Page 32 - (DK Eyewitness) Travel Guide 2017 - Alaska
P. 32

30      INTRODUCING  ALASK A


        Alaska’s Glaciers

        Much of Alaska’s spectacular landscape has been
        shaped by 5,000 major and countless minor glaciers that
        scraped downhill from icefields in the coastal mountains,
        gouging out steep-sided valleys. As glaciers melted,
        valleys that were below sea level were filled by seawater
        to create long, narrow fjords. Although glaciers continue
        to reshape the land scape, most of these rivers of ice –
        the earth’s largest reservoir of freshwater – are currently
        receding, and scientific research suggests that human-
        caused warming of the planet may be the primary reason.
                                              Crevasses develop when stresses
                                              on the flowing ice cause large
                                              cracks in glaciers. The largest
                                              crevasses are found on steep
                                              sections of rapidly flowing ice.






        Outlet Glaciers, such as Mendenhall Glacier near Juneau, spill
        down steeply from icefields, creating ravines that serve as outlets
        for the icefield. They often flow into lakes created by the glacier’s
        terminal moraine, a ridge of debris at the foot of the glacier.

        Glacial Changes
                                 Lateral moraines are
        As glaciers flow downhill, friction against   strips of ground rock on
        the rock melts the bottom ice, forming    the edges of glaciers.
        a “slide” so the glacier can surge ahead.
        Increasing air temperatures can cause
        melting at glacier faces, but can also
        cause surging, as higher temperatures
        mean more snowfall, and therefore, pres­  Bergy bits are large
        sure, on parent icefields. Tidewater gla­  chunks of glacier ice
                                 or small ice bergs,
        ciers flowing into warming seas tend to   rising up to 13 ft
        recede due to higher water temperatures.  (4 m) out of the water.
          Alaska’s Prominent Glaciers
          Key                                              Canada
                                     Alaska            Alaska
          1 Aialik (see p107)
          2 Exit (see p103)
          3 Portage (see p85)
          4 Eklutna (see p83)
          5 Matanuska (see p184)                      Canada
          6 Columbia (see p119)
          7 Worthington (see p121)
          8 Childs (see p123)
          9 Bering (see p41)
          0 Kennicott (see p193)    Gulf of Alaska
          q Malaspina (see p155)
          w Hubbard (see p31)
          e Margerie (see p146)               0 km   200
          r Mendenhall (see p145)   Pacific Ocean
                                              0 miles     200





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