The Mean Value Theorem
Imagine you drive Delhi to Agra — 200 km — in exactly 4 hours, so your average speed is 50 km/h. Was your speed exactly 50 km/h at some instant? If your motion was smooth, the Mean Value Theorem says yes. That is its soul: it links the average rate of change of a function over an interval to its instantaneous rate at some point inside.
The Intuition
Think of f(x) as a smooth path from x=a to x=b. The average rate of change is the slope of the chord joining the endpoints:
Average slope=b−af(b)−f(a)
If the path has no sharp corners or breaks, then at some interior point the tangent's slope must exactly equal this chord slope — geometrically, the tangent there is parallel to the chord. (If you always went slower than average you'd never arrive; always faster and you'd overshoot — so you must hit the average at least once.)
The Precise Statement
If f is
- continuous on [a,b], and
- differentiable on (a,b),
then there exists at least one c∈(a,b) with
f′(c)=b−af(b)−f(a)
Continuity means no breaks; differentiability means a well-defined tangent at every interior point — no corners, no vertical tangents.
A Simple Example
Take f(x)=x2 on [1,3]. The average slope is 3−19−1=4, and f′(x)=2x. Setting 2c=4 gives c=2∈(1,3), and indeed f′(2)=4.
The theorem guarantees existence, not uniqueness — there may be more than one such c.
Why It Matters …