The best cell phones to my best ability of 2010 are the Sprint HTC EVO 4g, Verizon HTC Droid Incredible, Nexus One, Nokia N8, T-Mobile Mytouch 3g slide, T-Mobile HTC HD2, Verizon palm pre plus, AT&T palm pre plus, Apple iPhone 3GS, and the Motorola Droid from Verizon.
it is about 2.17 g/cc
The Density of Seawater=1.03g/ml
Density current
Answer 1) At the Surface. Answer 2) I disagree with the above answer. For practical purposes water is not compressible. Therefore the density is the same all over. The difference in density at the surface and at the bottom is so small that it is negligible. However, fresh water is less dense than seawater, since the salts dissolved in the seawater makes it more dense. For that reason, if you consider seawater near the mouth of a river, that water will be less dense than the seawater in general.
Salinity in the ocean is highest in regions where evaporation is high and precipitation is low. Density in seawater is determined by both temperature and salinity.
The halogen found in seawater is bromine.
Seawater has very high levels of sodium , salt, from materials in the sand, freshwater, lakes and ponds, have very low, if any salt levels , so, never consume seawater without first filtering it, it will kill you.
The density of seawater increases if salinity increases.
Density currents - more dense seawater sinking beneath less dense seawater.
Relative salinity is the most important factor in seawater density.
the salt makes seawater denser than freshwater. more salt increases the density
the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater
the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater
the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater
Density current
density current
No, an iceberg is approximately 10% less dense than seawater. This is why it floats
Seawater does not have a density of 5.
A density current forms when more dense seawater moves toward less dense seawater.