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  2. Geothermal gradient - Wikipedia

    en.wikipedia.org/wiki/Geothermal_gradient

    Geothermal gradient is the rate of change in temperature with respect to increasing depth in Earth 's interior. As a general rule, the crust temperature rises with depth due to the heat flow from the much hotter mantle; away from tectonic plate boundaries, temperature rises in about 25–30 °C/km (72–87 °F/mi) of depth near the surface in ...

  3. Earth's crust - Wikipedia

    en.wikipedia.org/wiki/Earth's_crust

    Continental crust is a tertiary crust, formed at subduction zones through recycling of subducted secondary (oceanic) crust. [18] The average age of Earth's current continental crust has been estimated to be about 2.0 billion years. [21] Most crustal rocks formed before 2.5 billion years ago are located in cratons.

  4. Earth - Wikipedia

    en.wikipedia.org/wiki/Earth

    Earth's crust consists of slowly moving tectonic plates, ... This process maintains the current average surface temperature of 14.76 °C (58.57 °F), at which water ...

  5. Global surface temperature - Wikipedia

    en.wikipedia.org/wiki/Global_surface_temperature

    The red line shows direct surface temperature measurements since 1880. [ 2] Global surface temperature (GST) refers to the average temperature of Earth 's surface. It is determined nowadays by measuring the temperatures over the ocean and land, and then calculating a weighted average. The temperature over the ocean is called the sea surface ...

  6. Geothermal energy - Wikipedia

    en.wikipedia.org/wiki/Geothermal_energy

    Outside of the seasonal variations, the geothermal gradient of temperatures through the crust is 25–30 °C (77–86 °F) per km of depth in most of the world. The conductive heat flux averages 0.1 MW/km 2. These values are much higher near tectonic plate boundaries where the crust is thinner.

  7. Asthenosphere - Wikipedia

    en.wikipedia.org/wiki/Asthenosphere

    Asthenosphere. The asthenosphere (from Ancient Greek ἀσθενός (asthenós) 'without strength') is the mechanically weak [ 1] and ductile region of the upper mantle of Earth. It lies below the lithosphere, at a depth between ~80 and 200 km (50 and 120 mi) below the surface, and extends as deep as 700 km (430 mi). However, the lower ...

  8. Geologic temperature record - Wikipedia

    en.wikipedia.org/wiki/Geologic_temperature_record

    The geologic temperature recordare changes in Earth's environmentas determined from geologicevidence on multi-million to billion (109) year time scales. The study of past temperatures provides an important paleoenvironmental insight because it is a component of the climate and oceanographyof the time. Methods.

  9. European climate agency: Last Sunday was the hottest day on ...

    www.aol.com/news/earths-temperature-hit-time...

    Copernicus' preliminary data shows that the global average temperature Sunday was 17.09 degrees Celsius (62.76 degrees Fahrenheit), beating the record set just last year on July 6, 2023 by .01 ...