As you move closer to the Earth's inner core, the temperature increases. This is because the inner core is surrounded by layers of molten metal and rock, which generate heat through radioactive decay and residual heat from Earth's formation. The temperature at the Earth's inner core can reach up to around 5700°C (10,300°F).
Temperature and pressure increase massively from the Earth's surface to the centre of the Earth. At the inner core, the pressure is so great that iron is solid, even at such high temperatures.
No, the temperature of the Earth's core remains relatively constant over time. The heat in the core is generated from radioactive decay and residual heat from the planet's formation, which creates a stable thermal environment.
Pressure increases with depth in the Earth, compressing materials and raising temperatures. Radioactive decay in the Earth's core generates heat, contributing to the high temperatures there. These processes collectively determine the temperature gradient from the crust to the core of the Earth.
The temperature increases as you move from the Earth's crust towards the core. The temperature in the crust varies depending on factors such as depth and geothermal gradient, while the core's temperature reaches over 5000 degrees Celsius due to the immense pressure and radioactive decay.
As you move closer to the Earth's inner core, the temperature increases. This is because the inner core is surrounded by layers of molten metal and rock, which generate heat through radioactive decay and residual heat from Earth's formation. The temperature at the Earth's inner core can reach up to around 5700°C (10,300°F).
No, the temperature of Earth actually increases as you move closer to the core. This is due to the heat generated by the decay of radioactive elements in the Earth's interior, as well as the residual heat from the planet's formation.
It increases. The closer you get to the Earth's core - the higher the pressure (and temperature).
Radioactive decay!
Radioactive decay!
In general, the temperature decreases towards the surface.
the grvitational pull of the earth becomes stronger as you cet closer to the core.
Pressure and radioactivity.
Temperature and pressure increase massively from the Earth's surface to the centre of the Earth. At the inner core, the pressure is so great that iron is solid, even at such high temperatures.
As you move closer to the core of the Earth, both pressure and temperature increase. The increase in pressure is due to the weight of the overlying rocks and materials compressing the layers below. The increase in temperature is mainly a result of the Earth's internal heat and radioactive decay of elements.
The temperature increases as you get closer to the center of the Earth. This is due to the heat generated by the radioactive decay of elements in the Earth's core and the compression of materials under the immense pressure at the center, reaching temperatures of over 5,700 degrees Celsius at the inner core.
No, the temperature of the Earth's core remains relatively constant over time. The heat in the core is generated from radioactive decay and residual heat from the planet's formation, which creates a stable thermal environment.