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Earth

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Earth

Earth is the third planet from the Sun and the only astronomical object known to harbor life. This is made possible by Earth being an ocean world, the only one in the Solar System sustaining liquid surface water. Almost all of Earth's water is contained in its global ocean, covering 70 % of Earth's crust. The remaining 29 % of Earth's crust is land, most of which is located in the form of continental landmasses within Earth's land hemisphere. Most of Earth's land is at least somewhat humid and covered by vegetation, while large ice sheets at Earth's polar deserts retain more water than Earth's groundwater, lakes, rivers, and atmospheric water combined. Earth's crust consists of slowly moving tectonic plates, which interact to produce mountain ranges, volcanoes, and earthquakes. Earth has a liquid outer core that generates a magnetosphere capable of deflecting most of the destructive solar winds and cosmic radiation. Earth has a dynamic atmosphere, which sustains Earth's surface conditions and protects it from most meteoroids and UV-light at entry. It is composed primarily of nitrogen and oxygen. Water vapor is widely present in the atmosphere, forming clouds that cover most of the planet. The water vapor acts as a greenhouse gas and, together with other greenhouse gases in the atmosphere, particularly carbon dioxide (CO2), creates the conditions for both liquid surface water and water vapor to persist via the capturing of energy from the Sun's light. This process maintains the current average surface temperature of 14 °C (58 °F), at which water is liquid under normal atmospheric pressure. Differences in the amount of captured energy between geographic regions (as with the equatorial region receiving more sunlight than the polar regions) drive atmospheric and ocean currents, producing a global climate system with different climate regions, and a range of weather phenomena such as precipitation, allowing components such as carbon and nitrogen to cycle. Earth is rounded into an ellipsoid with a circumference of about 40,000 kilometers (24,900 miles). It is the densest planet in the Solar System. Of the four rocky planets, it is the largest and most massive. Earth is about eight light-minutes (1 AU) away from the Sun and orbits it, taking a year (about 365 days) to complete one revolution. Earth rotates around its own axis in slightly less than a day (in about 23 hours and 56 minutes). Earth's axis of rotation is tilted with respect to the perpendicular to its orbital plane around the Sun, producing seasons. Earth is orbited by one permanent natural satellite, the Moon, which orbits Earth at 384,400 km (238,855 mi)—1 light seconds—and is roughly a quarter as wide as Earth. The Moon's gravity helps stabilize Earth's axis, causes tides and gradually slows Earth's rotation. Likewise, Earth's gravitational pull has already made the Moon's rotation tidally locked, keeping the same near side facing Earth. Earth, like most other bodies in the Solar System, formed about 4 billion years ago from gas and dust in the early Solar System. The formation of the ocean and the subsequent development of life occurred during the first billion years of Earth's history. Life spread globally and has been altering Earth's atmosphere and surface, leading to the Great Oxidation Event two billion years ago. Humans emerged 300,000 years ago in Africa and have spread across every continent on Earth. Humans depend on Earth's biosphere and natural resources for their survival, but have increasingly impacted the planet's environment. Humanity's current impact on Earth's climate and biosphere is unsustainable, threatening the livelihood of humans and many other forms of life, and causing widespread extinctions.

Infobox

Alternative names
The world The globe Terra Tellus Gaia
Adjectives
Earthly Terrestrial Terran Tellurian
Symbol
and
Aphelion
152097597 km
Perihelion
147098450 km
Semi-major axis
149598023 km
Eccentricity
0
Orbital period (sidereal)
365 d (1 aj)
Average orbital speed
29 km/s
Mean anomaly
358 °
Inclination
7 ° – Sun's equator; 1 ° – invariable plane; 0 ° – J2000 ecliptic
Longitude of ascending node
−11 ° – J2000 ecliptic
Time of perihelion
3 January 2026
Argument of perihelion
114 °
Satellites
1, the Moon
Mean radius
6371 km
Equatorial radius
6378 km
Polar radius
6356 km
Flattening
1/298 (ETRS89)
Circumference
40075 km equatorial 40007 km meridional
Surface area
510072000 km2 Land: 148940000 km2 Water: 361132000 km2
Volume
1 ×1012 km3
Mass
(5 ±0 )×1024 kg
Mean density
5 g/cm3
Surface gravity
9 m/s2 (exactly 1 g0)
Moment of inertia factor
0
Escape velocity
11 km/s
Synodic rotation period
1 d (24h 00 m 00s)
Sidereal rotation period
0 d (23h 56 m 4 )
Equatorial rotation velocity
1674 km/h
Axial tilt
23 °
Albedo
0 geometric 0 Bond
Temperature
255 K (−18 °C) (blackbody temperature)
Surface temp.
Surface temp. min mean max −89 °C 14 °C 56 °C
Surface equivalent dose rate
0 μSv/h
Absolute magnitude (H)
−3
Surface pressure
101 kPa (at sea level)
Composition by volume
78 % nitrogen (dry air) 20 % oxygen (dry air) ≤1% water vapor (variable) 0 % argon 0 % carbon dioxide 0 % neon 0 % helium 0 % methane 0 % krypton 0 % hydrogen Source:

Tables

Geologic layers of Earth · Bulk properties › Internal structure
Depth (km)
Depth (km)
Illustration of Earth's cutaway, not to scale
Depth (km)
Illustration of Earth's cutaway, not to scale
Component layer name
Illustration of Earth's cutaway, not to scale
Density (g/cm3)
0–60
0–60
Illustration of Earth's cutaway, not to scale
0–60
Illustration of Earth's cutaway, not to scale
Lithosphere
Illustration of Earth's cutaway, not to scale
0–35
0–35
Illustration of Earth's cutaway, not to scale
0–35
Illustration of Earth's cutaway, not to scale
Crust
Illustration of Earth's cutaway, not to scale
2 –2
35–660
35–660
Illustration of Earth's cutaway, not to scale
35–660
Illustration of Earth's cutaway, not to scale
Upper mantle
Illustration of Earth's cutaway, not to scale
3 –4
660–2,890
660–2,890
Illustration of Earth's cutaway, not to scale
660–2,890
Illustration of Earth's cutaway, not to scale
Lower mantle
Illustration of Earth's cutaway, not to scale
3 –5
100–700
100–700
Illustration of Earth's cutaway, not to scale
100–700
Illustration of Earth's cutaway, not to scale
Asthenosphere
Illustration of Earth's cutaway, not to scale
2,890–5,100
2,890–5,100
Illustration of Earth's cutaway, not to scale
2,890–5,100
Illustration of Earth's cutaway, not to scale
Outer core
Illustration of Earth's cutaway, not to scale
9 –12
5,100–6,378
5,100–6,378
Illustration of Earth's cutaway, not to scale
5,100–6,378
Illustration of Earth's cutaway, not to scale
Inner core
Illustration of Earth's cutaway, not to scale
12 –13
Illustration of Earth's cutaway, not to scale
Depth (km)
Component layer name
Density (g/cm3)
0–60
Lithosphere
0–35
Crust
2 –2
35–660
Upper mantle
3 –4
660–2,890
Lower mantle
3 –5
100–700
Asthenosphere
2,890–5,100
Outer core
9 –12
5,100–6,378
Inner core
12 –13

References

  1. All astronomical quantities vary, both secularly and periodically. The quantities given are the values at the instant J2
  2. Probing the New Solar System
  3. Earth's circumference is almost exactly 40,000 km because the meter was calibrated on this measurement—more specifically
  4. Due to natural fluctuations, ambiguities surrounding ice shelves, and mapping conventions for vertical datums, exact val
    http://www.landcover.org/
  5. Source for minimum, mean, and maximum surface temperature
  6. If Earth were shrunk to the size of a billiard ball, some areas of Earth such as large mountain ranges and oceanic trenc
  7. Journal of African Earth Sciences
    https://ui.adsabs.harvard.edu/abs/2005JAfES..43..379C
  8. Locally varies between 5 and 200 km.
  9. Locally varies between 5 and 70 km.
  10. Astronomy and Astrophysics
    https://ui.adsabs.harvard.edu/abs/1982A&A...105..359A
  11. Aphelion is 103 % of the distance to perihelion. Due to the inverse square law, the radiation at perihelion is about 106
  12. For Earth, the Hill radius is R H = a ( m 3 M ) 1 3 {\display
  13. Orbital Debris Quarterly News
    https://orbitaldebris.jsc.nasa.gov/quarterly-news/pdfs/odqnv22i1.pdf
  14. Astronomy and Astrophysics
    https://ui.adsabs.harvard.edu/abs/1994A&A...282..663S
  15. "Useful Constants"
    http://hpiers.obspm.fr/eop-pc/models/constants.html
  16. NSSDCA
    https://nssdc.gsfc.nasa.gov/planetary/factsheet/earthfact.html
  17. Allen's Astrophysical Quantities
    https://books.google.com/books?id=w8PK2XFLLH8C&pg=PA294
  18. Handbook of Chemistry and Physics
    https://archive.org/details/crchandbookofche81lide
  19. The Astronomical Almanac
    https://web.archive.org/web/20130826043456/http://asa.usno.navy.mil/SecK/2011/Astronomical_Constants_2011.txt
  20. World Geodetic System (WGS-84). Available online Archived 11 March 2020 at the Wayback Machine from National Geospatial-
    http://earth-info.nga.mil/GandG/wgs84/
Image
Source:
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