The density of air is 1.3 kg/m3 at sea level. from your knowledge of air pressure at ground level, estimate the height of the atmosphere. as a simplifying assumption, take the atmosphere to be of uniform density up to some height, after which the density rapidly falls to zero. (in reality, the density of the atmosphere decreases as we go up.)

Is a  vector quantity  that refers to "the rate at which an object changes its position." imagine a person moving rapidly - one step forward and one step back - always returning to the original starting position. while this might result in a frenzy of activity, it would result in a zero velocity. because the person always returns to the original position, the motion would never result in a change in position. since velocity is defined as the rate at which the position changes, this motion results in zero velocity. if a person in motion wishes to maximize their velocity, then that person must make every effort to maximize the amount that they are displaced from their original position. every step must go into moving that person further from where he or she started. for certain, the person should never change directions and begin to return to the starting position.

The geological theory that states that pieces of earth's lithosphere are in constant slow motion is the theory of plate tectonics.