Temperatures at depths up to 2000m, in Europe
2000 celcius
The temperature at the boundary between the asthenosphere and the stiffer mantle is estimated to be around 1300-1400 degrees Celsius. This is where the rock starts to become more rigid due to the increase in temperature and pressure as you move deeper into the Earth.
The crust is the cool part of the Earth. It is the surface we live on. It should be at a comfortable temperature until it reaches down to the mantle, the next layer. That area will be hotter. Then at the center, is the core. That is the hot part of the Earth's interior. It is about 3500° C. Estimates vary from 2000 to 7000, but it is HOT!About 447 in Fahrenheit
From inside out (approximate temperature in Celcius) The inner core is about 7000 degrees C Outer core: 5000 C Lower mantle: 2000 C Upper mantle: 500 C Crust: 0 C
Diamonds form when they're under high pressure.
2000 celcius
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.
Temperature is about 2000 to 3000 degrees celsius maybe less.The mantle is hot but not the hottest layer.It is is the second layer of the Earth. The mantle is the thickest layer of the earth, it is the layer of the earth beneath the crust.Upper mantle and Lower mantle are the two parts of the mantle, The lower mantle is deeper and denser than the upper mantle .
In Depth - 2000 was released on: USA: 6 January 2000
The temperature at the boundary between the asthenosphere and the stiffer mantle is estimated to be around 1300-1400 degrees Celsius. This is where the rock starts to become more rigid due to the increase in temperature and pressure as you move deeper into the Earth.
In Depth was created on 2000-02-06.
Bedrock is at 2000 depth
Iron in the Earth's crust is solid. The melting point of iron is 1811 K, 1538 °C, 2800 °F. The temperature of the crust increases with depth to around 200 °C (392 °F) to 400 °C (752 °F) at the boundary with the mantle below. As depth increases further, so does temperature and pressure. About 2800 kilometers below the Earth, the temperature is high enough that the outer part of the Earth's core is molten metal, an iron and nickle mixture. That is about 2000 kilometers thick and then it appears to become solid again at the very center.
2000 Mickey Mantle Bat Card
I think it might be about 2000 feet.
2000 miles
The crust is the cool part of the Earth. It is the surface we live on. It should be at a comfortable temperature until it reaches down to the mantle, the next layer. That area will be hotter. Then at the center, is the core. That is the hot part of the Earth's interior. It is about 3500° C. Estimates vary from 2000 to 7000, but it is HOT!About 447 in Fahrenheit