If Earth had lost its magnetic field 4 billion years ago and lacked geological activity, its atmosphere could have been significantly thinner, potentially resembling that of Mars. The absence of a magnetic field would have allowed solar wind to erode the atmosphere over time, although Earth's gravity might have retained some gases. In contrast, Venus, despite lacking a magnetic field, has a thick atmosphere due to its geological activity and an active ionosphere that protects it from solar wind. The discussion highlights that without geological processes, Earth's atmosphere would likely be less dense, but its mass could still allow for a thicker atmosphere than Mars. Overall, the interplay of gravity, geological activity, and magnetic fields is crucial in determining atmospheric retention on planets.