Think of the money supply like a bathtub. The water level (money) can rise or fall depending on how much water is poured in or taken out. In an open economy, the main ways the “water level” changes are:
In short, the money supply rises when the central bank “pours in” more money or when banks lend more, and it falls when the opposite happens.
Commercial banks are like money gardeners. When you deposit £1,000, the bank keeps a small portion as reserve (say 10%) and lends out the rest. The loaned money is spent, then re‑deposited somewhere else, and the cycle repeats. This process creates new money that did not exist before.
Each round adds more money to the economy, even though the original deposit was only £1,000. That’s why banks are the main engines of credit creation.
The credit multiplier tells us how many times the initial deposit can be amplified through lending. It’s simply the reciprocal of the reserve ratio:
\$m = \frac{1}{r}\$
where r is the reserve ratio (expressed as a decimal).
| Reserve Ratio (r) | Multiplier (m) |
|---|---|
| 0.10 (10 %) | 10 |
| 0.05 (5 %) | 20 |
| 0.02 (2 %) | 50 |
Example: If the reserve ratio is 10 %, a £1,000 deposit can ultimately generate £10,000 in total money supply (1 000 × 10). The lower the reserve ratio, the higher the multiplier, and the faster the money supply grows.
In an open economy, foreign deposits and capital inflows feed into this multiplier mechanism, so changes in international confidence or exchange rates can have a big ripple effect on the domestic money supply.