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When they were formed, ice in the soil may have melted, turned the ground into mud, then flowed across the surface. Underground volcanism may have melted frozen ice; the water then flowed away and the ground collapsed to leave chaotic terrain. By discovering many geological forms that are typically formed from large amounts of water, they caused a revolution in our ideas about water on Mars. After orbiting Mars and returning images used for landing site selection, the orbiter and lander detached and the lander entered the Martian atmosphere and soft-landed at the selected site. The lander carried instruments to achieve the primary scientific objectives of the lander mission: to study the biology, chemical composition (organic and inorganic), meteorology, seismology, magnetic properties, appearance, and physical properties of the Martian surface and atmosphere. The primary objectives of the Viking orbiters were to transport the landers to Mars, perform reconnaissance to locate and certify landing sites, act as a communications relays for the landers, and to perform their own scientific investigations.
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