Table of Contents
What is the pressure in the asthenosphere?
The asthenosphere is approximately 200 km [124 miles] thick and, owing to its depth below the Earth’s surface, warm (~ 1,400 degC [2,640 degF]) but not molten. Here the mantle deforms by plastic flow in response to applied pressures above 100 MPa [14,500 psi].
What is the pressure at the boundary between the asthenosphere and the stiffer mantle?
The pressure at the boundary between the mantle and the outer core of Earth is inferred to be approximately… 1.4 million atmospheres. What is the inferred temperature at the boundary between Earth’s stiffer mantle and outer core?
What is between the crust and the asthenosphere?
The upper mantle extends from the crust to a depth of about 410 kilometers (255 miles). The upper mantle is mostly solid, but its more malleable regions contribute to tectonic activity. Two parts of the upper mantle are often recognized as distinct regions in Earth’s interior: the lithosphere and the asthenosphere.
What is the pressure of the earth’s crust ATM?
The standard, or near-average, atmospheric pressure at sea level on the Earth is 1013.25 millibars, or about 14.7 pounds per square inch.
What is the pressure at the boundary between the outer core and the inner core?
Extrapolating from that measurement, scientists estimated the boundary between Earth’s inner and outer core is a searing 10,832 F, give or take about 930 degrees, at a pressure of 3.3 million atmospheres (or 3.3 million times the atmospheric pressure at sea level).
Is the asthenosphere part of the Earth’s crust?
The lithosphere is the solid, outer part of the Earth. The lithosphere includes the brittle upper portion of the mantle and the crust, the outermost layers of Earth’s structure. It is bounded by the atmosphere above and the asthenosphere (another part of the upper mantle) below.
How does the lithospheric mantle differ from the asthenosphere?
The lithosphere is the brittle crust and uppermost mantle. The asthenosphere is a solid but it can flow, like toothpaste. The lithosphere rests on the asthenosphere.
What is the pressure of the crust GPa?
1 gigapascal
For our purposes, 1 atmosphere is the pressure of air at the surface of the earth. This pressure is also commonly given in units of a “bar”. 1 kilobar = 1 kbar = 1000 bars = 1000 atmospheres of pressure. 1 GPa = 1 gigapascal = 10 kbar….
Region (depths) | Mineralogy |
---|---|
Crust (average depth 40 km) | Feldspar, quartz |
What is the temperature and pressure of the asthenosphere?
Asthenosphere is plastic-like viscous rock; more solid closer to core. High temperature and pressure: 500-900°C (932-1652°F) at the boundary with the crust; over 4000°C (7230°F) at the boundary with the core.
Is the lithosphere the same as the asthenosphere boundary?
The lithosphere–asthenosphere boundary (referred to as the LAB by geophysicists) represents a mechanical difference between layers in Earth’s inner structure. Earth’s inner structure can be described both chemically ( crust, mantle, and core) and mechanically.
How is the continental crust compared to the oceanic crust?
Compared to the average density and composition of oceanic crust, continental crust is What are the inferred pressure and temperature at the boundary of Earth’s stiffer mantle and outer core?
Where is the boundary between the core and the mantle?
At the base of the mantle, about 2,900 kilometers (1,802 miles) below the surface, is the core-mantle boundary, or CMB. This point, called the Gutenberg discontinuity, marks the end of the mantle and the beginning of Earth’s liquid outer core.