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Slip Point, Clallam Bay
Slip Point sits on the southern shore of the Strait of Juan de Fuca at the eastern end of Clallam Bay on the Olympic Peninsula, about 39 miles (63 km) west-northwest of Port Angeles and 0.7 miles (1 km) northeast of the community of Clallam Bay, Washington.
Terrace, Skeena River
Terrace, a community at the confluence of the Skeena and Kitsumkalum Rivers, lies about 71 miles (114 km) east-northeast of Prince Rupert and 64 miles (103 km) southwest of Hazelton, British Columbia.
Little Port Walter, Baranof Island
Little Port Walter is an embayment and research facility on the southern shore of Port Walter, situated on the southeastern coast of Baranof Island and the western shore of Chatham Strait, about 53 miles (85 km) south-southeast of Sitka and 9 miles (14.5 km) north of Port Alexander, Alaska.
Cowichan Bay, Vancouver Island
Cowichan Bay is a community situated on the south shore of an estuary shared by the Cowichan and Koksilah Rivers that form an extensive tidal flat on the east coast of southern Vancouver Island, about 26 miles (42 km) north-northwest of Victoria and 4 miles (6 km) southeast of Duncan, British Columbia.
Eagle River Flats, Knik Arm
Eagle River Flats is a 2,471‐acre (1,000‐ha) tidal flat and salt marsh at the mouth of Eagle River on Eagle Bay, on the eastern shore of Knik Arm at Joint Base Elmendorf–Richardson, about 10 miles (16 km) northeast of Anchorage and 7 miles (11 km) west of Eagle River, Alaska.
Stewart, Bear River
Stewart is a Canadian border community at the mouth of the Bear River and the head of Portland Canal, connected to Hyder, Alaska by 2 miles (3.2 km) of road, about 99 miles (159 km) east-southeast of Wrangell and 114 miles (183 km) north of Prince Rupert, British Columbia.
Coghill River, Dartmouth Glacier
The Coghill River in Chugach National Forest flows southwest for 5 miles (8 km) from the terminus of Dartmouth Glacier to Coghill Lake, which is 4.7 miles (7.5 km) long, and then runs west-southwest for 3 miles (4.8 km) to College Fjord near Coghill Point, about 54 miles (87 km) west of Valdez and 32 miles (51 km) northeast of Whittier, Alaska.
Gilttoyees Creek, Foch-Gilttoyees Provincial Park
Gilttoyees Creek originates in a series of cirque basins on the east and south flanks of Tentacle Peak in the Kitimat Ranges, and flows generally southeast for about 20 miles (32 km) through Foch-Gilttoyees Provincial Park and Protected Area before reaching Gilttoyees Inlet, which opens onto Douglas Channel, about 60 miles (97 km) southeast of Prince Rupert and 20 miles (32 km) southwest of Kitimat, British Columbia.
Clo-oose, Cheewhat River
Clo-oose is the site of an abandoned village of the Ditidaht First Nation on the southwest coast of Vancouver Island, above a beach 0.25 miles (0.4 km) west of the Cheewhat River mouth, about 20 miles (32 km) west-northwest of Port Renfrew and 19 miles (31 km) southeast of Bamfield, British Columbia.
Noatak River, Kotzebue Sound
Noatak River starts from several small cirque glaciers on the northeast flank of Mount lgikpak in the Schwatka Mountains and flows generally west for 425 miles (684 km) to Hotham Inlet in Kotzebue Sound, about 75 miles (121 km) southeast of Kivalina and 6 miles (10 km) north-northeast of Kotzebue, Alaska.
About the background graphic
This ‘warming stripe’ graphic is a visual representation of the change in global temperature from 1850 (top) to 2019 (bottom). Each stripe represents the average global temperature for one year. The average temperature from 1971-2000 is set as the boundary between blue and red. The colour scale goes from -0.7°C to +0.7°C. The data are from the UK Met Office HadCRUT4.6 dataset.
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