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The average depth of ocean crust that is 60 million years old is estimated to be around 3.8 kilometers. This depth is determined by the rate of seafloor spreading and the age of the oceanic crust.
The Earth's crust has an average thickness of about 15-30 kilometers (9-20 miles) beneath continents and about 5-10 kilometers (3-6 miles) beneath oceans.
The depth of the crust varies between 10 and 70 km in different areas, depending where you would measure it.
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 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.
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.