Niagara Falls: Border-Straddling, Surface-Water Fed, Not Groundwater
Niagara Falls straddles the U.S.–Canada border** — not "in Canada." The international boundary runs through the Horseshoe Falls. And its water is **100% surface water** from the Great Lakes system — not groundwater.
Water Source: The Great Lakes Superhighway
- Lake Superior → St. Marys River → Lake Huron
- Lake Huron → St. Clair River → Lake St. Clair → Detroit River → Lake Erie
- Lake Erie → **Niagara River** (58 km / 36 mi) → **Niagara Falls**
- Flow: 5,700 m³/s (200,000 cfs) average — 25% diverted for hydro
- Travel time: ~200 years for a water molecule from Superior to Falls
- Zero groundwater contribution at the falls — it's all lake outflow
Border Geography
- Horseshoe Falls (90% flow): Mostly in **Canada (Ontario)** — but border cuts through it
- American Falls + Bridal Veil Falls (10% flow): Entirely in **USA (New York)**
- Goat Island: Splits the river — US territory
- Boundary: 1908 treaty defined line; 1950 remedial works adjusted
Why Not Groundwater?
- Great Lakes = **glacial meltwater + precipitation** — surface origin
- Niagara River = **surface outflow** from Lake Erie
- Groundwater = **subsurface flow in aquifers** — contributes to lake levels indirectly, but not the river's direct flow
- Falls = **erosional knickpoint** cutting back through Lockport Dolomite caprock
Human Engineering
- 1950 Treaty: Minimum flow 100,000 cfs (day), 50,000 cfs (night) over falls
- Robert Moses / Sir Adam Beck plants: Divert 50–75% flow for power
- 1969 Dewatering: American Falls stopped 5 months — rock talus study
Niagara is a **binational, surface-water, treaty-managed, hydroelectric-engineered** wonder. Groundwater? Not in the equation.