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Opens on Chapter 5’s example: 30 miles at 30 mph and 30 at 60; a camera pair 3 miles apart, 2 min 40 s; a ball falling d = 16t².
How it works
Average speed is total distance ÷ total time, never the average of the speeds: slow legs take longer, so they count for more. On a graph the average rate between two points is the slope of the secant, the straight line through them. The mean value theorem says, in plain words, that on a smooth trip you were going at exactly your average speed at least once; that's why an average-speed camera's reading is a fair one. Shrink the interval toward one point and the secant slopes settle on the slope at that point: Chapter 6's idea.
Numbers can be typed as 1,450, $38, 0.40, 12%, 1/6 or 2 3/8. Functions can be typed as 16t², 6 + 48t − 16t^2, 1000e^(0.05t) or √x; answers are rounded half up, the way the book rounds. Everything stays in your browser: no sign-up, nothing stored or sent.