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Earth's axis of rotation is tilted 2. Earth's surface is covered with water. The majority of Earth's polar regions are covered in ice, including the Antarctic ice sheet and the sea ice of the Arctic ice pack. Earth's interior remains active with a solid iron inner core, a liquid outer core that generates the Earth's magnetic field, and a convecting mantle that drives plate tectonics. Within the first billion years of Earth's history, life appeared in the oceans and began to affect the atmosphere and surface, leading to the proliferation of aerobic and anaerobic organisms. Some geological evidence indicates that life may have arisen as much as 4. Since then, the combination of Earth's distance from the Sun, physical properties, and geological history have allowed life to evolve and thrive. Over 9. 9% of all the species of life. Based in Austin, TX, the EarthSky team has a blast bringing you daily updates on your cosmos and world. We love your photos and welcome your news tips. What Does The 'Y2K' Hoax Have To Do With Understanding God's Timeline? You may remember that in the late '90s we were warned that the Year 2000 computer bug could be. Founded in 2002 by Nobel Laureate Carl Wieman, the PhET Interactive Simulations project at the University of Colorado Boulder creates free. The word 'planet' derives from the Ancient Greek Mother Nature Network is the world's leading source for environmental news, advice on sustainable living, conservation and social responsibility. Hi there, I'm a huge Radiolab fan, I've listened to your podcasts for quite a while. While I'm sure this isn't really the best way to show my support, I noticed that. EO Kids October 18, 2016. New magazine with stories just for kids. Find out where all of Earth's fresh water is and try some fun experiments. Download the first issue. Humanity has developed diverse societies and cultures; politically, the world is divided into about 2. Name and etymology. The modern English word Earth developed from a wide variety of Middle English forms. In its earliest appearances, eor. By early Modern English, many nouns were capitalized, and the earth became (and often remained) the Earth, particularly when referenced along with other heavenly bodies. More recently, the name is sometimes simply given as Earth, by analogy with the names of the other planets. Another convention capitalizes . It almost always appears in lowercase in colloquial expressions such as . The formation and evolution of Solar System bodies occurred along with the Sun. In theory, a solar nebula partitions a volume out of a molecular cloud by gravitational collapse, which begins to spin and flatten into a circumstellar disk, and then the planets grow out of that disk along with the Sun. A nebula contains gas, ice grains, and dust (including primordial nuclides). According to nebular theory, planetesimals formed by accretion, with the primordial Earth taking 1. Between approximately 4. The origin of the world's oceans was condensation augmented by water and ice delivered by asteroids, protoplanets, and comets. On time scales lasting hundreds of millions of years, the supercontinents have assembled and broken apart. Roughly 7. 01. 62. The continents later recombined to form Pannotia, 6. High- latitude regions have since undergone repeated cycles of glaciation and thaw, repeating about every 4. The last continental glaciation ended 1. A half billion years later, the last common ancestor of all life arose. The resultant molecular oxygen (O2) accumulated in the atmosphere and due to interaction with ultraviolet solar radiation, formed a protective ozone layer (O3) in the upper atmosphere. Aided by the absorption of harmful ultraviolet radiation by the ozone layer, life colonized Earth's surface. This hypothesis has been termed . Over the past 7. 01. The development of agriculture, and then civilization, led to humans having an influence on Earth and the nature and quantity of other life forms that continues today. Over the next 7. 01. From that point, the Earth is expected to be habitable for another 7. Models predict that the Sun will expand to roughly 1 AU (1. As a red giant, the Sun will lose roughly 3. Earth will move to an orbit 1. AU from the Sun when the star reaches its maximum radius. Most, if not all, remaining life will be destroyed by the Sun's increased luminosity (peaking at about 5,0. Shown are distances between surface relief and the geocentre. The South American Andes summits are visible as elevated areas. Data from the Earth. Due to rotation, the Earth is flattened along the geographic axis and bulging around the equator. Local topography deviates from this idealized spheroid, although on a global scale these deviations are small compared to Earth's radius: The maximum deviation of only 0. Mariana Trench (1. Mount Everest (8,8. It is composed mostly of iron (3. Due to mass segregation, the core region is estimated to be primarily composed of iron (8. The principal oxides are silica, alumina, iron oxides, lime, magnesia, potash, and soda. The silica functions principally as an acid, forming silicates, and all the most common minerals of igneous rocks are of this nature. The outer layer is a chemically distinct silicate solid crust, which is underlain by a highly viscous solid mantle. The crust is separated from the mantle by the Mohorovi. The thickness of the crust varies from about 7. The crust and the cold, rigid, top of the upper mantle are collectively known as the lithosphere, and it is of the lithosphere that the tectonic plates are composed. Beneath the lithosphere is the asthenosphere, a relatively low- viscosity layer on which the lithosphere rides. Important changes in crystal structure within the mantle occur at 4. Beneath the mantle, an extremely low viscosity liquid outer core lies above a solid inner core. At approximately 7. These plumes can produce hotspots and flood basalts. The final major mode of heat loss is through conduction through the lithosphere, the majority of which occurs under the oceans because the crust there is much thinner than that of the continents. These plates are rigid segments that move in relation to one another at one of three types of plate boundaries: convergent boundaries, at which two plates come together, divergent boundaries, at which two plates are pulled apart, and transform boundaries, in which two plates slide past one another laterally. Earthquakes, volcanic activity, mountain- building, and oceanic trench formation can occur along these plate boundaries. At the same time, the upwelling of mantle material at divergent boundaries creates mid- ocean ridges. The combination of these processes recycles the oceanic crust back into the mantle. Due to this recycling, most of the ocean floor is less than 7. The oldest oceanic crust is located in the Western Pacific and has an estimated age of 7. Other notable plates include the Arabian Plate, the Caribbean Plate, the Nazca Plate off the west coast of South America and the Scotia Plate in the southern Atlantic Ocean. The Australian Plate fused with the Indian Plate between 5. The fastest- moving plates are the oceanic plates, with the Cocos Plate advancing at a rate of 7. At the other extreme, the slowest- moving plate is the Eurasian Plate, progressing at a typical rate of 2. The remaining 2. 9. Tectonics and erosion, volcanic eruptions, flooding, weathering, glaciation, the growth of coral reefs, and meteorite impacts are among the processes that constantly reshape the Earth's surface over geological time. Less common is basalt, a denser volcanic rock that is the primary constituent of the ocean floors. Nearly 7. 5% of the continental surfaces are covered by sedimentary rocks, although they form about 5% of the crust. The most abundant silicate minerals on Earth's surface include quartz, feldspars, amphibole, mica, pyroxene and olivine. The mean height of land above sea level is 8. The total arable land is 1. Earth's hydrosphere consists chiefly of the oceans, but technically includes all water surfaces in the world, including inland seas, lakes, rivers, and underground waters down to a depth of 2,0. The deepest underwater location is Challenger Deep of the Mariana Trench in the Pacific Ocean with a depth of 1. The oceans cover an area of 7. Most fresh water, about 6. The height of the troposphere varies with latitude, ranging between 8 km at the poles to 1. Oxygenic photosynthesis evolved 7. The ozone layer blocks ultravioletsolar radiation, permitting life on land. Water vapor, carbon dioxide, methane, and ozone are the primary greenhouse gases in the atmosphere. Without this heat- retention effect, the average surface temperature would be . Three- quarters of the atmosphere's mass is contained within the first 1. This lowest layer is called the troposphere. Energy from the Sun heats this layer, and the surface below, causing expansion of the air. This lower- density air then rises and is replaced by cooler, higher- density air. The result is atmospheric circulation that drives the weather and climate through redistribution of thermal energy. When atmospheric conditions permit an uplift of warm, humid air, this water condenses and falls to the surface as precipitation. This water cycle is a vital mechanism for supporting life on land and is a primary factor in the erosion of surface features over geological periods. Precipitation patterns vary widely, ranging from several meters of water per year to less than a millimeter. Atmospheric circulation, topographic features, and temperature differences determine the average precipitation that falls in each region. At higher latitudes, the sunlight reaches the surface at lower angles, and it must pass through thicker columns of the atmosphere. As a result, the mean annual air temperature at sea level decreases by about 0. Ranging from the equator to the polar regions, these are the tropical (or equatorial), subtropical, temperate and polar climates. For example, the Scandinavian peninsula has more moderate climate than similarly northern latitudes of northern Canada. The wind enables this moderating effect. The windward side of a land mass experiences more moderation than the leeward side. In the Northern Hemisphere, the prevailing wind is west- to- east, and western coasts tend to be milder than eastern coasts. This is seen in Eastern North America and Western Europe, where rough continental climates appear on the east coast on parallels with mild climates on the other side of the ocean. The Earth is closest to the Sun (at perihelion) in January, which is summer in the Southern Hemisphere. It is furthest away (at aphelion) in July, which is summer in the Northern Hemisphere, and only 9. Sun falls on a given square area of land than at perihelion. Despite this, there are larger land masses in the Northern Hemisphere, which are easier to heat than the seas. Consequently, summers are 2. NASA image. Above the troposphere, the atmosphere is usually divided into the stratosphere, mesosphere, and thermosphere. Beyond these, the exosphere thins out into the magnetosphere, where the geomagnetic fields interact with the solar wind. This causes a slow but steady loss of the atmosphere into space. Because unfixed hydrogen has a low molecular mass, it can achieve escape velocity more readily, and it leaks into outer space at a greater rate than other gases. Photosynthesis provided a source of free oxygen, but the loss of reducing agents such as hydrogen is thought to have been a necessary precondition for the widespread accumulation of oxygen in the atmosphere. Instead, most of the hydrogen loss comes from the destruction of methane in the upper atmosphere. The field extends outwards from the core, through the mantle, and up to Earth's surface, where it is, approximately, a dipole. The poles of the dipole are located close to Earth's geographic poles. At the equator of the magnetic field, the magnetic- field strength at the surface is 3. This causes secular variation of the main field and field reversals at irregular intervals averaging a few times every million years. The most recent reversal occurred approximately 7. The solar wind flows from left to right. The extent of Earth's magnetic field in space defines the magnetosphere. Ions and electrons of the solar wind are deflected by the magnetosphere; solar wind pressure compresses the dayside of the magnetosphere, to about 1. Earth radii, and extends the nightside magnetosphere into a long tail. For bodies near the celestial equator, this is equivalent to an apparent diameter of the Sun or the Moon every two minutes; from Earth's surface, the apparent sizes of the Sun and the Moon are approximately the same. This gives an apparent movement of the Sun eastward with respect to the stars at a rate of about 1. Due to this motion, on average it takes 2. The orbital speed of Earth averages about 2. Earth's diameter, about 1. Moon, 3. 84,0. 00 km (2. When combined with the Earth. Viewed from the celestial north pole, the motion of Earth, the Moon, and their axial rotations are all counterclockwise. Viewed from a vantage point above the north poles of both the Sun and Earth, Earth orbits in a counterclockwise direction about the Sun. The orbital and axial planes are not precisely aligned: Earth's axis is tilted some 2. Earth. Without this tilt, there would be an eclipse every two weeks, alternating between lunar eclipses and solar eclipses. Objects must orbit the Earth within this radius, or they can become unbound by the gravitational perturbation of the Sun. Earth, along with the Solar System, is situated in the Milky Way and orbits about 2. It is about 2. 0 light- years above the galactic plane in the Orion Arm. Due to Earth's axial tilt, the amount of sunlight reaching any given point on the surface varies over the course of the year. This causes the seasonal change in climate, with summer in the Northern Hemisphere occurring when the Tropic of Cancer is facing the Sun, and winter taking place when the Tropic of Capricorn in the Southern Hemisphere faces the Sun. During the summer, the day lasts longer, and the Sun climbs higher in the sky. In winter, the climate becomes cooler and the days shorter. In northern temperate latitudes, the Sun rises north of true east during the summer solstice, and sets north of true west, reversing in the winter. The Sun rises south of true east in the summer for the southern temperate zone and sets south of true west. Above the Arctic Circle, an extreme case is reached where there is no daylight at all for part of the year, up to six months at the North Pole itself, a polar night. In the Southern Hemisphere, the situation is exactly reversed, with the South Pole oriented opposite the direction of the North Pole. Six months later, this pole will experience a midnight sun, a day of 2. South Pole. By astronomical convention, the four seasons can be determined by the solstices. In the Northern Hemisphere, winter solstice currently occurs around 2. December; summer solstice is near 2. June, spring equinox is around 2. March and autumnal equinox is about 2. September. In the Southern Hemisphere, the situation is reversed, with the summer and winter solstices exchanged and the spring and autumnal equinox dates swapped. Its axial tilt does undergo nutation; a slight, irregular motion with a main period of 1. Both of these motions are caused by the varying attraction of the Sun and the Moon on Earth's equatorial bulge. The poles also migrate a few meters across Earth's surface. This polar motion has multiple, cyclical components, which collectively are termed quasiperiodic motion. In addition to an annual component to this motion, there is a 1. Chandler wobble. Earth's rotational velocity also varies in a phenomenon known as length- of- day variation. These dates change over time due to precession and other orbital factors, which follow cyclical patterns known as Milankovitch cycles. Because the Southern Hemisphere is tilted toward the Sun at about the same time that Earth reaches the closest approach to the Sun, the Southern Hemisphere receives slightly more energy from the Sun than does the northern over the course of a year. This effect is much less significant than the total energy change due to the axial tilt, and most of the excess energy is absorbed by the higher proportion of water in the Southern Hemisphere. Earth provides liquid water. Earth's biosphere is thought to have begun evolving about 7. On land, biomes are separated primarily by differences in latitude, height above sea level and humidity. Terrestrial biomes lying within the Arctic or Antarctic Circles, at high altitudes or in extremely arid areas are relatively barren of plant and animal life; species diversity reaches a peak in humid lowlands at equatorial latitudes. Those termed non- renewable resources, such as fossil fuels, only renew over geological timescales. Large deposits of fossil fuels are obtained from Earth's crust, consisting of coal, petroleum, and natural gas. These deposits are used by humans both for energy production and as feedstock for chemical production. Mineral ore bodies have also been formed within the crust through a process of ore genesis, resulting from actions of magmatism, erosion, and plate tectonics. The land- based ecosystem depends upon topsoil and fresh water, and the oceanic ecosystem depends upon dissolved nutrients washed down from the land. From 1. 98. 0 to 2. This is predicted to produce changes such as the melting of glaciers and ice sheets, more extreme temperature ranges, significant changes in weather and a global rise in average sea levels. Surveying, the determination of locations and distances, and to a lesser extent navigation, the determination of position and direction, have developed alongside cartography and geography, providing and suitably quantifying the requisite information. Earth's human population reached approximately seven billion on 3. October 2. 01. 1. Human population density varies widely around the world, but a majority live in Asia. By 2. 02. 0, 6. 0% of the world's population is expected to be living in urban, rather than rural, areas. Half of that land area is desert (1. The northernmost permanent settlement in the world is Alert, on Ellesmere Island in Nunavut, Canada. When the consensus of the membership permits, it provides a mechanism for armed intervention. The station's crew, made up of six people, is usually replaced every six months. It is the largest moon in the Solar System relative to the size of its planet, although Charon is larger relative to the dwarf planet. Pluto. The natural satellites of other planets are also referred to as . The same effect on the Moon has led to its tidal locking: its rotation period is the same as the time it takes to orbit Earth. As a result, it always presents the same face to the planet. As the Moon orbits Earth, different parts of its face are illuminated by the Sun, leading to the lunar phases; the dark part of the face is separated from the light part by the solar terminator. The Moon's axis is located by Cassini's third law. Due to their tidal interaction, the Moon recedes from Earth at the rate of approximately 3. Over millions of years, these tiny modifications. Paleontological evidence and computer simulations show that Earth's axial tilt is stabilized by tidal interactions with the Moon. The angular size (or solid angle) of these two bodies match because, although the Sun's diameter is about 4. Moon's, it is also 4. This hypothesis explains (among other things) the Moon's relative lack of iron and volatile elements and the fact that its composition is nearly identical to that of Earth's crust. During these approaches, it can orbit Earth for brief periods of time. Earth is sometimes personified as a deity. In many cultures it is a mother goddess that is also the primary fertility deity. In the West, belief in a flat Earth. It was only during the 1. Earth's age was at least many millions of years. The quantities given are the values at the instant J2. The difference between Earth's perihelion and aphelion is 5 million kilometers.^ ab. As of July 5, 2. 01. United States Strategic Command tracked a total of 1. Retrieved 1. 0 October 2. Based on data from the Vector Map and Global Landcover datasets, extreme values for coverage of lakes and streams are 0. Earth's surface. The ice shields of Antarctica and Greenland are counted as land, even though much of the rock that supports them lies below sea level.^Particularly as the setting for human civilization and experience. Why should it use up the soil? Ond God gecygde . Me is geseald . See: Chorowicz, Jean (October 2. Journal of African Earth Sciences. Bibcode: 2. 00. 5JAf. ES. 4. 3. 3. 79. C. 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