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The Central Valley watershed feeding into Suisun Bay via the Sacramento–San Joaquin Delta is excluded; see the following section for the Sacramento and San Joaquin river systems. For additional detail on Bay Area creeks, see List of watercourses in the San Francisco Bay Area .
Beluga whales within James Bay basin could be distinct from those found in Hudson Bay. [5] Hundreds of rivers flow into James Bay. The geography of the region gives many of them similar characteristics. They tend to be wide and shallow near the Bay (in the James Bay Lowlands), whereas they are steeper and narrower farther upstream (as they pour ...
This page was last edited on 23 December 2018, at 15:34 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
It proposed damming James Bay, using the techniques of the Zuiderzee/IJsselmeer, to prevent its waters mixing with the salt water of Hudson Bay to the north. This would produce an enormous freshwater lake, some of which would be pumped south into Georgian Bay where it would increase the freshwater levels of the lower Great Lakes.
Southern James Bay is a coastal wetland complex in northeastern Ontario, Canada bordering James Bay and Quebec. It was designated as a wetland of international importance via the Ramsar Convention on May 27, 1987. The shallow waters of the James Bay region represent an important late autumn staging area for migratory, Arctic-breeding waterbirds ...
The river travels 63 miles (101 km) from its headwaters on the west side of the North Coast Range to its confluence with the Eel River, about 14 miles (23 km) upstream from the Pacific Ocean and 17 miles (27 km) south of Eureka, California. The river's elevation is over 5,000 feet (1,500 m) at its source and only 60 feet (18 m) when it merges ...
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These watercourses (rivers, creeks, sloughs, etc.) in the San Francisco Bay Area are grouped according to the bodies of water they flow into. Tributaries are listed under the watercourses they feed, sorted by the elevation of the confluence so that tributaries entering nearest the sea appear first.
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