well that answer will be 6000 km - depths below surface of earth (km)
The temperature at a depth of 1000 km inside the Earth can reach around 1000 to 2000 degrees Celsius. This heat is primarily generated by the radioactive decay of elements in the Earth's mantle and core.
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
The Earth's crust has an average depth of about 30-50 km. It is primarily composed of oxygen, silicon, aluminum, and iron, with varying amounts of other elements. The temperature of the crust increases with depth, ranging from about 200°C at the surface to over 800°C at the base of the crust.
lithosphere
well that answer will be 6000 km - depths below surface of earth (km)
At a depth of 1000 km below the surface, the temperature of the Earth's interior is estimated to be around 1200-1400 degrees Celsius. This heat is generated by the Earth's core and is a result of radioactive decay and residual heat from the planet's formation.
The temperature at a depth of 1000 km inside the Earth can reach around 1000 to 2000 degrees Celsius. This heat is primarily generated by the radioactive decay of elements in the Earth's mantle and core.
well that answer will be 6000 km - depths below surface of earth (km)
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
At a depth of about 1000 kilometers, the temperature of the Earth's interior can reach approximately 1300 to 1500 degrees Celsius (about 2372 to 2732 degrees Fahrenheit). This temperature is primarily due to the immense pressure and the heat generated from the decay of radioactive isotopes within the Earth's mantle and core. The exact temperature can vary based on specific geological conditions and the composition of the surrounding materials.
A depth of 6000 km would be within the lower mantle layer of the Earth. The lower mantle extends from about 660 km to 2900 km below the Earth's surface.
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
5 km
The Earth's crust has an average depth of about 30-50 km. It is primarily composed of oxygen, silicon, aluminum, and iron, with varying amounts of other elements. The temperature of the crust increases with depth, ranging from about 200°C at the surface to over 800°C at the base of the crust.
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.