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Tracy Arm is a fjord in the U.S. state of Alaska near Juneau (outlet at 57° 46' 40" N 133° 37' 0" W). It is named after the Secretary of the Navy Benjamin Franklin Tracy.It is located about 45 miles (72 km) south of Juneau and 70 miles (110 km) north of Petersburg, Alaska, off of Holkham Bay and adjacent to Stephens Passage within the Tongass National Forest.
Photojournalist Larry Pannell estimates around "two thirds" of the Sawyer Glacier has disappeared since he first visited in 2012. Climate change: Shocking photos show Alaska glacier melting Skip ...
Tracy Arm extends to the north from the bay to Sawyer Glacier. Endicott Arm leads southeast from the bay to Dawes Glacier. [1] Both arms are fjords, which formerly held glaciers along their entire lengths. The bay is separated from the adjacent arms by an area of shallower water.
A century later glacier retreat has opened a multi-armed bay more than 30 miles long. The tidewater glacier has divided into three independent glaciers, Yahtse, Tsaa and Guyot Glacier. Other examples of glaciers currently in the retreat phase are South Sawyer and Sawyer Glaciers in Alaska, retreating 2.1 and 2.3 km respectively from 1961 to 2005.
On these cruises (usually toward the end), I look forward to encountering Hubbard Glacier, the largest tidewater glacier in North America. Its scale is truly staggering, stretching 6 miles wide ...
Blanca Glaciers - two extinct glaciers (N.& S. glacier) on Mt. Blanca. These glaciers were located at 37° 35N., longitude 105° 28W. at 12,000 feet in the Sangre de Cristo Mountain Range. These glaciers were located at 37° 35N., longitude 105° 28W. at 12,000 feet in the Sangre de Cristo Mountain Range.
Also on the Canadian side and entering the lower Stikine, like the Great Glacier, are the Mud and Flood Glaciers, which form the boundaries of the small Boundary Range, which is an eastern abutment of the range comprising the Stikine Icecap and marks the approximate boundary claimed by the United States prior to the Alaska Boundary Settlement ...
The retreat of glaciers since 1850 is a well-documented effect of climate change. The retreat of mountain glaciers provide evidence for the rise in global temperatures since the late 19th century. Examples include mountain glaciers in western North America, Asia, the Alps in central Europe, and tropical and subtropical regions of South America ...