Credit: NASA |
Ice comes in different forms depending on pressures. “Ice I,” the least dense form of ice, is what floats in your chilled beverages. As pressures increase, ice molecules become more tightly packed and thus more dense. Because Ganymede’s oceans are up to 500 miles (800 kilometers) deep, they would experience more pressure than Earth’s oceans. The deepest and most dense form of ice thought to exist on Ganymede is called “Ice VI.”
The fact that salty water may persist at the bottom of the rocky seafloor, rather than ice, is favorable for the development of life. Researchers think life emerges through a series of chemical interactions at water-mineral interfaces, so a wet seafloor on Ganymede might be a key ingredient for life there.