1) Gravity surveys measure differences in gravitational attraction across Earth's surface. Denser rocks like iron pull down more strongly than less dense rocks like sand. 2) Geologists use gravimeters to detect these differences and map underground features without digging, such as springs, rivers, volcanic bases, and evidence of ice sheet loss. 3) Satellites also create gravity maps from space, showing areas of high and low gravitational pull that can reveal underground rock movements and ocean currents.