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Geophysics

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Geophysics is a physical science that investigates the processes and properties of Earth. It also explores the surrounding space environment. Scientists use quantitative methods and observations to study these systems. This field focuses on the Earth's shape and its invisible fields. These include gravitational, magnetic, and electromagnetic fields.

Earth gravity
Earth gravity

Geophysics looks at the internal structure and composition of the planet. It also examines how internal dynamics create surface features like volcanoes and tectonic plates. This science provides a unifying framework for studying planetary evolution and habitability.

To understand the Earth, geophysicists study several distinct physical phenomena. Gravity is one primary force. The gravitational pull of the Moon and Sun creates tides in our oceans. This results in two high tides and two low tides every lunar day. A lunar day lasts 24 hours and 50 minutes. This leaves a gap of 12 hours and 25 minutes between high tides.

Pswaves
Pswaves

Gravity also affects how rocks behave deep underground. As depth increases, gravity makes rocks press down on each other. This increases the density of the rocks. Scientists use gravity measurements to find mineral deposits or study tectonic plates.

Another major area of study is vibrations, specifically seismic waves. These waves travel through the Earth's interior or along its surface. When an earthquake or explosion occurs, it creates these vibrations. Seismographs are used to measure these ground motions. If waves encounter a change in rock density, they reflect. This is called reflection seismology. It helps scientists map the structure of the Earth several kilometers deep. Scientists also study refraction, which is the change in a wave's travel direction. This helps them infer the deep structure of the planet.

Magnetism is a vital force that protects our planet. The Earth's magnetic field shields us from the solar wind. This field originates from the fluid motions in the outer core.

Geomagnetisme
Geomagnetisme

The field is roughly a tilted dipole, meaning it acts like a magnet with two poles. However, this field changes over time through geomagnetic secular variation. At random intervals, the polarity of the field reverses. These reversals happen every 440,000 to a million years on average.

Geodynamo Between Reversals
Geodynamo Between Reversals

One recent brief reversal, the Laschamp event, occurred 41,000 years ago. Geologists find evidence of these reversals in volcanic rocks and seafloor stripes.

Electricity and electromagnetic waves also play a role in the Earth system. There is a constant downward electric field near the surface. It averages about 120 volts per meter. This is caused by cosmic rays ionizing the atmosphere. This leaves the Earth with a net positive charge. A global current of about 1800 amperes flows in this circuit. This current moves from the ionosphere down to Earth and back up through thunderstorms.

Structure of the magnetosphere mod
Structure of the magnetosphere mod

Electromagnetic waves also occur in the magnetosphere and the Earth's outer core. In the liquid iron of the outer core, electric currents generate magnetic fields through induction.

Heat flow and radioactivity are the engines that drive many planetary processes. Radioactive decay accounts for about 80% of the Earth's internal heat. The main isotopes responsible are potassium-40, uranium-238, uranium-235, and thorium-232.

Thorium decay chain from lead-212 to lead-208
Thorium decay chain from lead-212 to lead-208

This heat powers the geodynamo and plate tectonics. Heat moves to the surface mostly through thermal convection. Some heat travels through the mantle in columns called mantle plumes.

Convection-snapshot
Convection-snapshot

The Earth is constantly cooling, which releases this energy. This heat flow at the surface can even be used as geothermal energy.

Finally, geophysics connects many different scientific fields. It uses fluid dynamics to study the oceans and the atmosphere. The rotation of the Earth affects these fluids through the Coriolis effect. This effect helps determine storm patterns in the atmosphere. In the oceans, it drives large-scale circulation patterns. Geophysics also relies on mineral physics to understand the Earth's interior. By studying how minerals behave, scientists can use seismology to map the deep composition of our world. This integration of theory and observation helps us understand the entire planetary system.

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🖼️ Images & Media (9)
File:Earth gravity.png
Earth gravity.png
File:Pswaves.jpg
Pswaves.jpg
File:Geomagnetisme.svg
Geomagnetisme.svg
File:Geodynamo Between Reversals.gif
Geodynamo Between Reversals.gif
File:Thorium decay chain from lead-212 to lead-208.svg
Thorium decay chain from lead-212 to lead-208.svg
File:Convection-snapshot.png
Convection-snapshot.png
File:Earthquake wave paths.svg
Earthquake wave paths.svg
File:Structure of the magnetosphere mod.svg
Structure of the magnetosphere mod.svg
File:EastHanSeismograph.JPG
EastHanSeismograph.JPG
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