Both are coastal indentations, but they differ in shape, origin, and regional usage.
| Feature | Firth | Bay |
|---|---|---|
| Definition | Long, narrow inlet; often a drowned river valley (ria) or glacial trough | Broad, curved indentation; wider than deep |
| Shape | Elongated, steep sides, often branching | Semicircular or U-shaped, gentle slopes |
| Formation | Glacial erosion (Scotland, Norway) or tectonic | Erosion of soft rock, sea-level rise, tectonics |
| Regional Usage | Scotland, Orkney, Shetland, Norway (“fjord”) | Worldwide (Chesapeake Bay, Bay of Bengal, San Francisco Bay) |
| Examples | Firth of Forth, Firth of Clyde, Moray Firth, Solway Firth | Bay of Fundy, Hudson Bay, Monterey Bay, Guanabara Bay |
| Salinity | Often estuarine (river influence strong) | Varies: marine, estuarine, lagoonal |
“Firth” is essentially a regional term (Scots/Norse) for a large estuary or fjord-like inlet. “Bay” is a general geomorphic term. A firth is a type of bay, but not all bays are firths. The boundary is linguistic and morphological, not strict.