Its about .1 to 1.5 million atmosheres.
The temperature range within the stiffer mantle is between 500 and 900 degrees Celsius. This region is known as the upper mantle and is composed of solid rock that can deform under high pressure and temperature.
Its about .1 to 1.5 million atmosheres.
The density of Earth's mantle varies depending on its depth. The part right below the crust has a density of about 3.4 grams per cubic centimeter while the lowest part of the mantle is 5.6 grams per cubic centimeter.
The temperature of the Earth's mantle can range from 1,300 to 2,400 degrees Celsius (2,372 to 4,352 degrees Fahrenheit). These temperatures vary depending on the location within the mantle and can be influenced by factors such as depth and proximity to the core.
The pressure in the Earth's crust can vary but is typically around 200 to 400 megapascals. In the mantle, pressures range from about 30 to 140 gigapascals. In the core, pressures are extremely high, reaching up to 360 to 370 gigapascals in the inner core.
Its about .1 to 1.5 million atmosheres.
The temperature range within the stiffer mantle is between 500 and 900 degrees Celsius. This region is known as the upper mantle and is composed of solid rock that can deform under high pressure and temperature.
Its about .1 to 1.5 million atmosheres.
The stiffer mantle (upper) is one of the layers of the earth's crust and composed of hot liquid rock. The range of density is between 3-100 or 3.4g/cm and 4.3g/cm.
The stiffer mantle (upper) is one of the layers of the earth's crust and composed of hot liquid rock. The range of density is between 3-100 or 3.4g/cm and 4.3g/cm.
The stiffer mantle (upper) is one of the layers of the earth's crust and composed of hot liquid rock. The range of density is between 3-100 or 3.4g/cm and 4.3g/cm.
The boundary between the plastic (asthenosphere) and the stiffer mantle (lithosphere) is typically found at depths of about 100 to 700 kilometers beneath the Earth's surface. At this depth, the pressure can range from approximately 3 to 25 gigapascals, and temperatures can vary between 1,300 to 3,000 degrees Celsius. This transition zone marks a significant change in the physical properties of the mantle materials.
The stiffer mantle, often referred to as the upper mantle, extends from about 35 kilometers (22 miles) to approximately 660 kilometers (410 miles) below Earth's surface. It is composed of solid rock that behaves viscously over long periods, accommodating tectonic processes without flowing like the molten rock found in the lower mantle. The transition between the upper and lower mantle occurs at around 660 kilometers, where the material becomes more ductile due to increased pressure and temperature.
The density of Earth's mantle varies depending on its depth. The part right below the crust has a density of about 3.4 grams per cubic centimeter while the lowest part of the mantle is 5.6 grams per cubic centimeter.
The inferred temperature at the interface between the stiffer mantle and the asthenosphere is closest to approximately 1300 to 1500 degrees Celsius (2372 to 2732 degrees Fahrenheit). This temperature range is crucial for the behavior of the asthenosphere, as it becomes partially molten and more ductile, allowing for mantle convection and tectonic plate movement.
Not if it is within the normal range
The temperature of the Earth's mantle can range from 1,300 to 2,400 degrees Celsius (2,372 to 4,352 degrees Fahrenheit). These temperatures vary depending on the location within the mantle and can be influenced by factors such as depth and proximity to the core.