integral
An integral is a way of adding up an infinite number of tiny pieces to get a whole. Picture the area under a curve — a hilly, irregular shape that no simple formula seems to fit. Slice it into countless paper-thin vertical strips, find the area of each, and add them all up. As the strips get thinner and thinner, the total settles on one exact answer: that answer is the integral. In short, it measures accumulation — how much something piles up.
This is why it shows up everywhere. Know how fast a car is going at every instant, and integrating that speed tells you the total distance traveled. Know the rate water flows into a tank, and the integral gives the total volume collected. Anytime a quantity builds up from a changing rate, the integral is the tool that sums it.
The deepest surprise is that integration is the exact reverse of the derivative — the operation that measures how fast something changes. This is the Fundamental Theorem of Calculus: differentiating undoes integrating, like multiplying undoes dividing. A common mistake is to think the integral is just "area" and nothing more; the area is the picture, but the real idea is accumulating a quantity from its rate of change.
The area under the curve f(x) from a to b — the accumulated total between those two points.
The elongated S sign ∫ is a stretched-out "S" for sum (Latin summa), introduced by Gottfried Leibniz in 1675; Newton had developed the same ideas independently about a decade earlier (his method of fluxions, c. 1665-66) but published later, sparking a bitter priority dispute.