Recent observations from the James Webb Space Telescope reveal changes on Jupiter's moon Europa, indicating active geologic processes and an internal water source.
The presence of amorphous and crystalline ice on Europa's surface suggests the influence of an underground ocean nearly 30 kilometers beneath the icy shell.
Evidences like fractured surface materials and the presence of CO2 hint at processes pushing materials from Europa's interior ocean to the surface.
Europa's surface is affected by radiation from Jupiter's magnetic field, leading to disruptions in the crystalline structure of ice.
JWST's spectral studies show varying ice crystallization patterns on Europa, pointing to rapid resurfacing processes fueled by tidal heating and radioactive decay.
Discovery of crystalline ice in regions like Tara Regio challenges previous assumptions about Europa's surface composition and porous nature.
Unusual surface features, including evidence of sodium chloride and strange chemistry, suggest complex geologic activity below Europa's icy shell.
The formation of chaos regions on Europa may involve material upwelling through diapirs, leading to rapid freezing of water into crystalline ice.
Processes like plumes and impacts also play a role in delivering water and forming crystalline ice on Europa's surface, which is constantly evolving.
JWST's findings contribute to the growing evidence for a liquid ocean beneath Europa's icy surface, making it a dynamic and ever-changing moon.