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Couloir Cliffs were
named by the Granite Harbor Geological Party, led by the geologist Griffith
Taylor, of Robert Scott's British Antarctic Expedition (1910-13), because these
cliffs have numerous chimneys and couloirs (a mountainside gorge). In summer
1911-1912, Taylor led a four-man field party on a survey of Victoria Land and
finished their Granite Harbor work in the second week of January 1912.

Steep
rock walls underwater at Couloir Cliffs are coated with ice giving the
appearance of an underwater ice waterfall. The bottom is fifteen feet deep next
to the icefall in this picture and covered with rocks and boulders and anchor
ice.

The
exposed rock topside soaks up warmth from the sun, melting the covering snow.
This underwater ice cliff may be formed from this meltwater migrating through
permeable rock and freezing when it encounters cold seawater, or it may be
formed from a very cold underwater rock mass freezing seawater.

A
huge ice mound hung down from the sea ice ceiling and touched bottom. The
underside of the sea ice ceiling is not always flat; it can be mounded and there can be
scattered stalactites.

The
sea urchin Sterechinus neumayeri is a ubiquitous scavenger in shallow
water here at the Couloir Cliffs icefalls. The urchins are in right foreground
of this photo. Animals trapped in the frozen icefall are a food source.
Nearby there was a long nemertean worm frozen in place on the icefall
suggesting that it had been crawling along when meltwater streamed down over it
and froze it in place. It was a frozen meal awaiting the arrival of the
urchins.

The Sterechinus neumayeri urchins look for food on
the bottom and up on the icefall itself. The brown color of the icefall is due
to diatoms which the urchins scrape off and eat.
| Text ©Peter Brueggeman. Photographs
©Norbert Wu. Photographs may not be used in any form without the
express written permission of Norbert Wu.
Norbert Wu no longer grants permission for uncompensated use of his photos under any circumstances whatsoever;
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