Page 121 - (DK Eyewitness) Travel Guide 2017 - Alaska
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PRINCE  WILLIA M   SOUND      119

       3 College Fjord
       Transport map E4. g tour from
       Whittier. 8
       The College Fjord arm of
       Prince William Sound and the
       neighboring Harriman Fjord
       include an impressive concen-
       tration of easily accessible
       tidewater glaciers, as well
       as myriad valley glaciers and
       hanging glaciers (see pp30–31).  Black-legged kittiwakes perching on a small ice floe
         In 1899, New York railroad
       magnate Edward Harriman   Kittiwakes
       launched a scientific expedi tion   The towering cliffs across Passage Arm from Whittier are home to
       along the Alaskan coast,   a colony of thousands of black-legged kittiwakes (Rissa tridactyla).
       including College Fjord, where   During the summer nesting season they can be seen wheeling
       he named the glaciers after the   around the precarious cliff faces where they nest, breed, and hatch
       Ivy League colleges attended    their chicks. With a rela tively rapid wingbeat, kittiwakes are highly
       by the scientists on board his   maneuverable and able to land on narrow cliff ledges even in strong
       ship, the George W. Elder. As one   winds. In the winter, these pelagic gulls spend most of their time on
       travels into the fjord, the glaciers   the open ocean, feeding on small fish and plankton.
       on the left are named for
       women’s col leges and those
       on the right for men’s schools.   groups or rafts of sea otters and   being impeded by the friction
       Chunks as large as a house   icebergs laden with harbor seals,   of ice against rock. It calved so
       often calve from the massive   and blast their horns with the   much ice that it choked the
       300-ft- (90-m-) high glacier faces.  hope that the vibrations would   waters between its 3-mile
                           cause the glacier to calve.  (5-km) wide face and its
                             However, in the early 1980s,   terminal moraine with large
       4 Columbia Glacier   Columbia Glacier began to   icebergs that froze together.
                           surge at a pace as great as    As a result, the glacier face has
       Transport map E3. g tour boats   115 ft (35 m) per day, calving   receded about 13 miles (21 km)
       from Valdez. 8
                           icebergs into Prince William   since 1982 and can no longer
       During the 1980s, 40-mile-    Sound much faster than snow   be reached by ferry, although
       (64-km-) long, 2,000-ft- (600-m-)   compression on the ice field   there are hopes that this may
       thick Columbia Glacier was a   could replace it. It is thought   stabilize. Currently, this active
       highlight on the Alaska Marine   that the melting ice created a   glacier is most readily accessed
       Highway route between   cushion of water beneath the   on day cruises (check out www.
       Whittier and Valdez. Ferries   main ice sheet, allowing the   stephenscruises.com) and
       would typically stop amid the   glacier to progress without   private tour boats from Valdez.






















       Cruisers aboard a tour boat approaching Columbia Glacier, Prince William Sound




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