planet, its rings, and its 10 major icy moons. VIMS then separated light into its various wavelengths, information that tells scientists more about the makeup of the material reflecting it. Combined with detailed images captured by Cassini's Imaging Science Subsystem, the VIMS data was used to make the new global spectral map of Enceladus. It shows that infrared signals correlate with the geologic activity known to be ongoing at the south pole, where plumes of ice grains and vapor shoot out from an ocean that lies under the icy crust. The so-called "tiger stripe" gashes, where the plumes originate, are seen here. But some of the same infrared features are also seen in the northern hemisphere. That tells scientists not just that the northern area is covered with fresh ice but that the same kind of geologic activity, a resurfacing of the landscape, has occurred in both hemispheres. The resurfacing in the north may be due to icy jets, or a more gradual movement of ice through fractures in the crust, from the subsurface ocean to the surface. Movie available at https://photojournal.jpl.nasa.gov/catalog/PIA24023