about 90%.
water molecules can evaporate at the surface but not below the surface
The answer is false. Ground water is water retained below earth's surface. BELOW THE SURFACE.
Ground water, or an aquifer.
71% of Earth's surface
ground water
1/8 is.
An Iceberg Made of water but ice is lighter than water. Nine tenths of an iceberg is below the surface and so it is unseen.
Nine tenths (9/10) of an iceberg is underwater.
Typically, about 90% of an iceberg is underwater, while only about 10% is visible above the surface. This is because ice is less dense than seawater, causing most of the iceberg to remain submerged.
They are chunks of floating ice drifting away from polar regions. The density of ice is just a little less than the density of sea water, so most of the volume of an iceberg is below the surface, and so a small-looking iceberg can have a huge volume of ice below the surface. The Titanic ran into an iceberg and was holed below its waterline so the water rushed in and the ship sank.
79% of an iceberg is underwater, so 21% or about one fifth is above it. However given the shape and size of an iceberg, as little as 10% can be above water at times, so it can be between one tenth and one ninth above water.
1/8 of the iceberg is at the surface while the rest remains. This is an average iceberg (based on titanic)
Because up to 90% of an iceberg's mass is found under the water's surface
Approximately 90% of an iceberg is below water because ice is less dense than water, so a large portion of the iceberg needs to be submerged to displace enough water and stay afloat. The submerged portion is what gives icebergs their stability and makes them less likely to tip over.
water molecules can evaporate at the surface but not below the surface
About 2/9ths of the berg would be above the water. Can you detail out?
Approximately 9/10 of an iceberg is below the water. The figure is approximate because the density of the berg depends on how must the ice is compacted and how much air it contains. It also depends on the density of the seawater which, in turn, depends on its salinity and temperature.