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The Earth
View of Earth as seen from Apollo 17
The following material has been copied and edited from . It is hoped that the page will be progressively customised with more material pertaining to processes through geological time.


Earth (often referred to as the Earth, Terra, or Planet Earth) is the third in the in terms of distance from the , and the fifth largest. It is also the largest of its 's , making it the largest body in the solar system, and it is the only place in the known to support . Accepted scientific theory states that the Earth was formed around ago [1] and its largest natural satellite, the , was orbiting it shortly thereafter, around 4.53 billion years ago.

Since it formed, the Earth has changed through geological and biological processes that have hidden traces of the original conditions. The is divided into several that gradually migrate across the surface over geologic time spans. The interior of the planet remains active, with a thick layer of convecting yet solid and an iron core that generates a .

The outer layer of the Earth can be divided into several compartments: the (or sphere of water), the (or sphere of soils and rocks), and the (or sphere of the air), a (the totality of living organisms), and more recently and perhaps metaphorically a .

The Earth's conditions have been significantly altered by the presence of life forms, which create an ecological balance that modifies the surface conditions. About 71% of the surface is covered in salt-water oceans, and the remainder consists of continents and islands.

There is significant interaction between the Earth and its space environment. The relatively large moon provides ocean and has gradually modified the length of the planet's rotation period. A bombardment during the early history of the planet is believed to have played a role in the formation of the oceans. Later, impacts are understood to have caused significant changes to the surface environment. Changes in the orbit of the planet may also be responsible for the that have covered significant portions of the surface in glacial sheets.


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Upper Crust
Lower Crust
Upper Mantle Lithospheric Mantle
Deeper Upper Mantle
Lower Mantle
Outer Core
Inner Core
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where buy cialis

Main article:

Based on the available evidence, current scientists have been able to reconstruct detailed information about the planet's past. Earth is believed to have formed around 4.57 billion years ago out of the , along with the Sun and the other planets. Initially molten, the outer layer of the planet cooled when water began accumulating in the atmosphere when the planet was about half its current radius, resulting in the solid crust. The moon formed soon afterwards, possibly as the result of the impact with a Mars-sized object known as . Outgassing and activity produced the primordial atmosphere; condensing , augmented by ice delivered by , [2]. The highly energetic chemistry is believed to have produced a self-replicating molecule around 4 billion years ago, and half a billion years later, the lived [3]

The development of allowed the sun's energy to be harvested directly; the resultant accumulated in the atmosphere and gave rise to the . The incorporation of smaller cells within larger ones resulted in the called [4]. Cells within colonies became increasingly specialized, resulting in true multicellular organisms. Aided by the absorption of harmful by the ozone layer, life colonized the surface of Earth.

Over hundreds of millions of years, continents formed and broke up as the surface of Earth continually reshaped itself. The continents have migrated across the surface of the Earth, occasionally combining to form a . Roughly 750 million years ago (mya), the earliest known supercontinent , began to break apart. The continents later recombined to form , 600–540 mya, then finally , which broke apart 180 mya [5].

Since the 1960s, it has been hypothesized that severe action between , during the , covered much of the planet in a sheet of ice. This hypothesis has been termed "", and is of particular interest because it preceded the , when multicellular lifeforms began to proliferate [6].

Since the , about 535 mya, there were five [7]. The last occurred 65 mya, when a meteorite collision probably triggered the extinction of the (non-avian) and other large reptiles, but spared small animals such as , which then resembled shrews. Over the past 65 million years, mammalian life has diversified, and several mya, a small African ape gained the ability to stand upright. This enabled tool use and encouraged communication that provided the nutrition and stimulation needed for a larger . The development of agriculture, and then civilization, allowed humans to influence the Earth in a short timespan as no other life form had, affecting both the nature and quantity of other life forms, and the global climate.

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Main article:
Earth cutaway from core to exosphere. Partially to scale

The interior of the Earth, like that of the other , is divided into layers. The Earth has an outer solid , a highly viscous , a liquid that is much less viscous than the mantle, and a solid .

The geologic component layers of the Earth [8] are at the following depths below the surface:

Depth Layer
Kilometres Miles
0–60 0–37 (locally varies between 5 and 200 km)
0–35 0–22 ... (locally varies between 5 and 70 km)
35–60 22–37 ... Uppermost part of mantle
35–2890 22–1790
100–700 62–435 ...
2890–5100 1790–3160
5100–6378 3160–3954

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Main article:
A map pointing out the Earth's major plates.

According to plate tectonics theory currently accepted by the vast majority of scientists working in this area, the outermost part of the Earth's interior is made up of two layers: the comprising the , and the solidified uppermost part of the . Below the lithosphere lies the , which comprises the inner, viscous part of the mantle.

The lithosphere essentially floats on the asthenosphere. The lithosphere is broken up into what are called . These plates move in relation to one another at one of three types of plate boundaries: , , and . , , -building, and formation occur along plate boundaries.

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Main article:

The Earth's varies greatly from place to place. About 70% of the surface is covered by water, with much of the below sea level. If all of the land on Earth were spread evenly, then water would rise to an altitude of more than 2500 metres (approximately 8000 ft.). The remaining 30% not covered by water consists of , , , , etc.

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Main article:

The abundance of water on Earth is a unique feature that distinguishes the "" from others in the solar system. Approximately 70.8 percent of the Earth is covered by water and only 29.2 percent is terra firma.

The Earth's hydrosphere consists chiefly of the , but technically includes all water surfaces in the world, including inland seas, lakes, rivers, and underground waters. The average depth of the oceans is 3,794 m (12,447 ft), more than five times the average height of the continents. The mass of the oceans is approximately 1.35 × 10^18 tonnes, or about 1/4400 of the total mass of the Earth.


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Main article:

The Earth's atmosphere has no definite boundary, slowly becoming thinner and fading into outer space. Three-quarters of the atmosphere's mass is contained within the first 11 km of the planet's surface. This lowest layer is called the . Further up, the atmosphere is usually divided into the , , and . Beyond these, the thins out into the . An important part of the atmosphere for life on Earth is the .

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Main article:

The totality of life on Earth is sometimes said to form a "". This biosphere is generally believed to have begun about 3.5 billion (3.5 x 109) years ago. Earth is the only place in the universe officially recognized by the communities of Earth where life is absolutely known to exist, and some scientists believe that . It includes all living matter on the planet or that portion of the planet occupied by life. It reaches well into the other three spheres, although there are no permanent inhabitants of the atmosphere. Relative to the volume of the Earth, the biosphere is only the very thin surface layer which extends from 11,000 meters below sea level to 15,000 meters above.

The biosphere is divided into a number of , inhabited by broadly similar and . On land primarily and height above the sea level separates biomes. Terrestrial biomes lying within the , or in high altitudes are relatively barren of and life, while most of the more populous biomes lie near the .

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Main article:

The most prominent features of the Earth's climate are its two large polar regions, two narrow zones, and a wide equatorial region. patterns vary widely, ranging from several metres of water per year to less than a millimetre.

Ocean currents are important factors in determining climate, particularly the spectacular which distributes heat energy from the equatorial oceans to the polar regions.

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Main article:

The pedosphere is the outermost layer of the Earth that is composed of and subject to . It exists at the interface of the , , and .


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[1] G.B. Dalrymple, 1991, "The Age of the Earth", Stanford University Press, California, .

[2] A. Morbidelli et al, 2000, "", Meteoritics & Planetary Science, vol. 35, no. 6, pp. 1309–20.

[3] W. Ford Doolitte, "Uprooting the Tree of Life", Scientific American, Feb. 2000.

[4] L. V. Berkner, L. C. Marshall, 1965, "On the Origin and Rise of Oxygen Concentration in the Earth's Atmosphere", Journal of the Atmospheric Sciences, Vol. 22, No. 3, pp. 225–61.

[5] J.B. Murphy, R.D. Nance, "", American Scientist, vol. 92, pp. 324–33.

[6] J.L. Kirschvink, 1992, "Late Proterozoic Low-Latitude Global Glaciation: The Snowball Earth", The Proterozoic Biosphere, pp 51–52.

[7] D. Raup & J. Sepkoski, 1982, "Mass extinctions in the marine fossil record", Science, vol. 215, pp. 1501–03.

[8] T. H. Jordan, "", Proceedings National Academy of Science, 1979, Sept., 76(9): 4192–4200.</ref>


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This page incorporates material from which is available under the terms of the . Wikipedia url for material on this page:

adapted from the German Wikipedia Earth Sciences portal

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