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 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.
Not if it is within the normal range
It is the state in which the arterial blood pressure 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.
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.