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FAQs about the Natural History of the Inside Passage
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Click arrow
to start movie of the Johns Hopkins Glacier calving.
Source: NASA |
The glaciers seen in Glacier
Bay today are remnants of the Little Ice Age that began
about 4,000 years ago and reached its maximum extent in
Glacier Bay around 1750, when general melting began. In
1794, Captain George Vancouver and his crew described
what we now call Glacier Bay as just a small five-mile
indent in a gigantic glacier that stretched to the horizon.
That massive glacier was 4,000 feet thick, 20 miles wide,
and extended more than 100 miles to the St. Elias mountain
range. In 1879, when naturalist John Muir visited Glacier
Bay, the ice had retreated more than 30 miles forming
an actual bay. By 1916, the Grand Pacific Glacier, the
primary glacier responsible for carving the bay, had melted
back 60 miles to the head of Tarr Inlet.
Glacier Bay contains both
tidewater and non-tidewater glaciers. According to the
National Park Service, Glacier Bay National Park boundaries
today include 11 tidewater glaciers, glaciers that flow
out of the mountains and terminate in tidal waters. Eight
of these tidewater glaciers flow into Glacier Bay. Many
of the tidewater glaciers that Muir first observed in
1879 have been reduced to small glaciers that terminate
on land.
In general, tidewater glaciers
in Glacier Bay have been in a state of retreat since the
1750. However, between 1920 and 1930, the Jophns Hopkins
and Grand Pacific Glaciers began to advance. In 2004,
the Johns Hopkins Glacier was advancing at the rate of
8 feet per day but the Grand Pacific was receding at approximately
4 feet per day. The most active tidewater glacier is McBride
that is retreating at the rate of 3,000 feet per year.
Since tidewater glaciers
follow their own cycles that are independent of climate
changes, individual tidewater glaciers may recede, advance,
or remain stable at any given time. There is one thing
you can be certain—a glacier's face you see today
will be changed by tomorrow and even more significantly
20 years from now.
Additonal Resources:
Glacier
Bay National Park and Preserve
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