Since the Bay of Fundy becomes shallower and narrower, incoming tidal flows get forced especially high as water piles up behind mudflats at the mouth of the bay. Since North America, Europe, and Asia are pressed closer together than the continents in the Southern Hemisphere, water gets “constricted” in the Northern Hemisphere in a way that slightly amplifies tides. In addition, the position and configuration of continents in the Northern Hemisphere contributes to the high tides. The bay is just the right width and depth for water to slosh back and forth at a frequency-every 12 or 13 hours-that matches the natural frequency of high tides, which are driven by the gravitational pull of the Moon and Sun on Earth. The geometry of the bay causes tidal resonance, which plays a key role in elevating tides. coast has a tidal range of 1 to 2 meters (3 to 6 feet). With a tidal range up to 12 meters (38 feet), the funnel-shaped bay has the highest observed tides in the world. Sediment-rich waters are a common sight in the Bay of Fundy. On land, fall weather had transformed the foliage of hardwoods and other deciduous trees and shrubs.
On the afternoon of October 20, 2019, the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite captured this image of sediment-rich water in the Bay of Fundy, the Shubenacadie River, and other nearby waterways in far eastern Canada.
Their waters are often chocolate-colored, swirling with eddies, and bordered by red dunes and sandbars. From above, rivers that flow into the Bay of Fundy look a bit different than most.
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