The temperature of the outer core is higher than its melting point. The outer core is mainly composed of liquid iron and nickel, which has a melting point higher than the temperature of the outer core due to the immense pressure at that depth.
The temperature of the Earth's mantle is higher than the temperatures of the outer layers, such as the crust, but lower than the core.
Well, if you look at it in a purely elemental capacity we see trends that with an increase in electron shielding, we get a decrease in melting point. This is said to be because with larger electron shielding we have a lower Z(eff) (effective nuclear charge) between atoms meaning weaker forces keeping them together and thus a lower melting point. I think this is an important logical procedure when understanding why things melt and what things like Z(eff) really mean in terms of an atom's behaviour. It's a good learning tool but, outside of periodicity, I would never feel comfortable attributing a melting point to electron shielding. Good idea for elements, terrible idea for molecules.
at the lower part of the fire
In a bunsen burner, the inner blue flame is hotter than the outer yellow flame because the blue flame is the primary combustion zone where complete combustion of the gas occurs. This results in a higher temperature due to the efficient burning of the gas. The outer yellow flame is cooler as it is the secondary combustion zone where some incomplete combustion occurs, leading to lower energy release and temperature.
The inner core is solid because of the immense pressure at that depth, which keeps the iron and nickel in a solid state despite the high temperatures. In the outer core, where pressure is slightly lower, the higher temperatures cause the iron and nickel to be in a liquid state.
higher
The outer core is liquid. Its pressure is low enough and its temperature high enough for it to melt. The inner core is solid. Both its pressure and temperature are higher than the outer core, but the increased pressure overwhelms the increased temperature, keeping the inner core from melting.
higher
outer core; Earth Science Reference Tables page 10
The temperature of the Earth's mantle is higher than the temperatures of the outer layers, such as the crust, but lower than the core.
The extremely high pressure at the inner core drives the melting point of the iron and other materials up beyond the temperature of the inner core. Therefore they remain solid. The pressure in the outer core is lower sop the melting point is below the temperature in this region and so it is a liquid.
the melting point is about i think 100,576 degrees Fahrenheit hope i helped :)
The outer core is liquid because it is under high pressure which lowers the melting point of the metals present in it. The inner core is solid because the immense pressure at the Earth's center, combined with the high temperature, keeps the iron and nickel in a solid state.
The inner core is under more pressure than the outer core.
The temperature of the Earth's mantle is higher than the outer crust but lower than the Earth's core. The mantle is composed of solid rock that can deform and flow over long periods of time due to its high temperature.
The inner core is solid due to high pressure preventing the temperature from melting the iron-nickel alloy. The outer core is liquid because the lower pressure allows for the metal to remain in a molten state.
Covalent compounds are formed when atoms share electrons to achieve a full outer shell. They typically have lower melting and boiling points compared to ionic compounds, and are often gases, liquids, or soft solids at room temperature. Covalent compounds do not conduct electricity in their pure form.