Did you know...
Earth (or
the Earth) is the third
planet from the
Sun, and the densest and fifth-largest of the eight planets in the
Solar System. It is also the largest of the Solar System's four
terrestrial planets. It is sometimes referred to as the
World, the Blue Planet, or by its Latin name,
Terra.
Home to millions of
species including
humans, Earth is currently the only place where
life is known to exist. The planet formed
4.54 billion years ago, and
life appeared on its surface within a billion years. Earth's
biosphere has significantly altered
the atmosphere and other
abiotic conditions on the planet, enabling the proliferation of
aerobic organisms as well as the formation of the
ozone layer which, together with
Earth's magnetic field, blocks harmful
solar radiation, permitting life on land. The
physical properties of the Earth, as well as its
geological history and orbit, have allowed life to persist during this period. The planet is expected to continue supporting life for at least another
500 million years.
Earth's
outer surface is divided into several rigid segments, or
tectonic plates, that migrate across the surface over periods of
many millions of years. About 71% of the surface is covered with salt water oceans, the remainder consisting of
continents and islands which together have many lakes and other sources of water contributing to the
hydrosphere. Liquid water, necessary for all known life, is not known to exist in
equilibrium on any other planet's surface. Earth's
poles are mostly covered with solid ice (
Antarctic ice sheet) or
sea ice (
Arctic ice cap).
The planet's interior remains active, with a thick layer of relatively solid
mantle, a liquid
outer core that generates a magnetic field, and a solid iron
inner core.
Earth interacts with other objects in space, especially the Sun and the
Moon. At present, Earth orbits the Sun once for every roughly 366.26 times it rotates about its axis, which is equal to 365.26
solar days, or one
sidereal year. The Earth's axis of rotation is
tilted 23.4° away from the
perpendicular to its
orbital plane, producing seasonal variations on the planet's surface with a period of one
tropical year (365.24 solar days). Earth's only known
natural satellite, the Moon, which began orbiting it about
4.53 billion years ago, provides ocean
tides, stabilizes the axial tilt and gradually slows the planet's rotation. Between approximately
3.8 billion and
4.1 billion years ago, numerous
asteroid impacts during the
Late Heavy Bombardment caused significant changes to the greater surface environment.
Both the
mineral resources of the planet, as well as the products of the biosphere, contribute resources that are used to support a global human population. These inhabitants are grouped into about 200 independent
sovereign states, which interact through diplomacy, travel, trade, and military action. Human cultures have developed many views of the planet, including personification as a deity, a belief in a
flat Earth or in
Earth as the center of the universe, and a modern perspective of the world as an
integrated environment that requires stewardship.
Scientists have been able to reconstruct detailed information about the planet's past. The earliest dated Solar System material was formed
4.5672 ± 0.0006 billion years ago, and by 4.54 billion years ago (within an uncertainty of 1%) the Earth and the other planets in the Solar System had formed out of the
solar nebula—a disk-shaped mass of dust and gas left over from the formation of the Sun. This assembly of the Earth through accretion was thus largely completed within 10–20 million years. Initially
molten, the outer layer of the planet Earth cooled to form a solid crust when water began accumulating in the atmosphere. The Moon formed shortly thereafter,
4.53 billion years ago.
The current consensus model for the formation of the Moon is the
giant impact hypothesis, in which the Moon was created when a Mars-sized object (sometimes called
Theia) with about 10% of the Earth's mass impacting the Earth in a glancing blow. In this model, some of this object's mass would have merged with the Earth and a portion would have been ejected into space, but enough material would have been sent into orbit to coalesce into the Moon.
Outgassing and
volcanic activity produced the primordial atmosphere of the Earth. Condensing
water vapor, augmented by ice and liquid water delivered by asteroids and the larger
proto-planets,
comets, and
trans-Neptunian objects produced the oceans. The newly formed Sun was only 70% of its present
luminosity, yet evidence shows that the early oceans remained liquid—a contradiction dubbed the
faint young Sun paradox. A combination of
greenhouse gases and higher levels of
solar activity served to raise the Earth's surface temperature, preventing the oceans from freezing over. By
3.5 billion years ago, the Earth's
magnetic field was established, which helped prevent the atmosphere from being stripped away by the
solar wind.
Two major models have been proposed for the rate of continental growth: steady growth to the present-day and rapid growth early in Earth history. Current research shows that the second option is most likely, with rapid initial growth of continental crust followed by a long-term steady continental area. On
time scales lasting hundreds of millions of years, the surface continually reshaped as continents formed and broke up. The continents migrated across the surface, occasionally combining to form a
supercontinent. Roughly
750 million years ago (
Ma), one of the earliest known supercontinents,
Rodinia, began to break apart. The continents later recombined to form
Pannotia, 600–540 Ma, then finally
Pangaea, which broke apart 180 Ma.
At present, Earth provides the only example of an environment that has given rise to the
evolution of life. Highly energetic chemistry is believed to have produced a self-replicating molecule around
4 billion years ago and half a billion years later the
last common ancestor of all life existed. The development of
photosynthesis allowed the Sun's energy to be harvested directly by life forms; the resultant oxygen accumulated in the atmosphere and formed a layer of
ozone (a form of
molecular oxygen [O
3]) in the upper atmosphere. The incorporation of smaller cells within larger ones resulted in the
development of complex cells called
eukaryotes. True multicellular organisms formed as cells within
colonies became increasingly specialized. Aided by the absorption of harmful
ultraviolet radiation by the
ozone layer, life colonized the surface of Earth.
Since the 1960s, it has been hypothesized that severe
glacial action between 750 and 580 Ma, during the
Neoproterozoic, covered much of the planet in a sheet of ice. This hypothesis has been termed "
Snowball Earth", and is of particular interest because it preceded the
Cambrian explosion, when multicellular life forms began to proliferate.
Following the Cambrian explosion, about 535 Ma, there have been five
major mass extinctions. The
most recent such event was 65 Ma, when an asteroid impact triggered the extinction of the (non-avian)
dinosaurs and other large reptiles, but spared some small animals such as
mammals, which then resembled
shrews. Over the past 65 million years, mammalian life has diversified, and several million years ago an African ape-like animal such as
Orrorin tugenensis gained the ability to stand upright. This enabled tool use and encouraged communication that provided the nutrition and stimulation needed for a larger brain, which allowed the evolution of the human race. The development of agriculture, and then civilization, allowed humans to influence the Earth in a short time span as no other life form had, affecting both the nature and quantity of other life forms.
The present pattern of
ice ages began about 40 Ma and then intensified during the
Pleistocene about 3 Ma. High-
latitude regions have since undergone repeated cycles of glaciation and thaw, repeating every 40–100,000 years. The last continental glaciation ended 10,000 years ago.
The future of the planet is closely tied to that of the Sun. As a result of the steady accumulation of helium at the Sun's core, the
star's total luminosity will slowly increase. The luminosity of the Sun will grow by 10% over the next 1.1
Gyr (1.1 billion years) and by 40% over the next 3.5 Gyr. Climate models indicate that the rise in radiation reaching the Earth is likely to have dire consequences, including the loss of the planet's oceans.
The Earth's increasing surface temperature will accelerate the
inorganic CO2 cycle, reducing its concentration to levels lethally low for plants (10
ppm for
C4 photosynthesis) in approximately
500 million to
900 million years. The lack of vegetation will result in the loss of oxygen in the atmosphere, so animal life will become extinct within several million more years. After another billion years all surface water will have disappeared and the mean global temperature will reach 70 °C (158 °F). The Earth is expected to be effectively habitable for about another
500 million years from that point, although this may be extended up to
2.3 billion years if the nitrogen is removed from the atmosphere. Even if the Sun were eternal and stable, the continued internal cooling of the Earth would result in a loss of much of its CO
2 due to reduced
volcanism, and 35% of the water in the oceans would descend to the
mantle due to reduced steam venting from mid-ocean ridges.
The Sun, as part of its
evolution, will become a
red giant in about 5 Gyr. Models predict that the Sun will expand out to about 250 times its present radius, roughly 1 AU (150,000,000 km). Earth's fate is less clear. As a red giant, the Sun will lose roughly 30% of its mass, so, without tidal effects, the Earth will move to an orbit 1.7 AU (250,000,000 km) from the Sun when the star reaches it maximum radius. The planet was therefore initially expected to escape envelopment by the expanded Sun's sparse outer atmosphere, though most, if not all, remaining life would have been destroyed by the Sun's increased luminosity (peaking at about 5000 times its present level). However, a 2008 simulation indicates that Earth's orbit will decay due to tidal effects and drag, causing it to enter the red giant Sun's atmosphere and be vaporized.