Glaciers
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Vassar Glacier, College Fjord
Vassar Glacier flows southeast for 4.3 miles (7 km) from the eastern flank of Peak 8080 in the Chugach Mountains to the western shore of College Fjord near the confluence of Harvard Arm and Yale Arm and 2 miles (3.2 km) west of College Point, about 52 miles (83 km) west of Valdez and 42 miles (68 km) northeast of Whittier, Alaska.
Valerie Glacier, Disenchantment Bay
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.
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.
Meares Glacier, Unakwik Inlet
Meares Glacier starts at an elevation of about 7200 feet (2195 m) in the Chugach Mountains between Mount Michelson to the north and Columbia Peak to the south and trends generally southwest for 16 miles (26 km) to Unakwik Inlet in Prince William Sound, about 47 miles (76 km) northeast of Whittier and 40 miles (64 km) west of Valdez, Alaska.
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.
Brady Glacier, Taylor Bay
Brady Glacier lies in Glacier Bay National Park and Preserve, flowing from the Brady Icefield at 11,942 feet (3,640 m) in the Fairweather Range of the Saint Elias Mountains to Taylor Bay on Cross Sound’s north shore, about 139 miles (224 km) southeast of Yakutat and 32 miles (52 km) west of Gustavus, Alaska.
Aialik Glacier, Kenai Fjords National Park
Aialik Glacier flows southeast for 8 miles (13 km) from the Harding Icefield in the Kenai Mountains to tidewater at Aialik Bay in Kenai Fjords National Park, about 66 miles (106 km) east-northeast of Homer and 16 miles (26 km) southwest of Seward, Alaska.
Grapeview, Case Inlet
Grapeview is a community that includes Allyn, Stretch Island, and Reach Island located on the western shore at the head of Case Inlet in South Puget Sound, about 19 miles (31 km) west-northwest of Tacoma and 16 miles (26 km) northeast of Shelton, Washington.
Dirty Glacier, Harriman Fjord
The Dirty Glacier flows generally north for about 1.7 miles (2.7 km) from an elevation of 3,800 feet (1,158 m) in the Chugach Mountains of western Prince William Sound to its terminus at an outwash plain about 1 mile (1.6 km) from the head of Harriman Fjord, about 71 miles (114 km) west-southwest of Valdez and 16 miles (26 km) northeast of Whittier, Alaska.
Ancon Rock, Point Gustavus
Ancon Rock is a reef located about 0.5 miles (0.8 km) off Point Gustavus on the eastern shore, at the entrance to Glacier Bay within Glacier Bay National Park and Preserve, about 55 miles (89 km) west of Juneau and 8.5 miles (12 km) southwest of Gustavus, Alaska.
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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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