Geology Atmosphere Jezero Crater Martian Atmosphere Geological History Geological Features Gale Crater Research Methods Mars Exploration Habitability Geological Processes Environmental Conditions Volcanic Activity Interior Structure Volcanoes Exploration Geological Activity Martian Geology Mars Missions Atmospheric Phenomena Atmospheric Conditions Climate Volcanology Surface Features Ice Composition Research Astrobiology Thermal Evolution Polar Regions Planet Characteristics Seasonal Changes Research Missions Marsquakes InSight Mission Tectonic Activity Evolution Life Sustainability Crust and Mantle Composition Interior Structure Analysis and Findings Martian Interior Possibility of Life Internal Structure Martian Seismic Data Core Composition Mantle Composition Magnetic Field Loss Seismic Activity Curiosity Rover Perseverance Rover Medusae Fossae Formation Water Ice Ancient Life Volcanism Eridania Region Mars' Hydrological Past Martian Climate Modeling Methods Resonance Glaciers Gully Landscapes Water Presence Landscape Formation Gullies Magnetic Field Seasonal Eruptions Imaging Technology Araneiforms Atmospheric Science Exploration Missions Manganese Sedimentary Rocks Ancient Environments Atmospheric Processes Microbial Activity Mineralogy Environment Comparison NASA Missions Historical Missions Martian Composition Mars Facts Mars Meteorites Formation Rover Missions Mars Imaging Mars Orbiters Space Missions Radar Technology Atmospheric Composition Radar Reflections Climate Dynamics Water Cycle Equatorial Region Water Frost Resources Water Significance Tharsis Volcanoes Atmospheric Dynamics Water Existence Water Resources
SuperCam measurements suggest the Jezero rim boulder formed beyond Mars, pending confirmation.