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At 0 degrees Celsius fresh water has a density of 999.8 kilograms per cubic meter or 0.9998 grams per cubic centimeter. At 0 degrees Celsius frozen ice has a density of 916.8 kilograms per cubic meter or 0.9168 grams per cubic centimeter. So, ice will swim on the water like icebergs do. IF it were denser, it would sink. But it's not, so it floats.

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βˆ™ 16y ago
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βˆ™ 5mo ago

Ice floats on water because it is less dense than liquid water. When water freezes, its molecules form a crystalline structure that gives ice a lower density, causing it to float on the surface of the more dense liquid water.

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βˆ™ 14y ago

the answer that the question is looking for is "ice would sink in water" however one should take in to considuration the molecular stracher that ice takes vs water.

ice molecols are wider and create rings which requires them to take more space for the same matter.

There would also be less oxygen for humans to breath.

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βˆ™ 14y ago

At 0 degrees Celsius liquid water is more dense than solid water (ice). That's why ice floats. Pure water has a relative density of 0.9998 and ice is only 0.9167

An iceberg has a relative density of 0.9167 and seawater has a relative density of 1.025, so an iceberg has about 10% of its mass above water and nearly 90% of its mass hidden beneath the water's surface.

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βˆ™ 14y ago

Life would probably cease. The ice would sink to the bottom of the oceans and lakes and gradually all water would be frozen

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βˆ™ 13y ago

it floats..... due to hydrogen bonds in water, expansion upon freezing.... and a whole host of physics jargon( and that small bit of physics called chemistry too)

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βˆ™ 13y ago

Ice floats because it is less dense than water.

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Q: Does ice float or sink in the water?
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Do ice cubes in water float or sink?

They float, as ice is less dense than water.


Does ice float or sink in water why?

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To get an ice cube to sink in water, you need to increase its density. You can achieve this by adding salt to the water. The salt water is denser than the ice, causing the ice cube to sink.


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