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.
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 oceanic crust has an average depth in the range of 5-10 kilometers.
The Earth's oceanic crust is very thin at the mid-ocean ridges, and gradually thickens as it moves away from the ridges. The continental crust is thickest under mountain ranges. The average depth of oceanic crust is around 5 miles. The average depth of continental crust is 22 miles.
The Earth's crust has an average depth of about 30-50 km. It is primarily composed of oxygen, silicon, aluminum, and iron, with varying amounts of other elements. The temperature of the crust increases with depth, ranging from about 200°C at the surface to over 800°C at the base of the crust.
The depth of the crust varies between 10 and 70 km in different areas, depending where you would measure it.
the depth of earth's crust
The temperature increases with increasing depth within Earth's crust.
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.
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.
Under the continents, the earth crust is on average around 50 kilometers thick, which is 50,000 meters or 5,000,000 centimeters. Under the oceans, the earth crust is on average around 7 kilometers thick, which is 7,000 meters or 700,000 centimeters.