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Computer simulation of the Earth's magnetic field in a period of normal polarity between reversals.
Geophysics

Geophysics (/ˌdʒiːoʊˈfɪzɪks/) is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations and pure scientists use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial physics; and analogous problems associated with the Moon and other planets.

Although geophysics was only recognized as a separate discipline in the 19th century, its origins date back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 AD. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.

Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. In Exploration geophysics, geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.
Some geophysicists now also study the hydrological cycle including snow and ice. They study how the oceans and the atmosphere move. They study electricity and magnetism in the atmosphere, ionosphere, and magnetosphere. How the earth and sun affect each other is also part of geophysics.
Geophysics was only recognized as a special area of study in the 19th century. But, there were geophysicists in ancient history. The first magnetic compasses were made in the fourth century BC and the first seismoscope was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox. Instruments were developed to measure the Earth's shape, density and gravity field, as well as parts of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean.
Studying geophysics may help with problems such as mineral resources, reducing natural hazards, and protecting the environment. Geophysical survey data help find petroleum reservoirs, mineral deposits, groundwater, and archaeological relics. Such data can also tell the thickness of glaciers and soils, and tell which areas have environmental damage that should be fixed.

Kiddle: Geophysics
Wikipedia: Geophysics
 
 
 
 
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