Volume
An iceberg is a large piece of freshwater ice that has broken off from a snow-formed glacier or ice shelf and is floating in open water. It may subsequently become frozen into pack ice or come to rest on the seabed in shallower water. The word iceberg is a partial loan translation from Dutch ijsberg, literally meaning ice mountain. Icebergs are often referred to simply as bergs.
Typically, only one-tenth of the volume of an iceberg is above water. The shape of the under water portion can be difficult to judge by looking at the portion above the surface. This has led to the expression “tip of the iceberg”, generally applied to a problem or difficulty, meaning that the visible trouble is only a small manifestation of a larger problem.
Icebergs generally range from 3–250 feet above sea level and weigh 100,000 to 200,000 tons. The tallest known iceberg in the North Atlantic was 550 ft above sea level, making it the height of a 55-story building.
Though usually confined by winds and currents to move close to the coast, the largest icebergs recorded are calved, or broken off from, the Ross Ice Shelf of Antarctica. Icebergs in the Antarctic area sometimes have stripes, formed by layers of snow that react to different conditions. Blue stripes are often created when a crevice in the ice sheet fills up with meltwater and freezes so quickly that no bubbles form. When an iceberg falls into the sea, a layer of salty seawater can freeze to the underside. If this is rich in algae, it can form a green stripe. Brown, black and yellow lines are caused by sediment, picked up when the ice sheet grinds downhill towards the sea.
When an iceberg melts, it makes a fizzing sound called “Bergie Seltzer.” This sound is made when compressed air bubbles trapped in the iceberg pop. The bubbles come from air trapped in snow layers that later become glacial ice. Ice campers who camp on top of flat or hollowed icebergs are known as icebergers.
There was no system in place before 1912 to track icebergs to guard against ship collisions. The sinking of the RMS Titanic, which caused the deaths of more than 1,500 of its 2,223 passengers, created the demand for a system to observe icebergs. For the remainder of the ice season of that year, the United States Navy patrolled the waters and monitored ice flow.
Aerial surveillance of the seas in the early 1930s allowed for the development of charter systems that could accurately detail the ocean currents and iceberg locations. In 1945, experiments tested the effectiveness of radar in detecting icebergs. A decade later, oceanographic monitoring outposts were established for the purpose of collecting data. These outposts continue to serve in environmental studies.

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