because the oceanic crust lithospher descend into the mantle at the subduction zone .it will be taken to increasing higher temperature as it get deeper
The geothermal gradient in the Earth's continental crust typically ranges from about 20 to 30°C per kilometer depth. This means the temperature increases by 20-30°C for every kilometer you go deeper into the Earth's continental crust.
The average rate of temperature increase below the Earth's surface is about 25 to 30 degrees Celsius per kilometer of depth. This increase is known as the geothermal gradient and varies depending on factors such as location, tectonic activity, and local geology.
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.
Earth's average temperature is about 14 or 15 degrees Celsius although it varies a few degrees depending on your source. The hottest temperature recorded on Earth was 70.7°C (159°F) in the Lut Desert in Iran.
The total change in elevation is 200 meters and the total distance traveled is 400 kilometers. The average gradient in meters per kilometer can be calculated as the total change in elevation divided by the total distance, which is 200 meters / 400 km = 0.5 meters per kilometer.
The average geothermal gradient is around 25 to 30 degrees Celsius per kilometer of depth in the Earth's crust. This means that the temperature increases by this amount for every kilometer you descend into the Earth.
Geothermal gradient refers to the increase in temperature with depth below the Earth's surface. On average, the geothermal gradient is about 25-30°C per kilometer. This gradient varies depending on factors like location and geologic conditions.
gradient
The geothermal gradient in the Earth's continental crust typically ranges from about 20 to 30°C per kilometer depth. This means the temperature increases by 20-30°C for every kilometer you go deeper into the Earth's continental crust.
The average geothermal gradient in non-volcanic areas is typically around 25-30 degrees Celsius per kilometer of depth. This means that the temperature increases by this amount for every kilometer deeper into the Earth's crust.
The temperature at 2.4 miles underground can vary depending on various factors such as the geothermal gradient of the area and the composition of the surrounding rocks. On average, the geothermal gradient is about 25-30°C per kilometer depth, so at 2.4 miles (approximately 3.86 kilometers) underground, the temperature could be around 96-116°C (204-241°F). However, it's important to note that this is a rough estimate and actual temperatures can differ based on specific geological conditions.
The soil temperatre increases as depth increases due to the heat created by the compression of the surrounding earth. The rate of change of temperature with depth is referred to as the geothermal gradient. The geothermal gradient varies depending on location, so there is no uniform answer. On average, the geothermal gradient is approximately 75 degrees F per mile. In volcanically active areas, the gradient can be as high as 150 degrees F per mile. In ocean trenches, the gradient may be as low as 15 degrees F per mile. Decay of naturally occurring radioactive elements may also cause localized increases in temperature in some locations.
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.
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The average rate at which temperature increases with depth in the Earth's crust is approximately 25-30°C per kilometer. This is known as the geothermal gradient and varies depending on factors such as location, geology, and tectonic activity.
The temperature at 3.4 km below the Earth's surface generally increases with depth due to geothermal heating. On average, the geothermal gradient is about 25-30 degrees Celsius per kilometer, so at 3.4 km below the surface, the temperature could be around 85-102 degrees Celsius.
divide by the gradient