The average temperature on Earth is around 15 degrees Celsius.
The condition found in Earth's asthenosphere that produces partial melting of rock is high temperature and high pressure. The combination of these factors can cause the rock in the asthenosphere to partially melt and form magma, which can then rise towards the Earth's surface and lead to volcanic activity.
The average surface temperature of the Earth is approximately 288 Kelvin (K), which is equivalent to about 15 degrees Celsius or 59 degrees Fahrenheit.
The average temperature at sea level on Earth is around 15 degrees Celsius or 59 degrees Fahrenheit.
The temperature of Earth's crust varies widely depending on location. On average, the temperature of the crust increases by about 25 to 30 degrees Celsius per kilometer of depth. In general, at a depth of 30-40 kilometers, temperatures can reach 500-800 degrees Celsius.
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The highest temperature on Earth is 58 degrees celsius and the low is -88 degrees celsius.
58 degrees Celsius
The average temperature on Earth is around 15 degrees Celsius.
The condition found in Earth's asthenosphere that produces partial melting of rock is high temperature and high pressure. The combination of these factors can cause the rock in the asthenosphere to partially melt and form magma, which can then rise towards the Earth's surface and lead to volcanic activity.
The Wikipedia article on "Earth" mentions that at the center, the temperature "may" be up to 6000 degrees Celsius.
The average surface temperature of the Earth is approximately 288 Kelvin (K), which is equivalent to about 15 degrees Celsius or 59 degrees Fahrenheit.
The average temperature at sea level on Earth is around 15 degrees Celsius or 59 degrees Fahrenheit.
The sun is much hotter than the Earth's crust. The temperature at the Earth's core is estimated to be around 5700 degrees Celsius, whereas the temperature at the surface of the sun is about 5500 degrees Celsius.
The sun is much hotter than the Earth's core. The sun's core temperature reaches millions of degrees Celsius, whereas the Earth's core temperature is estimated to be around 5,000 degrees Celsius.
The temperature of Earth's crust varies widely depending on location. On average, the temperature of the crust increases by about 25 to 30 degrees Celsius per kilometer of depth. In general, at a depth of 30-40 kilometers, temperatures can reach 500-800 degrees Celsius.
The temperature decreases by about 6.5 degrees Celsius per kilometer in the troposphere, so the total temperature change between 3 km and 7 km above the Earth's surface would be approximately 26 degrees Celsius.