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Earth science

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Earth science

A volcanic eruption is the release of stored energy from below the surface of Earth, originating from radioactive decay and gravitational sorting in the Earth's core and mantle, and residual energy gained during the Earth's formation[1]

Earth science or geoscience is an all-embracing term referring to the fields of science dealing with planet Earth.[2] It is arguably a special branch of planetary science, though with a much older history. There are both reductionist and holistic approaches to Earth sciences. The formal discipline of Earth sciences may include the study of the atmosphere, hydrosphere, and biosphere, as well as the solid Earth. Typically, Earth scientists will use tools from physics, chemistry, biology, chronology, and mathematics to build a quantitative understanding of how the Earth system works, and how it evolved to its current state.

Contents

  • Fields of study 1
  • Earth's interior 2
  • Earth's electromagnetic field 3
  • Earth's atmosphere 4
  • Methodology 5
  • Earth's spheres 6
    • Partial list of the major earth science topics 6.1
      • Atmosphere 6.1.1
      • Biosphere 6.1.2
      • Hydrosphere 6.1.3
      • Lithosphere or geosphere 6.1.4
      • Pedosphere 6.1.5
      • Systems 6.1.6
      • Others 6.1.7
  • See also 7
  • References 8
  • Further reading 9
  • External links 10

Fields of study

Lava flows from the Kīlauea volcano into the ocean on the Island of Hawaii

The following fields of science are generally categorized within the Earth sciences:

Earth's interior

Plate tectonics, mountain ranges, volcanoes, and earthquakes are geological phenomena that can be explained in terms of energy transformations in the Earth's crust.[10] Beneath the Earth's crust lies the mantle which is heated by the radioactive decay of heavy elements. The mantle is not quite solid and consists of magma which is in a state of semi-perpetual convection. This convection process causes the lithospheric plates to move, albeit slowly. The resulting process is known as plate tectonics.[11][12][13][14]

Plate tectonics might be thought of as the process by which the earth is resurfaced. Through a process called seafloor spreading, new crust is created by the flow of magma from underneath the lithosphere to the surface, through fissures, where it cools and solidifies. Through a process called subduction, oceanic crust is pushed underground — beneath the rest of the lithosphere—where it comes into contact with magma and melts—rejoining the mantle from which it originally came.[12][14][15]

Areas of the crust where new crust is created are called divergent boundaries, those where it is brought back into the earth are convergent boundaries and those where plates slide past each other, but no new lithospheric material is created or destroyed, are referred to as transform (or conservative) boundaries[12][14][16] Earthquakes result from the movement of the lithospheric plates, and they often occur near convergent boundaries where parts of the crust are forced into the earth as part of subduction.[17] Volcanoes result primarily from the melting of subducted crust material. Crust material that is forced into the asthenosphere melts, and some portion of the melted material becomes light enough to rise to the surface—giving birth to volcanoes.[12][17]

Earth's electromagnetic field

An electromagnet is a magnet that is created by a current that flows around a soft iron core.[18] Earth has a solid iron inner core surrounded by semi-liquid materials of the outer core that move in continuous currents around the inner core;[19] therefore, the Earth is an electromagnet. This is referred to as the dynamo theory of Earth's magnetism.[19][20]

Earth's atmosphere

The magnetosphere shields the surface of Earth from the charged particles of the solar wind. It is compressed on the day (Sun) side due to the force of the arriving particles, and extended on the night side. Image not to scale.

The troposphere, stratosphere, mesosphere, thermosphere, and exosphere are the five layers which make up Earth's atmosphere. In all, the atmosphere is made up of about 78.0% nitrogen, 20.9% oxygen, and 0.92% argon. 75% of the gases in the atmosphere are located within the troposphere, the bottom-most layer. The remaining one percent of the atmosphere (all but the nitrogen, oxygen, and argon) contains small amounts of other gases including CO2 and water vapors.[21] Water vapors and CO2 allow the Earth's atmosphere to catch and hold the Sun's energy through a phenomenon called the greenhouse effect.[22] This allows Earth's surface to be warm enough to have liquid water and support life.

The magnetic field created by the internal motions of the core produces the magnetosphere which protects the Earth's atmosphere from the solar wind.[23] As the earth is 4.5 billion years old,[24] it would have lost its atmosphere by now if there were no protective magnetosphere.

In addition to storing heat, the atmosphere also protects living organisms by shielding the Earth's surface from cosmic rays. Note that the level of protection is high enough to prevent cosmic rays from destroying all life on Earth, yet low enough to aid the mutations that have an important role in pushing forward diversity in the biosphere.

Methodology

Methodologies vary depending on the nature of the subjects being studied. Studies typically fall into one of three categories: observational, experimental, or theoretical. Earth scientists often conduct sophisticated computer analysis or go to many of the world's most exotic locations to study Earth phenomena (e.g. Antarctica or hot spot island chains).

A foundational idea within the study Earth science is the notion of uniformitarianism. Uniformitarianism dictates that "ancient geologic features are interpreted by understanding active processes that are readily observed." In other words, any geologic processes at work in the present have operated in the same ways throughout geologic time. This enables those who study Earth's history to apply knowledge of how Earth processes operate in the present to gain insight into how the planet has evolved and changed throughout deep history.

Earth's spheres

Earth science generally recognizes four spheres, the lithosphere, the hydrosphere, the atmosphere, and the biosphere;[25] these correspond to rocks, water, air, and life. Some practitioners include, as part of the spheres of the Earth, the cryosphere (corresponding to ice) as a distinct portion of the hydrosphere, as well as the pedosphere (corresponding to soil) as an active and intermixed sphere.

Partial list of the major earth science topics

See: List of basic earth science topics

Atmosphere

Biosphere

Hydrosphere

Lithosphere or geosphere

Pedosphere

Systems

Others

See also

References

  1. ^ Encyclopedia of Volcanoes, Academic Press, London, 2000
  2. ^ "earth science". Memidex/WordNet Dictionary. Retrieved 2012-06-11. 
  3. ^ Adams & Lambert 2006, p. 20
  4. ^ a b Smith & Pun 2006, p. 5
  5. ^ Fundamentals of Physical Geography, 2nd Edition, by M. Pidwirny, 2006
  6. ^ Wordnet Search: Geodesy
  7. ^ NOAA National Ocean Service Education: Geodesy
  8. ^ Elissa Levine, 2001, The Pedosphere As A Hub broken link?
  9. ^ Duane Gardiner, Lecture: Why Study Soils? excerpted from Miller, R.W. & D.T. Gardiner, 1998. Soils in our Environment, 8th Edition
  10. ^ Earth's Energy Budget
  11. ^ Simison 2007, paragraph 7
  12. ^ a b c d Adams & Lambert 2006, pp. 94,95,100,102
  13. ^ Smith & Pun 2006, pp. 13–17,218,G-6
  14. ^ a b c Oldroyd 2006, pp. 101,103,104
  15. ^ Smith & Pun 2006, p. 327
  16. ^ Smith & Pun 2006, p. 331
  17. ^ a b Smith & Pun 2006, pp. 325,326,329
  18. ^ American Heritage, p. 576
  19. ^ a b Oldroyd 2006, p. 160
  20. ^ Demorest, Paul (2001-05-21). "Dynamo Theory and Earth's Magnetic Field.". Retrieved 2007-11-17. 
  21. ^ Adams & Lambert 2006, pp. 107–108
  22. ^ American Heritage, p. 770
  23. ^ Adams & Lambert 2006, pp. 21–22
  24. ^ Smith & Pun 2006, p. 183
  25. ^ Earth's Spheres. ©1997-2000. Wheeling Jesuit University/NASA Classroom of the Future. Retrieved November 11, 2007.

Further reading

  • Allaby M., 2008. Dictionary of Earth Sciences, Oxford University Press, ISBN 978-0-19-921194-4
  • Adams, Simon; Lambert, David (2006). Earth Science: An illustrated guide to science. New York, NY: Chelsea House.  
  • Joseph P. Pickett (executive editor) (1992). American Heritage dictionary of the English language (4th ed.). Boston, MA:  
  • Korvin G., 1998. Fractal Models in the Earth Sciences, Elsvier, ISBN 978-0-444-88907-2
  • "Earth's Energy Budget". Oklahoma Climatological Survey. 1996–2004. Retrieved 2007-11-17. 
  • Miller, George A.; Christiane Fellbaum; and Randee Tengi; and Pamela Wakefield; and Rajesh Poddar; and Helen Langone; Benjamin Haskell (2006). "WordNet Search 3.0". WordNet a lexical database for the English language. Princeton University/Cognitive Science Laboratory /221 Nassau St./ Princeton, NJ 08542. Retrieved 2007-11-10. 
  • "NOAA National Ocean Service Education: Geodesy". National Oceanic and Atmospheric Administration. 2005-03-08. Retrieved 2007-11-17. 
  • Oldroyd, David (2006). Earth Cycles: A historical perspective. Westport, Connicticut: Greenwood Press.  
  • Reed, Christina (2008). Earth Science: Decade by Decade. New York, NY: Facts on File.  
  • Simison, W. Brian (2007-02-05). "The mechanism behind plate tectonics". Retrieved 2007-11-17. 
  • Smith, Gary A.; Pun, Aurora (2006). How Does the Earth Work? Physical Geology and the Process of Science. Upper Saddle River, NJ 07458: Pearson Prentice Hall.  
  • Tarbuck E. J., Lutgens F. K., and Tasa D., 2002. Earth Science, Prentice Hall, ISBN 978-0-13-035390-0

External links

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