Axiomatic Permanence
Science works by assuming permanence. When a single obseration is made, it is assumed that the system remains stable and unchanging. Upon further observation, when change is noted, the nature of that change is assumed to be constant. When the nature of that change is itself modified, we must assume another, deeper permanence. Consider a ball: at first glance, we might guess the ball always sits there. Until we tilt the surface and it starts moving — at which point we might assume its movement is constant with respect to the incline of the plane. Until we see that it moves faster over time, and we discover acceleration. In a sense, we assume our present knowledge is constant until we are required to take the derivative: from position, to velocity, to acceleration. But the example doesn't stop here — if we travel high enough above the Earth, we'll note a difference in the acceleration. The question is: how deep does this rabbit hole go?