Ethnological results of the Point Barrow expedition: Ninth Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1887-1888, Government Printing Office, Washington, 1892, pages 3-442 — John Shaqi
Ethnological results of the Point Barrow expedition: Ninth Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1887-1888, Government Printing Office, Washington, 1892, pages 3-442Murdoch, John
History
Ethnological results of the Point Barrow expedition: Ninth Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1887-1888, Government Printing Office, Washington, 1892, pages 3-442
Murdoch, John
Eskimos -- Alaska -- Barrow, Point, Region
Sometimes, however, the heavy pack, under the pressure of violent and
long-continued westerly winds, pushes across the bar and is forced up
on the beach. The ice sometimes comes in with great rapidity. The
natives informed us that a year or two before the station was
established the heavy ice came in against the village cliffs, tearing
away part of the bank and destroying a house on the edge of the cliff
so suddenly that one of the inmates, a large, stout man, was unable to
escape through the trap-door and was crushed to death. Outside of the
land-floe the ice is a broken pack, consisting of hummocks of
fragmentary old and new ice, interspersed with comparatively level
fields of the former. During the early part of the winter this pack is
most of the time in motion, sometimes moving northeastward with the
prevailing current and grinding along the edge of the barrier,
sometimes moving off to sea before an offshore wind, leaving “leads”
of open water, which in calm weather are immediately covered with new
ice (at the rate of 6 inches in 24 hours), and again coming in with
greater or less violence against the edges of this new ice, crushing
and crumpling it up against the barrier. Portions of the land-floe
even float off and move away with the pack at this season.
The westerly gales of the later winter, however, bring in great
quantities of ice, which, pressing against the land-floe, are pushed
up into hummocks and ground firmly in deeper water, thus increasing
the breadth of the fixed land-floe until the line of separation
between the land-floe and the moving pack is 4 or 5 or sometimes even
8 miles from land. The hummocks of the land-floe show a tendency to
arrange themselves in lines parallel to the shore, and if the pressure
has not been too great there are often fields of ice of the season not
over 4 feet thick between the ranges of hummocks, as was the case in
the winter of 1881-’82. In the following year, however, the pressure
was so great that there were no such fields, and even the level ice
inside of the barrier was crushed into hummocks in many places.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account