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  2. Columbia River - Wikipedia

    en.wikipedia.org/wiki/Columbia_River

    The Columbia River ( Upper Chinook: Wimahl or Wimal; Sahaptin: Nch’i-Wàna or Nchi wana; Sinixt dialect swah'netk'qhu) is the largest river in the Pacific Northwest region of North America. [11] The river forms in the Rocky Mountains of British Columbia, Canada.

  3. Columbia Bar - Wikipedia

    en.wikipedia.org/wiki/Columbia_Bar

    The Columbia Bar is a system of bars and shoals at the mouth of the Columbia River spanning the U.S. states of Oregon and Washington. It is one of the most dangerous bar crossings in the world, earning the nickname Graveyard of the Pacific. The bar is about 3 miles (5 km) wide and 6 miles (10 km) long. [1]

  4. Skookumchuck Narrows - Wikipedia

    en.wikipedia.org/wiki/Skookumchuck_Narrows

    Each day, tides force large amounts of seawater through the narrows—760,000,000 m 3 (200 × 10 ^ 9 US gal) of water on a 3 m (9.8 ft) tide. The difference in water levels on either side of the rapids can exceed 2 m (6 ft 7 in) in height. Current speeds can exceed 16 knots (30 km/h; 18 mph), up to 17.68 kn (32.74 km/h; 20.35 mph).

  5. Columbia Plateau - Wikipedia

    en.wikipedia.org/wiki/Columbia_Plateau

    Columbia Plateau. Coordinates: 45°59′58″N 119°00′05″W. The Columbia Plateau covers much of the Columbia River Basalt Group, shown in green on this map. The Washington cities of Spokane, Yakima and Pasco, and the Oregon city of Pendleton, lie on the Columbia Plateau. The Columbia Plateau is a geologic and geographic region that lies ...

  6. San Juan Islands - Wikipedia

    en.wikipedia.org/wiki/San_Juan_Islands

    San Juan Islands (in white) and surrounding region. Location of the San Juan Islands. The San Juan Islands is an archipelago in the Pacific Northwest of the United States between the U.S. state of Washington and Vancouver Island, British Columbia, Canada. The San Juan Islands are part of Washington state, and form the core of San Juan County .

  7. Tidal bore - Wikipedia

    en.wikipedia.org/wiki/Tidal_bore

    A bore in Morecambe Bay, in the United Kingdom Video of the Arnside Bore, in the United Kingdom The tidal bore in Upper Cook Inlet, in Alaska. A tidal bore, often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current.

  8. Cascadia subduction zone - Wikipedia

    en.wikipedia.org/wiki/Cascadia_subduction_zone

    The Cascadia subduction zone is a 960 km (600 mi) fault at a convergent plate boundary, about 110–160 km (70–100 mi) off the Pacific coast, that stretches from northern Vancouver Island in Canada to Northern California in the United States. It is capable of producing 9.0+ magnitude earthquakes and tsunamis that could reach 30 m (98 ft).

  9. Head of tide - Wikipedia

    en.wikipedia.org/wiki/Head_of_tide

    Head of tide. Head of tide, tidal limit [2] or tidehead [3] is the farthest point upstream where a river is affected by tidal fluctuations, [4] or where the fluctuations are less than a certain amount. [5] The river section influenced by tides and marine forces but without salinity is a tidal river, while downstream areas are brackish and ...