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OG green icebergs
Icebergs are massive blocks of ice, irregular in shape; they float with only about 12
percent of their mass above the sea surface. They are formed by glaciers—large rivers
of ice that begin inland in the snows of Greenland, Antarctica, and Alaska—and move
slowly toward the sea. The forward movement, the melting at the base of the glacier
where it meets the ocean, and waves and tidal action cause blocks of ice to break off
and float out to sea.
Icebergs are ordinarily blue to white, although they sometimes appear dark or
opaque because they carry gravel and bits of rock. They may change color with
changing light conditions and cloud cover, glowing pink or gold in the morning or
evening light, but this color change is generally related to the low angle of the Sun
above the horizon. However, travelers to Antarctica have repeatedly reported seeing
green icebergs in the Weddell Sea and, more commonly, close to the Amery Ice Shelf
in East Antarctica.
One explanation for green icebergs attributes their color to an optical illusion
when blue ice is illuminated by a near-horizon red Sun, but green icebergs stand out
among white and blue icebergs under a great variety of light conditions. Another suggestion
is that the color might be related to ice with high levels of metallic compounds,
including copper and iron. Recent expeditions have taken ice samples from
green icebergs and ice cores—vertical, cylindrical ice samples reaching down to great
depths—from the glacial ice shelves along the Antarctic continent. Analyses of these
cores and samples provide a different solution to the problem.
The ice shelf cores, with a total length of 215 meters (705 feet), were long enough
to penetrate through glacial ice—which is formed from the compaction of snow and
contains air bubbles—and to continue into the clear, bubble-free ice formed from
seawater that freezes onto the bottom of the glacial ice. The properties of this clear
sea ice were very similar to the ice from the green iceberg. The scientists concluded
that green icebergs form when a two-layer block of shelf ice breaks away and capsizes
(turns upside down), exposing the bubble-free shelf ice that was formed from
seawater.
A green iceberg that stranded just west of the Amery Ice Shelf showed two distinct
layers: bubbly blue-white ice and bubble-free green ice separated by a onemeter-
long ice layer containing sediments. The green ice portion was textured by
seawater erosion. Where cracks were present, the color was light green because of
light scattering; where no cracks were present, the color was dark green. No air bubbles
were present in the green ice, suggesting that the ice was not formed from the
compression of snow but instead from the freezing of seawater. Large concentrations
of single-celled organisms with green pigments (coloring substances) occur along the
edges of the ice shelves in this region, and the seawater is rich in their decomposing
organic material. The green iceberg did not contain large amounts of particles from
these organisms, but the ice had accumulated dissolved organic matter from the seawater.
It appears that unlike salt, dissolved organic substances are not excluded from
the ice in the freezing process. Analysis shows that the dissolved organic material
absorbs enough blue wavelengths from solar light to make the ice appear green.
Chemical evidence shows that platelets (minute flat portions) of ice form in the water and then accrete and stick to the bottom of the ice shelf to form a slush (partially
melted snow). The slush is compacted by an unknown mechanism, and solid, bubblefree
ice is formed from water high in soluble organic substances. When an iceberg
separates from the ice shelf and capsizes, the green ice is exposed.
The Amery Ice Shelf appears to be uniquely suited to the production of green icebergs.
Once detached from the ice shelf, these bergs drift in the currents and wind
systems surrounding Antarctica and can be found scattered among Antarctica’s less
colorful icebergs.
14. Directions: An introductory sentence for a brief summary of the passage is provided below. Complete the summary by selecting the THREE answer choices that express the most important ideas in the passage. Some sentences do not belong in the summary because they express ideas that are not presented in the passage or are minor ideas in the passage. This question is worth 2 points. Several suggestions, ranging from light conditions to the presence of metallic compounds, have been offered to explain why some icebergs appear green.
Answer Choices
1. Ice cores were used to determine that green icebergs were formed
from the compaction of metallic compounds, including copper and
iron.
2. All ice shelves can produce green icebergs, but the Amery Ice Shelf is
especially well suited to do so.
3. Green icebergs form when a twolayer block of ice breaks away from a
glacier and capsizes, exposing the bottom sea ice to view.
4. Ice cores and samples revealed that both ice shelves and green icebergs contain a layer of bubbly glacial ice and a layer of bubble-free sea ice.
5. Green icebergs are white until they come into contact with seawater
containing platelets and soluble organic green pigments.
6. In a green iceberg, the sea ice contains large concentrations of organic matter from the seawater. |
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