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Lecture 20 Earth's Interior and Geophysical Properties
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Lecture Outline IEarth's Internal Structure A)The Crust B)The Mantle C)The Core i.Composition ii.Core-Mantle Boundary IIIsostasy IIIEarth's Gravity IVEarth's Magnetic Field A)Magnetic Reversals B)Magnetic Anomalies VHeat Within the Earth VIConclusions Lecture 20 i
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Geophysics photo by John Galetzka, USGS geophysics: the branch of earth science which employs physical measurements and mathematical models to explore and analyze the structure and dynamics of the solid Earth and other bodies and their fluid envelopes
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Controls on Seismic Wave Velocity pressure state of matter composition of matter
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Controls on Seismic Wave Velocity Pressure
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Controls on Seismic Wave Velocity Composition Material V p (ms -1 ) Density (gcm -3 ) Salt 4.6 2.2 Quartz 6.1 2.7 Calcite 6.7 2.7 Dolomite 7.4 2.9 Siderite 7.0 4.0 Pyrite 8.4 5.0
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Controls on Seismic Wave Velocity State of Matter
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Earth's Internal Structure crust mantle core
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Earth's Internal Structure The Crust Mohorovicic Discontinuity (Moho)
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Earth's Internal Structure Crustal Thickness
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Earth's Internal Structure Crustal Thickness (United States)
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Earth's Internal Structure The Composition of the Crust
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Earth's Internal Structure The Mantle
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Mantle is Solid (S waves propagate) Mantle is Rigid (seismic waves propagate) Mantle is Fluid (convection cells present)
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Earth's Internal Structure The Composition of the Mantle Hofman Hart and Zindler Hutchinson Mason 1988 1986 1974 1966 SiO 2 45.96 46.38 45.00 48.10 MgO 37.78 38.12 39.00 31.10 FeO 7.54 7.62 8.00 12.70 Al 2 O 3 4.06 4.10 3.50 3.10 CaO 3.21 3.24 3.25 2.30
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Earth's Internal Structure The Core Size: radius 3480 km (1/2 Earth) volume 1/8 Earth mass 1/3 Earth Properties: density10-13 g/cm 3 pressure136-330 GPa temperature5500±1500 K stateliquid-solid
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Earth's Internal Structure Composition of the Core Iron Nickel ~ 4% Light Element (O or S) 10% by mass
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Earth's Internal Structure Major Discontinuities crust/mantle - the MOHO inside mantle (400 km and 670 km) mantle/outer core (CMB) outer/inner core (ICB)
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Earth's Internal Structure Major Discontinuities - The Moho
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Earth's Internal Structure The Core-Mantle Boundary MAJOR Discontinuity S-waves blocked by liquid outer core
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Isostasy the condition of equilibrium, comparable to floating, of the units of the lithosphere above the asthenosphere.
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Isostasy
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Isostastic Adjustment erosion and deposition glacial rebound crustal thickening
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Isostastic Adjustment Erosion and Deposition
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Isostastic Adjustment Glacial Rebound
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Isostastic Adjustment Crustal Thickening
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Gravity gravity: the attraction between two masses, such as the Earth and an object on its surface. Commonly referred to as the acceleration of gravity (g).
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Gravity
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Gravity Anomaly
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Earth's Magnetic Field
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Rock Magnetism
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Earth's Magnetic Field
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Heat within the Earth
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Sources of Earth's Heat Pressure Sunlight Radioactive Decay Primordial Heat
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Redistribution of Earth's Heat Radiation Conduction Convection
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Redistribution of Earth's Heat Conduction
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Redistribution of Earth's Heat Convection
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