An independent site about Canada as physical geography — the processes that made the ground
Autray
mrcautray.com
Five grounds · seventeen entries
Every entry is one place, located
Figures sourced or flagged
Section 02

The Tides

Sixteen metres, twice a day. A bay 270 kilometres long, shallowing toward its head, happens to slosh at almost exactly the period of the Atlantic tide. Everything else in this section follows from that coincidence, including the largest tidal range reliably measured anywhere.

The same rocky cove photographed at high water, wide, with a small boat afloat against a cliff, overcast Atlantic light
Plate IAt the mouth the bay behaves like any Atlantic coast. The range builds toward the head.Photo: Bay of Fundy · Wikimedia Commons

Entries in this section

4 entries
  • The Bay of Fundy

    The tide rises and falls by up to about sixteen metres twice a day because the bay's resonant period nearly matches the tide's and the water sloshes like a bath.

    44.28° N, 66.35° W → 45.30° N, 63.78° W · Tidal resonance
  • Burntcoat Head

    Where the largest range is reliably measured, and how a tidal range is measured at all.

    45.30° N, 63.80° W · Resonance at the bay head
  • The tidal bore

    A wave that runs upstream against the river when the flood tide overtakes it.

    45.3° N, 63.5° W · Translating hydraulic jump
  • Resonance

    The bay amplifies because its length and depth give it a natural period close to the tide's.

    45.3° N, 63.9° W · Frequency match, basin and tide