Chatham Sound


Chatham Sound is a sound on the North Coast of British Columbia, Canada, bordering on Alaska, United States. It is located between the Dundas and Stephens Islands and the Tsimpsean Peninsula near Prince Rupert. It is part of the Inside Passage and extends from Portland Inlet in the north to Porcher Island in the south.
It may have been named in 1788 by British Captain Charles Duncan after John Pitt, 2nd Earl of Chatham, who was First Lord of the Admiralty at that time.

Geography

Chatham Sound is a semi-enclosed basin with an area of about. It is connected to the open waters of the Hecate Strait and Dixon Entrance via several channels, such as Main, Brown, Hudson Bay, and Edye Passages. Along its southern end, the sound provides access to inland passages such as the Marcus and Arthur Passages, and the Grenville Channel beyond that.
The two major rivers that drain into the sound are the Nass River and Skeena River. Because of the large inflow of fresh water the salinity of the sound is lower than the adjacent ocean.

Hydrography

Most of Chatham Sound is less than deep, except in the northern part of the sound where depth exceeds.
Chatham Sound is an area of very large tides, with tidal ranges reaching peak values of and an average tidal range of,
tidal currents are proportionately strong, especially in the south and west areas.

Ecology

As a result of tidal mixing, Chatham Sound is an area of particularly high primary productivity and highly concentrated phytoplankton biomass.
The sound has the largest diversity of shrimp species in the Pacific North Coast Integrated Management Area, with numbers dominated by humpback shrimp.
There are also major aggregations of Dungeness crab in the area.
Once thought to be extinct, sponge reefs are now known to be a significant component of the sound floor. The largest cluster is now designated the Chatham Sound Reef Complex.

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