Fish Creek drains an area of about 1.1 million acres (460,000 ha), entirely with the zone of continuous permafrost, and flows generally northeast for about 110 miles (177 km) through the Arctic Coastal Plain in the National Petroleum Reserve to Harrison Bay at the western edge of the Colville River delta, about 141 miles (230 km) southeast of Utqiaġvik and 12 miles (19 km) north-northwest of Nuiqsut, Alaska.
Swanberg Dredge is a placer mining machine that extracts gold from sand and gravel and is located in a small artificial pond at Rocker Gulch, about 200 feet (61 m) north of the Nome-Council Highway on the Seward Peninsula, about 18 miles (29 km) west of Safety and 1 mile (1.6 km) east of Nome, Alaska.
Alamere Falls is located about 0.4 miles (0.6 km) north of Double Point where Alamere Creek cascades 40 feet (12 m) over a sea cliff, directly into the ocean at high tides and otherwise onto Wildcat Beach 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.
Fossil Point is a prominent landmark in Lake Clark National Park and Preserve on the southern shore of Tuxedni Bay, at the north end of Tuxedni Channel and west of Chisik Island, about 56 miles (90 km) southwest of Kenai and 54 miles (87 km) northwest of Homer, Alaska.
Point No Point is a sand spit on the northern end of the Kitsap Peninsula, between Norwegian Point to the northwest and Pilot Point to the southeast, near the southern end of Admiralty Inlet that connects the Salish Sea with Puget Sound, about 8 miles (13 km) north of Kingston and 1.3 miles (2.1 km) southeast of Hansville, Washington.
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.
Valerie Glacier is formed by several tributary glaciers that flow from the south flank of Mount Vancouver in the Saint Elias Mountains of the Icefield Ranges, and the merged ice streams flow generally southeast for about 14 miles (22.5 km) to laterally join with the Hubbard Glacier and terminate in Disenchantment Bay, about 154 miles (248 km) northwest of Haines and about 33 miles (53 km) north-northeast of Yakutat, Alaska.
Valdez Glacier starts on the south flank of Mount Cashman and flows southeast for about 20 miles (35 km) to its terminus at Valdez Glacier Lake, 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.
Point San Pedro forms the northwestern extent of Pedro Point Headland on San Pedro Mountain which reaches an elevation of about 624 feet (190 m) and has steep cliffs on both the northern and southern flanks, and forms the southern slope of the San Pedro Creek watershed, about 3.6 miles (5.8 km) north of Montara and the southern municipal boundary of Pacifica, California.
Eek River drains a watershed of 408,959 acres (165,500 ha) and flows generally west-northwest for 108 miles (174 km) from a small lake at an elevation of about 2,700 feet (823 m) on the north flank of Mount Oratia to the Kuskokwim River Delta, about 40 miles (64 km) south-southwest of Bethel and 32 miles (51 km) north of Quinhagak, 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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