It is the largest of the solar system's terrestrial planets, and the only planetary body that modern science confirms as harbouring life. The planet formed around 4.5 billion (4.5×109) years ago and shortly thereafter acquired its single natural satellite, the Moon.
Physical characteristics Edit
Main article: Geology
The interior of Earth, like that of the other terrestrial planets, is chemically divided into an outer siliceous solid crust, a highly viscous mantle, a liquid outer core that is much less viscous than the mantle, and a solid inner core. The liquid outer core gives rise to a weak magnetic field due to the convection of its electrically conductive material.
New material constantly finds its way to the surface through volcanoes and cracks in the ocean floors (see seafloor spreading). Much of Earth's crust is less than 100 million (1×108) years old; the very oldest parts of the crust are as much as 4.4 billion (4.4×109) years old .
Taken as a whole, Earth's composition by mass is:
- 34.6% Iron
- 29.5% Oxygen
- 15.2% Silicon
- 12.7% Magnesium
- 2.4% Nickel
- 1.9% Sulfur
- 0.05% Titanium
- 3.65% Other elements
See also gravity inside the Earth.
The interior of Earth reaches temperatures of 5270 K. The planet's internal heat was originally generated during its accretion (see gravitational binding energy), and since then additional heat has continued to be generated by the decay of radioactive elements such as uranium, thorium, and potassium. The heat flow from the interior to the surface is only 1/20,000 as great as the energy received from the Sun.
- 0-60 km - Lithosphere
- 0-30/35 km - Crust
- 30/35-2900 km - Mantle
- 100-700 km - Asthenosphere
- 2900-5100 km - Outer Core
- 5100-~6375 km - Inner Core
The average density of Earth is 5,515 kg/m3, making it the most dense planet in the Solar system. Since the average density of surface material is only around 3000 kg/m3, we must conclude that denser materials exist within the core of the Earth. In its earliest stages, about 4.5 billion (4.5×109) years ago, the Earth was mostly molten, and as a result gravity would have caused denser substances to sink towards the center in a process called planetary differentiation, while less dense materials would have migrated to the crust. As a result, the core is largely composed of iron (80%), along with nickel and silicon; while other dense elements, such as lead and uranium, are either too rare to be significant or tend to bind to lighter elements and thus remain in the crust (see: felsic materials).
The core is divided into two parts, a solid inner core with a radius of ~1250 km and a liquid outer core extending beyond it to a radius of ~3500 km. The inner core is generally believed to be solid and composed primarily of iron and some nickel. Some have argued that the inner core may be in the form of a single iron crystal. The outer core surrounds the inner core and is believed to be composed of liquid iron mixed with liquid nickel and trace amounts of lighter elements. It is generally believed that convection in the outer core, combined with stirring caused by the Earth's rotation (see: Coriolis forces), gives rise to the Earth's magnetic field through a process known as the dynamo theory. The solid inner core is too hot to hold a permanent magnetic field (see: Curie temperature) but probably acts to stabilise the magnetic field generated by the liquid outer core.
Earth's mantle extends to a depth of 2,900 km. The pressure, at the bottom of the mantle, is ~1.4 Matm (140 GPa). It is largely composed of substances rich in iron and magnesium. The melting point of a substance depends on the pressure it is under. As there is intense and increasing pressure as one travels deeper into the mantle, the lower part of this region is thought solid while the upper mantle is plastic (semi-molten). The viscosity of the upper mantle ranges between 1021 and 1024 Pa·s, depending on depth . Thus, the upper mantle can only flow very slowly.
Why is the inner core thought solid, the outer core thought liquid, and the mantle solid/plastic? The melting point of iron rich substances are higher than pure iron. The core is composed almost entirely of pure iron, while iron rich substances are more common outside the core. So, surface iron-substances are solid, upper mantle iron-substances are semi-molten (as it is hot and they are under relatively little pressure), lower mantle iron-substances are solid (as they are under tremendous pressure), outer core pure iron is liquid as it has a very low melting point (despite enormous pressure), and the inner core is solid due to the overwhelming pressure found at the center of the planet.
The crust ranges from 5 to 35 km in depth. The thin parts are oceanic crust composed of dense (mafic) iron magnesium silicate rocks and underlie the ocean basins. The thicker crust is continental crust which is less dense and composed of (felsic) sodium potassium aluminium silicate rocks. The crust-mantle boundary occurs as two physically different events. Firstly, there is a discontinuity in the seismic velocity which is known as the Mohorovicic discontinuity or Moho. The cause of the Moho is thought to be a change in rock composition from rocks containing plagioclase feldspar (above) to rocks that contain no feldspars (below). The second event is a chemical discontinuity between ultramafic cumulates and tectonized harzburgites which has been observed from deep parts of the oceanic crust that have been obducted into the continental crust and preseved as ophiolite sequences.
Main Article: Life
Earth is the only place where life is known to exist. The planet's lifeforms are sometimes said to form a "biosphere". This biosphere is generally believed to have begun evolving about 3.5 billion (3.5×109) years ago. The biosphere is divided into a number of biomes, inhabited by broadly similar flora and fauna. On land, biomes are separated primarily by latitude. Terrestrial biomes lying within the Arctic and Antarctic Circles are relatively barren of plant and animal life, while most of the more populous biomes lie near the Equator.
Main article: Earth's atmosphere
Earth has a relatively thick atmosphere composed of 78% nitrogen, 21% oxygen, and 1% argon, plus traces of other gases including carbon dioxide and water vapor. The atmosphere acts as a buffer between Earth and the Sun. The Earth's atmospheric composition is unstable and is maintained by the biosphere. The layers, troposphere, stratosphere, mesosphere, thermosphere, and the exosphere, vary around the globe and in response to seasonal changes.
Main article: Ocean http://commons.wikimedia.org/upload/thumb/b/b8/250px-The_Earth_seen_from_Apollo_17.png Plate Carrée Projection of a composite satellite image of Earth
Earth is the only planet in our solar system whose surface has liquid water. Water covers 71% of Earth's surface (97% of it being sea water and 3% fresh water ) and divides it into five oceans and seven continents. Earth's solar orbit, vulcanism, gravity, greenhouse effect, magnetic field and oxygen-rich atmosphere seem to combine to make Earth a water planet.
Earth is actually beyond the outer edge of the orbits which would be warm enough to form liquid water. Without some form of a greenhouse effect, Earth's water would freeze. Paleontological evidence indicates that at one point after blue-green bacteria (Archaea) had colonized the oceans, the greenhouse effect failed, and Earth's oceans may have completely frozen over for 10 to 100 million years in what is called a snowball Earth event.
On other planets, such as Venus, gaseous water is destroyed (cracked) by solar ultraviolet radiation, and the hydrogen is ionized and blown away by the solar wind. This effect is slow, but inexorable. This is one hypothesis explaining why Venus has no water. Without hydrogen, the oxygen interacts with the surface and is bound up in solid minerals.
In the Earth's atmosphere, a tenuous layer of ozone within the stratosphere absorbs most of this energetic ultraviolet radiation high in the atmosphere, reducing the cracking effect. The magnetosphere also shields the ionosphere from direct scouring by the solar wind.
Finally, vulcanism continuously emits water vapor from the interior. Earth's plate tectonics recycle carbon and water as limestone rocks are subducted into the mantle and volcanically released as gaseous carbon dioxide and steam. It is estimated that the minerals in the mantle may contain as much as 10 times the water as in all of the current oceans, though most of this trapped water will never be released.
Earth in the Solar System Edit
It takes Earth 23 hours, 56 minutes and 4.09 seconds (1 sidereal day) to rotate around the axis connecting the North Pole and the South Pole. Thus from Earth the main apparent motion of celestial bodies in the sky (except meteors which are within the atmosphere and low orbiting satellites) is the movement to the west at a rate of 15 °/hr = 15'/min, i.e. a Sun or Moon diameter every two minutes.
Earth orbits the Sun every 365.2564 mean solar days (1 sidereal year). Thus from Earth this gives an apparent movement of the Sun with respect to the stars at a rate of ca. 1 °/day, i.e. a Sun or Moon diameter every 12 hours, in the direction opposite to that of the daily rotation of the sky.
The orbital speed is 30 km/s, which is one Earth diameter in 7 minutes, and one Moon distance in 4 hours.
Earth has one natural satellite, "the Moon", which orbits around Earth every 27 1/3 days. Thus from Earth this gives an apparent movement of the Moon with respect to the Sun and the stars at a rate of roughly 12 °/day, i.e. a Moon diameter every hour, in the direction opposite to that of the daily rotation of the sky.
Viewed from Earth's North Pole, the motion of Earth, its moon and their axial rotations are all counterclockwise.
The orbital and axial planes are not precisely aligned: Earth's axis is tilted some 23.5 degrees against the Earth-Sun plane (which causes the seasons), and the Earth-Moon plane is tilted about 5 degrees against the Earth-Sun plane (otherwise there would be an eclipse every month).
The Hill sphere (sphere of influence) of the earth is about 1.5 Gm (930 thousand miles) in radius, within which one natural satellite (the Moon) comfortably orbits.
Earth also suffers from the Chandler wobble.
The Moon Edit
Main article: Moon
|Name||Diameter (km)||Mass (kg)||Semi-major axis (km)||Orbital period|
|Luna||3,474.8||7.349 × 1022||384,400||27 Days, 7 hours, 43.7 minutes|
Luna, or simply 'the Moon', is a relatively large terrestrial planet-like satellite, about one quarter of Earth's diameter. The natural satellites orbiting other planets are called "moons", after Earth's Moon.
The gravitational attraction between the Earth and moon cause the tides on Earth. The same effect on the moon has lead to its tidal locking: its rotation period is the same as the time it takes to orbit the Earth. As a result it always presents the same face to the planet.
The Moon may enable life by moderating the weather. Paleontological evidence and computer simulations show that Earth's axial tilt is stabilised by tidal interactions with the Moon. Without this stabilization against the torques applied by the Sun and planets to the Earth's equatorial bulge, some theorists believe that the rotational axis might be chaotically unstable, as it appears to be with Mars. If Earth's axis of rotation were to approach the plane of the ecliptic, extremely severe weather could result as this would make seaonal differences extreme. One pole would be pointed directly toward the sun during summer and directly away during winter. Planetologists who have studied the effect claim that this might kill all large animal and higher plant life. This remains a controversial subject, however, and further studies of Mars —which shares Earth's rotation period and axial tilt, but not its large moon or liquid core— may provide additional information.
The Moon is just far enough away to have, when seen from Earth, the same apparent angular size as the Sun (the Sun is 400 times larger, but the Moon is 400 times closer). This allows a total eclipse to occur on Earth.
The Moon's origin is unknown, but one popular hypothesis that it was formed from the collision of a Mars-sized protoplanet with the early Earth. This hypothesis explains (among other things) the Moon's relative lack of iron and volatile elements. See Giant impact theory.
Main article: Geography
Biggest geographic subdivision
- total: 510.073 million km2
- land: 148.94 million km2
- water: 361.132 million km2
- note: 70.8% of the world's surface is covered by water, 29.2% is exposed land
Land boundaries: the land boundaries in the world total 251,480.24 km (not counting shared boundaries twice)
Coastline: 356,000 km
Maritime claims: see United Nations Convention on the Law of the Sea
- contiguous zone: 24 nautical miles (NM) claimed by most, but can vary
- continental shelf: 200 m depth claimed by most or to depth of exploitation; others claim 200 NM or to the edge of the continental margin
- exclusive fishing zone: 200 NM claimed by most, but can vary
- exclusive economic zone: 200 NM claimed by most, but can vary
- territorial sea: 12 NM claimed by most, but can vary
- Note: boundary situations with neighboring states prevent many countries from extending their fishing or economic zones to a full 200 NM; 43 nations and other areas that are landlocked include Afghanistan, Andorra, Armenia, Austria, Azerbaijan, Belarus, Bhutan, Bolivia, Botswana, Burkina Faso, Burundi, Central African Republic, Chad, Czech Republic, Ethiopia, Holy See (Vatican City), Hungary, Kazakhstan, Kyrgyzstan, Laos, Lesotho, Liechtenstein, Luxembourg, Malawi, Mali, Moldova, Mongolia, Nepal, Niger, Paraguay, Rwanda, San Marino, Slovakia, Swaziland, Switzerland, Tajikistan, The Republic of Macedonia, Turkmenistan, Uganda, Uzbekistan, West Bank, Zambia, Zimbabwe
Main article: Climate
Two large areas of polar climates separated by two rather narrow temperate zones from a wide equatorial band of tropical to subtropical climates. Precipitation patterns vary widely, ranging from several metres of water per year to less than a millimetre.
Elevation extremes: (measured relative to sea level)
- Lowest point on land: Dead Sea −408 m
- Lowest point overall: Mariana Trench in the Pacific Ocean −10,924 m
- Highest point: Mount Everest 8,850 m (1999 est.)
Natural resources Edit
Main article: Natural resources
- Earth's crust contains large deposits of fossil fuels: (coal, oil, natural gas, methane clathrate). These deposits are used by humans both for energy production and as feedstock for chemical production.
- Mineral ore bodies have been formed in Earth's crust by the action of erosion and plate tectonics. These ore bodies form concentrated sources for many metals and other useful elements.
- Earth's biosphere produces many useful biological products, including (but far from limited to) food, wood, pharmaceuticals, oxygen, and the recycling of many organic wastes. The land-based ecosystem depends upon topsoil and fresh water, and the oceanic ecosystem depends upon dissolved nutrients washed down from the land.
Some of these resources, such as fossil fuels, are difficult to replenish on a short time scale, called non-renewable resources. The exploitation of non-renewable resources by human civilization has become a subject of significant controversy in modern environmentalism movements.
Land use Edit
- arable land: 10%
- permanent crops: 1%
- permanent pastures: 26%
- forests and woodland: 32%
- urban areas: 1.5%
- other: 30% (1993 est.)
Irrigated land: 2,481,250 km2 (1993 est.)
Natural hazards Edit
Large areas are subject to extreme weather such as (tropical cyclones), hurricanes,or typhoons that dominate life in those areas. Many places are subject to earthquakes, landslides, tsunamis, volcanic eruptions, tornadoes, sinkholes, floods, droughts, and other calamities and disasters.
Environment - current issues Edit
Large areas are subject to overpopulation, industrial disasters such as pollution of the air and water, acid rain and toxic substances, loss of vegetation (overgrazing, deforestation, desertification), loss of wildlife, species extinction, soil degradation, soil depletion, erosion, and introduction of invasive species.
Human population Edit
Two humans are in orbit around Earth on board the International Space Station, every six months they are exchanged.
During the exchange there are more, and sometimes others are also traveling briefly above the atmosphere. In total, about 400 people (astronauts, cosmonauts and taikonauts) have been outside Earth (in space) as of 2004. Most of them have reported a heightened understanding of its value and importance, reverence for human life and amazement at its beauty, not usually achieved by those living on the surface.
See also space colonization.
- 0-14 years: 1,818,803,078 (29.92%)
- male: 932,832,913 (15.35%)
- female: 885,970,165 (14.57%)
- 15-64 years: 3,840,881,326 (63.19%)
- male: 1,942,402,264 (31.95%)
- female: 1,898,479,062 (31.23%)
- 65 years and over: 419,090,130 (6.89%)
- male: 184,072,470 (3.03%)
- female: 235,017,660 (3.87%) (2000 est.)
Population growth rate: 1.3% (2000 est.)
Birth rate: 22 births/1,000 population (2000 est.)
Death rate: 9 deaths/1,000 population (2000 est.)
- at birth: 1.05 male(s)/female
- under 15 years: 1.05 male(s)/female
- 15-64 years: 1.02 male(s)/female
- 65 years and over: 0.78 male(s)/female
- total population: 1.01 male(s)/female (2000 est.)
Infant mortality rate: 54 deaths/1,000 live births (2000 est.)
Life expectancy at birth:
- total population: 64 years
- male: 62 years
- female: 65 years (2000 est.)
Total fertility rate: 2.8 children born/woman (2000 est.)
Administrative divisions: 267 nations, dependent areas, other, and miscellaneous entries
Descriptions of Earth Edit
Since Earth is rather large, it is not immediately obvious to the naked eye viewing from the surface that it is an oblate spheroid, bulging slightly at the equator and slightly flattened at the poles. In the past there were varying levels of belief in a flat Earth because of this. Prior to the introduction of space flight, this belief was countered with deductions based on observations of the secondary effects of the earth's shape and parallels drawn with the shape of other planets.
In science fiction the Earth is frequently the capital or a major administrative center of a hypothetical galactic government (especially when that galactic government is postulated to be human-dominated), often a representative federal republic, though empires and dictatorships are definitely not unseen. Notable are Star Trek and Babylon 5. However, in other science fiction, people from the future no longer remember what planet they originally came from (for example, Battlestar Galactica and The Foundation Series).
See also Edit
- Economy: world economy
- History: history of the world
- Legal system: international law
- Political List of countries
- Degree Confluence Project
- Equatorial bulge
- Earth in fiction
- Extraterrestrial life
- NASA's Earth fact sheet
- Discovering the Essential Universe (Second Edition) by Neil F. Comins (2001)
Template:Footer SolarSystemaf:Aarde ar:ارض ast:Tierra bg:Земя ca:Terra cs:Země cy:Daear da:Jorden de:Erde et:Maa (planeet) el:Γη es:Tierra eo:Tero eu:Lurra fr:Terre ko:지구 hi:पृथ्वी hr:Zemlja id:Bumi ia:Terra is:Jörðin it:Terra he:כדור הארץ la:Terra lv:Zeme jbo:Terdi hu:Föld ms:Bumi minnan:Tē-kiû nl:Aarde ja:地球 no:Jorden nds:Eer pl:Ziemia pt:Terra ro:Pământ ru:Земля (планета) simple:Earth sl:Zemlja sr:Земља su:Marcapada fi:Maa sv:Jorden uk:Земля (планета) zh:地球