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Nordyke Island, Kamishak Bay
Nordyke Island is about 35 feet (11 m) high, flat topped and grass covered, and located in Kamishak Bay, about 115 miles (186 km) northwest of Kodiak and 96 miles (155 km) southwest of Homer, Alaska.
Sumdum, Endicott Arm
Sumdum is a historical Tlingit village of the S’awdaan Kwáan located north of Powers Creek at the northern end of Endicott Arm where it meets Holkham Bay in Tracy Arm-Fords Terror Wilderness, about 70 miles (113 km) north-northwest of Petersburg and 49 miles (79 km) southeast of Juneau, Alaska.
Tigertail Glacier, Nassau Fjord
Tigertail Glacier starts at an elevation of about 2,850 feet (869 m) in the Sargent Icefield on the Kenai Peninsula and flows generally northeast for 3.3 miles (5.3 km) and terminates 0.2 miles (0.3 km) from the western shore of Nassau Fjord, which is a northern arm of Icy Bay in western Prince William Sound, about 36 miles (58 km) east-northeast of Seward and 36 miles (58 km) south-southeast of Whittier, Alaska.
Main Bay, Prince William Sound
Main Bay is an estuary on the Kenai Peninsula fed by a watershed of 3,795 acres (1,536 ha) mostly draining from an unnamed lake at an elevation of 205 feet (62 m) on the northern flank of Eshamy Peak in Prince William Sound, between Port Nellie Juan to the west and Knight Island Passage to the east, about 81 miles (131 km) west of Cordova and 28 miles (45 km) southeast of Whittier, Alaska.
Point Pogibshi, Kachemak Bay
Point Pogibshi is a prominent flat-topped grassy headland with rocky sides about 50 feet (15 m) high on the southern shore of Kachemak Bay, about 20 miles (23 km) southwest of Homer, and 5 miles (8 km) north-northeast of Nanwalek, Alaska.
Point Retreat, Admiralty Island
Point Retreat is a headland with a historic lighthouse on the Mansfield Peninsula at the northern tip of Admiralty Island, between Lynn Canal to the west and Saginaw Channel of Stephens Passage to the east, about 60 miles (97 km) south-southeast of Haines and 20 miles (32 km) northwest of Juneau, Alaska.
Drew Point, Smith Bay
Drew Point is located at the eastern entrance to Smith Bay on the Beaufort Sea and is formed by rapidly eroding permafrost and ice wedges at the edge of the Arctic Coastal Plain, about 81 miles (131 km) northwest of Nuiqsut and 70 miles (113 km) southeast of Utqiaġvik, Alaska.
Hubbard Glacier, Disenchantment Bay
Hubbard Glacier originates from icefields at an elevation of around 11,000 feet (3,400 m) in the Centennial Range of the Saint Elias Mountains in Kluane National Park and Reserve and flows about 48 miles (77 km) to the Alaska border and then continues for another 28 miles (45 km) through Wrangell-Saint Elias National Park to its terminus in Disenchantment Bay, about 220 miles (355 km) east-southeast of Cordova and 32 miles (52 km) north-northeast of Yakutat, Alaska.
China Poot Creek, Kachemak Bay
China Poot Creek starts at an elevation of about 3,500 feet (1,067 m) on the western flank of the Kenai Mountains and flows for 5.6 miles (9 km) to China Poot Lake, also called Leisure Lake, at an elevation of 168 feet (51 m), and then for another 0.9 miles (1.5 km) to China Poot Bay on the southeastern shore of Kachemak Bay, about 19 miles (31 km) northeast of Seldovia and 13 miles (21 km) southeast of Homer, Alaska.
Beatson Copper Mine, Latouche Island
Beatson Copper Mine and the abandoned mining community of Latouche are situated at the base of Mount Beatson and adjacent to Powder Point near the northwest tip of Latouche Island in Prince William Sound, about 82 miles (132 km) southwest of Cordova and 57 miles (92 km) southeast of Whittier, 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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