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Earth

<p ><img src="/38f289eb-5743-5ff0-90bb-25551f02595d.png"/><b>earth</b></p>

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<img src="/38f289eb-5743-5ff0-90bb-25551f02595d.png"/>earth</p>

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<b>Earth</b>&nbsp;(or&nbsp;<b>the Earth</b>) is the third&nbsp;<a href="http://en.wikipedia.org/wiki/Planet" title="Planet" >planet</a>&nbsp;from the&nbsp;<a href="http://en.wikipedia.org/wiki/Sun" title="Sun" >Sun</a>, and the&nbsp;<a href="http://en.wikipedia.org/wiki/Density" title="Density" >densest</a>&nbsp;and fifth-largest of the eight planets in the&nbsp;<a href="http://en.wikipedia.org/wiki/Solar_System" title="Solar System" >Solar System</a>. It is also the largest of the Solar System's four&nbsp;<a href="http://en.wikipedia.org/wiki/Terrestrial_planet" title="Terrestrial planet" >terrestrial planets</a>. It is sometimes referred to as the&nbsp;<a href="http://en.wikipedia.org/wiki/World" title="World" >world</a>, the Blue Planet,<sup id="cite_ref-blueplanet_25-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-blueplanet-25" >[21]</a></sup>&nbsp;or by its Latin name,<i><a href="http://en.wiktionary.org/wiki/Terra" class="extiw" title="wikt:Terra" >Terra</a></i>.<sup id="cite_ref-Terra_26-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-Terra-26" >[note 6]</a></sup>

Earth formed approximately&nbsp;<a href="http://en.wikipedia.org/wiki/Age_of_the_Earth" title="Age of the Earth" >4.54 billion years</a>&nbsp;ago by accretion from the&nbsp;<a href="http://en.wikipedia.org/wiki/Solar_nebula" title="Solar nebula" class="mw-redirect" >solar nebula</a>, and<a href="http://en.wikipedia.org/wiki/Abiogenesis" title="Abiogenesis" >life appeared</a>&nbsp;on its surface within one billion years.<sup id="cite_ref-age_earth1_27-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-age_earth1-27" >[22]</a></sup>&nbsp;The planet is home to millions of<a href="http://en.wikipedia.org/wiki/Species" title="Species" >species</a>, including&nbsp;<a href="http://en.wikipedia.org/wiki/Humans" title="Humans" class="mw-redirect" >humans</a>.<sup id="cite_ref-science_241_4872_1441_28-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-science_241_4872_1441-28" >[23]</a></sup>&nbsp;Earth's&nbsp;<a href="http://en.wikipedia.org/wiki/Biosphere" title="Biosphere" >biosphere</a>&nbsp;has significantly altered&nbsp;<a href="http://en.wikipedia.org/wiki/Earth%27s_atmosphere" title="Earth's atmosphere" class="mw-redirect" >the atmosphere</a>and other&nbsp;<a href="http://en.wikipedia.org/wiki/Abiotic" title="Abiotic" class="mw-redirect" >abiotic</a>&nbsp;conditions on the planet, enabling the proliferation of&nbsp;<a href="http://en.wikipedia.org/wiki/Aerobic_organism" title="Aerobic organism" >aerobic organisms</a>as well as the formation of the&nbsp;<a href="http://en.wikipedia.org/wiki/Ozone_layer" title="Ozone layer" >ozone layer</a>&nbsp;which, together with&nbsp;<a href="http://en.wikipedia.org/wiki/Earth%27s_magnetic_field" title="Earth's magnetic field" >Earth's magnetic field</a>, blocks harmful solar radiation, permitting life on land.<sup id="cite_ref-Harrison_2002_29-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-Harrison_2002-29" >[24]</a></sup>&nbsp;The&nbsp;<a href="http://en.wikipedia.org/wiki/Geophysics" title="Geophysics" >physical properties of the Earth</a>, as well as its&nbsp;<a href="http://en.wikipedia.org/wiki/Geological" title="Geological" class="mw-redirect" >geological</a>&nbsp;history and orbit, have allowed life to persist. The planet is expected to continue supporting life for another&nbsp;500 million&nbsp;to&nbsp;2.3 billion&nbsp;years.<sup id="cite_ref-britt2000_30-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-britt2000-30" >[25]</a></sup><sup id="cite_ref-carrington_31-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-carrington-31" >[26]</a></sup><sup id="cite_ref-pnas1_24_9576_32-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-pnas1_24_9576-32" >[27]</a></sup>

Earth's&nbsp;<a href="http://en.wikipedia.org/wiki/Crust(geology)" title="Crust (geology)" >crust</a>&nbsp;is divided into several rigid segments, or&nbsp;<a href="http://en.wikipedia.org/wiki/Tectonic_plate" title="Tectonic plate" class="mw-redirect" >tectonic plates</a>, that migrate across the surface over periods of&nbsp;<a href="http://en.wikipedia.org/wiki/Geologic_time_scale" title="Geologic time scale" >many millions of years</a>. About 71% of the surface is covered by salt water oceans, with the remainder consisting of continents and islands which together have many lakes and other sources of water that contribute to the&nbsp;<a href="http://en.wikipedia.org/wiki/Hydrosphere" title="Hydrosphere" >hydrosphere</a>. Earth's<a href="http://en.wikipedia.org/wiki/Geographical_pole" title="Geographical pole" >poles</a>&nbsp;are mostly covered with solid ice (<a href="http://en.wikipedia.org/wiki/Antarctic_ice_sheet" title="Antarctic ice sheet" >Antarctic ice sheet</a>) or&nbsp;<a href="http://en.wikipedia.org/wiki/Sea_ice" title="Sea ice" >sea ice</a>&nbsp;(<a href="http://en.wikipedia.org/wiki/Arctic_ice_cap" title="Arctic ice cap" class="mw-redirect" >Arctic ice cap</a>).&nbsp;<a href="http://en.wikipedia.org/wiki/Structure_of_the_Earth" title="Structure of the Earth" >The planet's interior</a>&nbsp;remains active, with a thick layer of relatively solid&nbsp;<a href="http://en.wikipedia.org/wiki/Mantle(geology)" title="Mantle (geology)" >mantle</a>, a liquid&nbsp;<a href="http://en.wikipedia.org/wiki/Outer_core" title="Outer core" >outer core</a>that generates a magnetic field, and a solid iron&nbsp;<a href="http://en.wikipedia.org/wiki/Inner_core" title="Inner core" >inner core</a>.

Earth interacts with other objects in space, especially the Sun and the&nbsp;<a href="http://en.wikipedia.org/wiki/Moon" title="Moon" >Moon</a>. At present, Earth orbits the Sun once every 366.26 times it rotates about its own axis, which is equal to 365.26&nbsp;<a href="http://en.wikipedia.org/wiki/Solar_day" title="Solar day" class="mw-redirect" >solar days</a>, or one&nbsp;<a href="http://en.wikipedia.org/wiki/Sidereal_year" title="Sidereal year" >sidereal year</a>.<sup id="cite_ref-sidereal_solar_33-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-sidereal_solar-33" >[note 7]</a></sup>&nbsp;The Earth's axis of rotation is&nbsp;<a href="http://en.wikipedia.org/wiki/Axial_tilt" title="Axial tilt" >tilted</a>&nbsp;23.4° away from the&nbsp;<a href="http://en.wikipedia.org/wiki/Perpendicular" title="Perpendicular" >perpendicular</a>&nbsp;of its&nbsp;<a href="http://en.wikipedia.org/wiki/Orbital_plane_(astronomy)" title="Orbital plane (astronomy)" >orbital plane</a>, producing seasonal variations on the planet's surface with a period of one&nbsp;<a href="http://en.wikipedia.org/wiki/Tropical_year" title="Tropical year" >tropical year</a>&nbsp;(365.24 solar days).<sup id="cite_ref-yoder1995_34-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-yoder1995-34" >[28]</a></sup>&nbsp;Earth's only known<a href="http://en.wikipedia.org/wiki/Natural_satellite" title="Natural satellite" >natural satellite</a>, the Moon, which began orbiting it about&nbsp;4.53 billion&nbsp;years ago, provides ocean&nbsp;<a href="http://en.wikipedia.org/wiki/Tides" title="Tides" class="mw-redirect" >tides</a>, stabilizes the axial tilt, and gradually slows the planet's rotation. Between approximately&nbsp;3.8 billion&nbsp;and&nbsp;4.1 billion&nbsp;years ago, numerous&nbsp;<a href="http://en.wikipedia.org/wiki/Asteroid" title="Asteroid" >asteroid</a>&nbsp;impacts during the<a href="http://en.wikipedia.org/wiki/Late_Heavy_Bombardment" title="Late Heavy Bombardment" >Late Heavy Bombardment</a>&nbsp;caused significant changes to the greater surface environment.

Both the&nbsp;<a href="http://en.wikipedia.org/wiki/Mineral" title="Mineral" >mineral</a>&nbsp;resources of the planet and the products of the&nbsp;<a href="http://en.wikipedia.org/wiki/Biosphere" title="Biosphere" >biosphere</a>&nbsp;contribute resources that are used to support a&nbsp;<a href="http://en.wikipedia.org/wiki/World_population" title="World population" >global human population</a>.<sup id="cite_ref-World_Population_Clock_35-0" class="reference" ><a href="http://en.wikipedia.org/wiki/Earth#cite_note-World_Population_Clock-35" >[29]</a></sup>&nbsp;These inhabitants are grouped into about 200 independent&nbsp;<a href="http://en.wikipedia.org/wiki/Sovereign_state" title="Sovereign state" >sovereign states</a>&nbsp;(193 United Nations recognized sovereign states), which interact through diplomacy, travel, trade, and military action.&nbsp;<a href="http://en.wikipedia.org/wiki/Human_culture" title="Human culture" class="mw-redirect" >Human cultures</a>&nbsp;have developed many views of the planet, including&nbsp;<a href="http://en.wikipedia.org/wiki/Personification" title="Personification" class="mw-redirect" >personification</a>&nbsp;as a&nbsp;<a href="http://en.wikipedia.org/wiki/Deity" title="Deity" >deity</a>, a belief in a&nbsp;<a href="http://en.wikipedia.org/wiki/Flat_Earth" title="Flat Earth" >flat Earth</a>&nbsp;or in the&nbsp;<a href="http://en.wikipedia.org/wiki/Geocentric_model" title="Geocentric model" >Earth as the center of the universe</a>, and a modern perspective of the world as an&nbsp;<a href="http://en.wikipedia.org/wiki/Gaia_hypothesis" title="Gaia hypothesis" >integrated environment</a>&nbsp;that requires stewardship.</p>

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