outer core; Earth Science Reference Tables page 10
The inner core of the Earth has a temperature higher than its melting point. Despite being made of solid iron and nickel, the immense pressure at the center of the Earth keeps it in a solid state even at temperatures above its melting point.
The temperature is getting higher because of the gases and because of that the ice is melting and in several years we all can die because we will drown.
The temperature of Earth's crust is much lower than the temperature of Earth's interior. The temperature of Earth's crust generally ranges from about 0°C to 30°C, while the temperature of Earth's interior can reach thousands of degrees Celsius in the mantle and core. The higher temperatures in the interior are due to the heat generated by radioactive decay and leftover heat from Earth's formation.
The composition of the magma plays a significant role in determining its melting temperature. Magma with higher silica content tends to have a higher melting temperature. Pressure also affects the melting temperature; higher pressure usually results in a higher melting temperature. Water content can lower the melting temperature of magma by acting as a flux, allowing minerals to melt at lower temperatures.
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Higher GC content in DNA is associated with a higher melting temperature, as GC base pairs have three hydrogen bonds compared to two in AT base pairs, making them more stable. Therefore, DNA sequences with higher GC content require higher temperatures to denature during melting compared to sequences with lower GC content.
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GC-rich DNA has a higher melting temperature due to stronger hydrogen bonding between guanine and cytosine compared to adenine and thymine. This results in increased stability and a higher melting temperature for GC-rich DNA sequences.
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 melting temperature of materials is affected by their confining pressure. The higher the pressure the higher the melting temperature. As such as you move deeper into the mantle, the tempraeture will increase, but because of the overlying material so to will the confining pressure which drives up the melting temperature. When high temperature mantle material moves nearer to the surface such as near a mid-ocean-ridge the confining pressure falls faster than the materials temperature and this can cause the melting point to drop below the temperature of the material leading to melting.
Siliocone has a higher one. Chlorine is already a gas at room temperature.