1 gigapascal is 1,000,000,000 Pa (pascals)
68.9 Gigapascals (GPa) , or 10,000,000 psi
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At 4000 km depth, the pressure would be incredibly high due to the weight of the overlying rock and material. The pressure can be estimated to be in the range of several hundred gigapascals at that depth.
The pressure at a depth of 3000 km in the Earth's mantle is estimated to be around 135 GPa (gigapascals), which is equivalent to about 1.35 million atmospheres of pressure. This immense pressure is a result of the weight of the overlying rocks and the gravitational forces acting on the materials at that depth.
The modulus of elasticity of styrofoam, also known as expanded polystyrene (EPS), typically ranges from 10-40 MPa (megapascals). This value represents the material's ability to deform elastically under stress and return to its original shape when the stress is removed. The low modulus of elasticity of styrofoam makes it a lightweight and flexible material commonly used in packaging and insulation applications.
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.
Under high pressure - around 150 gigaPascals - xenon turns metallic. In this phase it has a blue colour.
68.9 Gigapascals (GPa) , or 10,000,000 psi
The pressure of the Earth's crust varies depending on location and depth, but it can range from about 10 to 30 kilobars (1 to 3 gigapascals).
Yes, because it is in the center of the Earth.
Most riot shields list the material of construction as Lexan, the trade name for the polycarbonate polymer. The young's modulus of polycarbonate is 2.0-2.4 GPa (gigapascals).
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The Earth's inner core has the greatest temperature, reaching up to around 5700 degrees Celsius. The layer with the greatest pressure is the inner core as well, with pressures exceeding 330 to 360 gigapascals.
At 4000 km depth, the pressure would be incredibly high due to the weight of the overlying rock and material. The pressure can be estimated to be in the range of several hundred gigapascals at that depth.
The psi of the outer core is the rounding core actullay know as inside.
The pressure at a depth of 3000 km in the Earth's mantle is estimated to be around 135 GPa (gigapascals), which is equivalent to about 1.35 million atmospheres of pressure. This immense pressure is a result of the weight of the overlying rocks and the gravitational forces acting on the materials at that depth.
At the center of the inner core the pressure is roughly 3,600,000 atmospheres. According to Wikipedia.