Rivers

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Leque Island, South Pass Stillaguamish River

Leque Island is located at the mouth of the Stillaguamish River on South Pass channel that separates Camano Island from the mainland, about 43 miles (69 km) north of Seattle and 0.6 miles (1 km) southwest of Stanwood, Washington.

North Dawes Glacier, Endicott Arm

North Dawes Glacier starts from the Stikine Icefield at an elevation of about 5,200 feet (1,585 m) on the western flank of Sheppard Peak and flows generally southwest for 15 miles (24 km) to a proglacial lake at an elevation of 1000 feet (305 m) which is 2 miles (3.2 km) long and drained by a stream 1.3 miles (2.1 km) long at the head of an inlet extending north from Endicott Arm, about 74 miles (119 km) southeast of Juneau and 51 miles (82 km) north of Petersburg, Alaska.

Cape Espenberg, Seward Peninsula

Espenberg is a historic Iñupiaq settlement and present-day fish camp at Cape Espenberg, a peninsula composed of a series of dune-covered beach ridges on the Chukchi Sea coast of the Seward Peninsula that extends eastward into Kotzebue Sound, about 63 miles (101 km) east-northeast of Shishmaref and 43 miles (69 km) southwest of Kotzebue, Alaska.

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Alamere Falls, Point Reyes National Seashore

Alamere Falls, Point Reyes National Seashore

Alamere Falls is located in the Phillip Burton Wilderness of Point Reyes National Seashore, about 6 miles (10 km) south of Olema and 6.4 miles (10.3 km) northwest of Bolinas, California.

Haysport, Skeena River

Haysport, Skeena River

Haysport is the site of a historical community and salmon cannery on the north shore of the Skeena River adjacent to the Grand Trunk Railroad, about 61 miles (100 km) southwest of Terrace and 16 miles (26 km) southeast of Prince Rupert, British Columbia.

Old Valdez Townsite, Valdez Glacier Stream

Old Valdez Townsite, Valdez Glacier Stream

Old Valdez was the original townsite of Valdez built on the outwash plain formed by Valdez Glacier which is drained by Valdez Glacier Stream that flows generally south-southeast for 4.5 miles (7 km) to Port Valdez in Prince William Sound, about 43 miles (69 km) north-northwest of Cordova and 3.7 miles (6 km) southeast of Valdez, Alaska.

Eek River, Kuskokwim Delta

Eek River, Kuskokwim Delta

Eek River drains a watershed of 408,959 acres (165,500 ha) and flows generally west-northwest for 108 miles (174 km) to the Kuskokwim Delta, about 40 miles (64 km) south-southwest of Bethel and 32 miles (51 km) north of Quinhagak, Alaska.

Brentwood Bay, Saanich Inlet

Brentwood Bay, Saanich Inlet

Brentwood Bay is a community within the municipality of Central Saanich on the eastern shore of Saanich Inlet, about 11 miles (18 km) north-northwest of the city of Victoria and 6 miles (10 km) south-southwest of Sidney, British Columbia.

Dundas Bay, Glacier Bay National Park and Preserve

Dundas Bay, Glacier Bay National Park and Preserve

Dundas Bay is located on the north shore of Icy Strait in Glacier Bay National Park and Preserve, about 24 miles (39 km) west of Gustavus and 11 miles (18 km) north of Elfin Cove, Alaska.

Fort Columbia, Chinook Point

Fort Columbia, Chinook Point

Fort Columbia, a historic military facility situated on Chinook Point, defended the entrance to the Columbia River from 1896 to 1947 and is now a state park, about 7 miles (11 km) southeast of Ilwaco and 6 miles (10 km) northwest of Astoria, Oregon.

Crab River, Devastation Channel

Crab River, Devastation Channel

Crab River flows into Devastation Channel near the entrance to Alan Reach of Gardner Canal, about 81 miles (130km) southeast of Prince Rupert and 28 miles (45km) south-southwest of Kitamaat, British Columbia.

SS Uzbekistan, Darling River

SS Uzbekistan, Darling River

The wreck of the SS Uzbekistan is situated at the mouth of the Darling River, which flows south for 6 miles (10 km) through the heavily logged interior forests of southwestern Vancouver Island, about 31 miles (50 km) northwest of Port Renfrew and 9 miles (15 km) south-southeast of Bamfield, British Columbia.

Blyn, Sequim Bay

Blyn, Sequim Bay

Blyn is a small community located where Jimmycomelately Creek flows into Sequim Bay on the northern coast of the Olympic Peninsula, about 13 miles (21 km) southwest of Port Townsend and 7 miles (11 km) southeast of Sequim, Washington.

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. 

Click here for more information about the #warmingstripes.

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