30 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 of the Earth's crust varies depending on location and depth. On average, the temperature increases by about 25-30 degrees Fahrenheit per kilometer of depth. At the surface, the average temperature is around 50-70 degrees Fahrenheit, but it can reach much higher temperatures at greater depths.
False
Temperature generally increases with depth in Earth's crust, with an average increase of about 25 to 30 degrees Celsius per kilometer. This increase is due to the geothermal gradient, which is the rate at which Earth's temperature increases with depth. However, there can be variations in the geothermal gradient depending on factors like local geology, tectonic activity, and heat flow.
The temperature of the Earth's layers increases from the crust towards the core. The outermost layer, the crust, has the lowest temperature, while the inner core has the highest temperature. This gradient is due to the heat generated by radioactive decay in the core and the residual heat from the Earth's formation.
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 of the Earth's crust varies depending on location and depth. On average, the temperature increases by about 25-30 degrees Fahrenheit per kilometer of depth. At the surface, the average temperature is around 50-70 degrees Fahrenheit, but it can reach much higher temperatures at greater depths.
False
it depends on the deepth
The temperature of Earth's crust increases as you go deeper due to geothermal gradient. It varies depending on factors such as location and tectonic activity, but on average, the temperature increases by about 25 to 30 degrees Celsius per kilometer depth. The temperature difference can affect the physical and chemical properties of rocks and minerals found in each layer of the Earth's crust.
Temperature generally increases with depth in Earth's crust, with an average increase of about 25 to 30 degrees Celsius per kilometer. This increase is due to the geothermal gradient, which is the rate at which Earth's temperature increases with depth. However, there can be variations in the geothermal gradient depending on factors like local geology, tectonic activity, and heat flow.
The temperature of the Earth's layers increases from the crust towards the core. The outermost layer, the crust, has the lowest temperature, while the inner core has the highest temperature. This gradient is due to the heat generated by radioactive decay in the core and the residual heat from the Earth's formation.
it depends on the deepth
it depends on the deepth
The temperature increases with increasing depth within Earth's crust.
The earths crust varies. There is no temperature because it varies from cold to hot.
false, the temperature increases with depth