Beaches
Recent Articles
More Articles
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.
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.
Umpqua River, Winchester Bay
Umpqua River flows generally west-northwest for 111 miles (179 km), draining a watershed of 2.4 million acres (1 million ha), from the Cascade Mountains through the Coast Range to Winchester Bay in the Oregon Dunes, about 20 miles (32 km) north of Coos Bay and 5.5 miles (9 km) southwest of Reedsport, Oregon.
Ma-le’l Dunes, Humboldt Bay
Ma-le’l Dunes, a National Natural Landmark, lie between the Mad River Slough and the Pacific Ocean at the base of the Samoa Peninsula, which partially encloses the northern part of Humboldt Bay, about 1 mile (1.6 km) north of Manila and 3.5 miles (5.6 km) west of Arcata, California.
Northeast Cape, Saint Lawrence Island
Northeast Cape is a headland at the far eastern end of Saint Lawrence Island, formed by the Kinipaghulghat Mountains, between Cape Kulowye to the west and Cape Seevooka to the south, about 133 miles (214 km) southwest of Nome and 96 miles (155 km) east-southeast of Gambell, Alaska.
Pysht River, Pillar Point
Pysht River originates near Ellis Mountain on the Olympic Peninsula and flows generally northeast for 16 miles (26 km), draining a watershed of 29,632 acres (11,992 ha), to the Strait of Juan de Fuca at Pillar Point, about 31 miles (50 km) west-northwest of Port Angeles and 26 miles (42 km) southeast of Neah Bay, Washington.
Sixes River, Cape Blanco
Sixes River drains a watershed of about 85,832 acres (34,735 ha) and flows generally west for about 31 miles (50 km) through coastal forests in southwestern Oregon and enters the Pacific Ocean just north of Cape Blanco, about 19 miles (31 km) south-southwest of Bandon and 8 miles (13 km) north-northwest of Port Orford, Oregon.
Oso Flaco Creek, Guadalupe-Nipomo Dunes
Oso Flaco Creek drains a watershed of approximately 7,400 acres (2,995 ha) consisting mostly of agricultural land before forming Oso Flaco Lake, now part of the Oso Flaco Lake Natural Area in the Guadalupe-Nipomo Dunes, and then flows into the Pacific Ocean, about 68 miles (109 km) northwest of Santa Barbara and 5 miles (8 km) south of Oceano, California.
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.