Rivers
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Dismal Nitch, Columbia River
Dismal Nitch is a cove on the north shore of the lower Columbia River, historically significant as the last campsite of the Lewis and Clark Expedition before they sighted the Pacific Ocean, about 9 miles (15 km) southeast of Ilwaco, Washington and 4.5 miles (7 km) north-northwest of Astoria, Oregon.
Seldovia River, Kenai Mountains
Seldovia River drains a watershed of 16,980 acres (6,872 ha) and flows generally northwest for 5 miles (8 km) from Seldovia Lake in the Kenai Mountains to Seldovia Bay on the south shore of Kachemak Bay and Lower Cook Inlet, about 18 miles (29 km) south-southwest of Homer and 3.6 miles (6 km) south-southeast of Seldovia, Alaska.
Los Angeles River, Long Beach
Los Angeles River starts at the confluence of Bell Creek and Arroyo Calabasas that drain from the Simi Hills and Santa Monica Mountains respectively, and flows generally southeast for 30 miles (48 km) through the San Fernando Valley and downtown Los Angeles and then south for 20 miles (32 km) to San Pedro Bay at Long Beach, California.
Dala-Kildala Rivers Estuaries Provincial Park, Kildala Arm
Dala-Kildala Rivers Estuaries Provincial Park is located at the head of Kildala Arm, a fjord that extends generally southeast for 10 miles (16 km) from Douglas Channel, about 81 miles (130 km) southeast of Prince Rupert, and 13 miles (21 km) south-southeast of Kitamaat, British Columbia.
Ark Island, Aniakchak River
Ark Island is situated at the mouth of the Aniakchak River on the north shore of Aniakchak Bay and on the southeastern coast of the Alaska Peninsula, about 205 miles (330 km) southwest of Kodiak and 47 miles (75 km) northeast of Chignik, Alaska.
Hoquiam River, Grays Harbor
Hoquiam River drains a watershed of 62,720 acres (25,382 ha) with three principal tributaries that merge into a single channel that trends generally south for 2.5 miles (4 km) to the confluence with the Chehalis River at the head of Grays Harbor between the communities of Hoquiam to the west and Aberdeen to the east, about 47 miles (76 km) west of Olympia and 12 miles (19 km) northeast of Westport, Washington.
Kowesas River, Chief Mathews Bay
Kowesas River flows generally north for 22 miles (35 km), draining a watershed of 101,807 acres (41,200 ha) in the Coast Mountains before emptying into the head of Chief Mathews Bay, about 112 miles (180 km) southeast of Prince Rupert and 17 miles (27 km) south-southwest of Kemano, British Columbia.
McNeil Canyon, Kachemak Bay
McNeil Canyon is on the Kenai Peninsula and the northern shore of Kachemak Bay and trends south for about 2 miles (3.2 km) following the lower course of McNeil Creek, about 57 miles (92 km) south of Kenai and 12 miles (19 km) northeast of Homer, Alaska.
Tijuana River, Imperial Beach
Tijuana River drains a 1.1‑million‑acre (450,000 ha) watershed that originates in the Sierra de Juárez in northern Baja California and flows west‑northwest for 120 miles to the Pacific at the southern edge of Imperial Beach, about 11 miles south of San Diego and 5 miles northwest of Tijuana, Mexico.
Baird Glacier, Thomas Bay
Baird Glacier starts in the Stikine Icefield in the Boundary Ranges of the Coast Mountains near the Alaska-British Columbia border, and flows generally southwest for 24 miles (39 km) to its terminus at an outwash plain 2 miles (3.2 km) north of the head of Thomas Bay, about 100 miles (162 km) southeast of Juneau and 22 miles (35 km) north-northeast of Petersburg, 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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