Lets model your situation with every other variable kept constant. Basically, in this world, ice sinks water. We need to model for 2 bodies of water. Shallow bodies, like lakes and deep bodies like oceans. I'm going to ignore active volcanic activity. I'm also going to assume cases where the ambient temperature is sufficiently low enough to form ice. In our world, ice acts as incredibly good insulating layer(not much movement on the molecular level that allows the conduction of heat) due to its hydrogen and covalant bonding. Basically, it forms a packed, but evenly spaced, structure in which little moves. Its low density also inhibits the conduction of heat as nearby molecules are held at "arms length". In the case of a shallow body of water in the case of this world where ice sinks, we can also assume that geothermal and pressure heating due to depth is negligible. Hence, lacking this highly insulating layer, the warm water which rises would cool rapidly till freezing point, at which it would sink. And since cold water stays at the bottom, the ice would be melting very slowly. Therefore, ice builds from the bottom up and at a much faster rate than it would in our world. In a deeper body of water, its slightly harder to model due to geothermal heating. Very deep bodies of water might be able to retain some liquid water. In the case above, the ice sinks and it remains cold wherever it sinks to. However, when pressure and geothermal heating build up, the ice might be able to melt as it decends. In those places, there would be ice falling in the water, but there would not be any liquid ice floating on the surface. You basically get underwater snow. Fine snow if its not that cold/turbulent and a blizzard if it is. Lastly, im going to model your cup of soft drinks in which they love overfilling with ice, depriving you of the precious drink you pay for(at least over here). So here, your ice will stay at the bottom, which is already cold. Then since the top is warm and does not circulate down, it stays warm at the top but cold at the bottom. Hence, if u drink from the bottom, it will be colder than usual. But the average temperature will be higher. Also, assuming the same drinking rate, you will have more ice remaining and more of an incentive to ask for refunds, which you will not get anyway.
The outer core is liquid; the inner core is solid.
Th einner core is solid the outer core is liquid.
No. It behaves as a solid.
Based on the physical properties of the earth;The core is divided into outer core and inner core.the liquid layer of the earth core is the outer core,while the inner core is solid.
it's lava but in it's liquid form. A common misconception between magma and lava is lava is solid and magma is liquid hot.
Whether the solid will float or sink in a solid-liquid mixture depends on the relative densities of the solid and the liquid. If the density of the solid is greater than that of the liquid, then the solid will sink. If the density of the solid is less than that of the liquid, then the solid will float.
That depends on the relative densities of the solid and the liquid. If the solid is denser than the liquid, the solid will sink. If the liquid is denser, the solid will float.
No, solid O2 will not float on liquid O2 at all. There are several different phases of solid oxygen, depending on the conditions under which it is formed. But all of them are more dense than the liquid form, even near its freezing point (where it is most dense). None will come close to floating. Liquid oxygen has a density of about 1.141 grams/ml or so, and the solid forms have densities in the area of 1.4 grams/ml or so. Very few substances have a solid phase that floats on its liquid phase. Water is almost miraculous in this physical phenomenon. If ice did not float on water, earth's oceans would freeze solid within a few thousand years (or less).
float, depending on its density relative to the density of the liquid. If the solid is denser than the liquid, it will sink. If the solid is less dense than the liquid, it will float.
The phase changes of matter are melting (solid to liquid), freezing (liquid to solid), vaporization (liquid to gas), condensation (gas to liquid), sublimation (solid to gas), and deposition (gas to solid). These transitions occur due to changes in temperature and pressure.
Phase changes requiring the addition of heat energy are the phase changes from solid to liquid, liquid to gas, and solid to gas. These phase changes are termed melting (solid to liquid), evaporation (liquid to gas), and sublimation (solid to gas).
Liquid to solid is a phase change.
When you cool a liquid and it changes phase, it becomes a solid.
The liquid to gas phase change is vaporizing; the reverse is condensing. The other phase changes are: - solid to liquid: melting - liquid to solid: freezing - solid to gas: sublimation - gas to solid: deposition
Predominantly solid, but there is some liquid phase, and in certain situations, even a gaseous one.
The crust is not a solid shell; it is broken into huge, thick plates that float on the liquid mantle.
The melting phase changes are Solid~Liquid~Gas and the freezing phase changes are Gas~Liquid~Solid