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Earth had an extreme collision with a planet called Thea.


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The Earth was 10 million years old at the time of the conflict.


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The collision goes across Thea and Earth, creating new planets.


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That's the planet we live on.


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The researchers were dazzled by matching the moon soil found in the lunar expedition three times and the volcano found in Arizona, Hawaii.


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There is no difference in the oxygen isotopes of the two stones.


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In the words of Professor Edward Young, head of the research team, the moon's soil no longer found any difference in the oxygen isotope of Earth's soil.


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The planet called Thea was turning up then.


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Right at that time the push takes place and the world is created.


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11] The age of the oldest substances located inside the solar system is about 4.56 hundred million years.


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12] From today 4.54 hundred billion years ago [3] the primitive form on Earth was formed.


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In addition to the Sun, other cosmic objects of the solar system are formed and evolved.


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From a theoretical point of view, a solar nebula from a molecular cloud extracts some volume through gravitational collapse, which begins to rotate and flattened and formed in the astral wheel, and it is from this wheel that the sun and other planets originate.


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A nebula consists of gaseous matter, ice particles and cosmic dust (which also includes primitive nucleides).


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According to the nebula theory, ultra-tiny planets are formed through the process of fusion.


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Thus it took about 1 to 2 million years for the primitive earth to be formed.


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13] Research is currently underway on the formation of the moon and it is said that the moon formed approximately 4.53 billion years ago.


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[14] According to the data of a researched hypothesis, the moon is formed as a result of the accumulation of objects falling from Earth after the Earth hit with the Mars-sized object Thia.


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15] From this event, it is said that the mass of the planet Thea was about 10% of the mass of the Earth, [16] which struck the Earth in an angular way, [17] and some of its mass after injury even faded with the Earth.


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What struck countless asteroids in about 4.1 to 3.5 billion years, causing massive changes to the larger surface of the Moon, and the reason for this was the presence of the Earth.


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Geological history has arisen as a result of volcanic origin and outgassing (outgassing) of gases rich in water vapor to Earth's atmosphere and oceans.


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Earth's oceans have originated in the combination of concentrated water and ice coming from asteroids, tiny planets, and comets.


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[18] In the Faint Young Sun Paradox model, atmospheric “greenhouse gases” prevent ocean water from becoming ice when the newly formed sun had only 70% solar brightness higher than the current time.


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[19] 3.5 billion years ago Earth's magnetic field was formed, which protects the Earth's atmosphere from blowing away as a result of solar wind.


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20] Strong exudation of the earth has occurred when the molten outer part of the earth is cooled and hardened.


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In two models [21] it is explained by the fact that the land gradually came to the present state, [22] or at the beginning of the history of the Earth [23] changed rapidly [24] and subsequently gradually formed continental territories.


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25] [26] [27] Continents have formed a geological leaf as a result of constant heat loss inside the Earth.


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Geological time has lasted hundreds of million years, and at this time the continents have merged and broken apart.


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Rodinia, the oldest continent, began to break down about 75 million years ago.


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The continent was then reunited from 60 million years to 54 million years ago and later merged into Panotia, later in Panzia, to later collapse 18 million years ago.


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28] The current form of the ice age began around 4 million years ago and was concentrated in the Pleistocene period 30 million years ago.


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The height of the high-latitude regions continued to decline due to glaciers and ice throats from 40,000 to 100,000 years ago.


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The last continental glacier ended 10,000 years ago.


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[29] The Advent and Evolution of Life Life TimelineThis box: ViewTalk-4500———-4000———3500———3000——2500——2000——1500———1000———500——0—WaterSingle-celled LifePhotosynthesiseUkaryotesMulticellular Lifethropods MollusCsplantsDinesUKARYotesMulticellular Lifethropods AursmammalsFlowersBirdSprimates→Earth (−4540) →Early water← Early Life→Early Oxygen→Atmospheric Oxygen→Oxygen Crisis→Sexual Reproduction→EdiaCara Biota→Cambrian Explosion→Tetrapoda→Early APESP h a n e r o z o i c o i c p o t e r o t e r o z o r o t e r o z r c h e a nh a d e a nPongolahuroniancryogenanDeankarooquaternaryiceages (a million years ago) (chemical reactions led to the first molecule being discovered around 400 million years ago).


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Another 50 million years later, the finding of the last single ancestor of all living beings coincided.


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30] Solar energy directly facilitates the life and reproduction of organisms as a result of the evolution of photosynthesis.


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The resulting oxygen (O2) is integrated into the atmosphere and interacting with the sun's ultra-violet rays creates a protective ozone layer (O3) above the atmosphere to protect the Earth from it.


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31] The merger of tiny cells with large cells leads to the formation of complex cells called concentric.


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32] Multicellular organisms are formed if cells within the colony become more specialized.


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The absorption of harmful ultraviolet radiation on the ozone layer causes organisms to coalesce on the surface.


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33] The oldest living fossils ever found are sandstone microbial matte fossils dating back to 3.48 billion years ago found in Western Australia, [34] [35] [36] [37] [38] metasediment organic graphite from 3.7 billion years ago obtained in western Greenland, [39] organic obtained in Western Australia. Cylinders.


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40] [41] In neoproterozoic times from 75 to 58 million years ago, much of the Earth was believed to have been icy.


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This concept is called “snowball earth” and has special importance because it was then when complex multicellular organisms began to be formed, the Cambrian eruption took place.


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42] The Cambrian eruption followed by five other major types of explosions 535 million years ago.


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43] The most recent eruption is the Cretaceous-Tertiary extinction, organized 66 million years ago.


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At this time, dinosaurs that cannot fly under the influence of asteroids and other large reptiles continue to extinct, but small species of fauna, such as mammals, survive.


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Until 66 million years east, mammals varied in life, and another millions of years ago African monkey-like animals, such as Aurorin teugenesis, gained the ability to stand upright.


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44] The development of agriculture and later the development of civilization led to an increase in human influence on the environment and nature and come to the present state.


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45] The future of the Earth is closely related to the expected long-term future of the Earth to the Sun.


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In the next 1.1 billion years (1 billion years = 109 years), the brightness of sunlight could increase by another 10% and another 40% increase in the next 3.5 billion years.


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46] Rising temperatures on Earth's surface will accelerate the inorganic carbon cycle, resulting in a drastic drop in its concentration in the air for plants (C4 would be only 10ppm in photosynthesis) about 500 — 900 million years later (1 million years = 106 years).


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47] Because of botanism, there will be no oxygen in the atmosphere, and the animal world will become extinct.


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48] Over the next billion years, all water on the surface will dry up [49] and the average temperature around the globe will rise to around 70°C [48] (158°F).


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Since this period, it is expected that the Earth will remain habitable for the next 500 million years, [47] it is also possible for up to 2.3 billion years if there is no nitrogen in the atmosphere.


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50] Even if the sun is eternal and stable, 27% of the water contained in modern oceans will be lost at the groundwater level of the geo-interior, this is due to a decrease in the amount of vapor emitted from the rocks located within the ocean.


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51] Within 5 billion years, the size of the Sun will change and turn into a red giant or red monster.


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From different models it is estimated that the shape of the sun will increase by about 1 AU (15,000,000 kW). m), which is 250 times greater than its current range.


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[46] [52] The fate of the Earth is very well clear at this time.


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As a red monster, the sun will lose about 30% of its mass during this time.


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So, the tide-kiln Earth, in an orbit would orbit the Sun at a distance of about 1.7 AU, during this time the star becomes its highest circumference.


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Most of the surviving biodiversity, but not all, will die due to the increased brightness of the sun (the maximum limit of brightness will be 5,000 times higher than the current limit).


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46] The results of a simulation carried out in 2008 indicate that, due to no tide-kiln effect, the Earth's orbit will decrease at one time and the sun will drag it towards itself, resulting in the Earth entering the Sun's atmosphere and becoming vapor at one time.


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52] The shape of the Earth is very similar to an oblong sphere.


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As a result of rotation, it flattens along the geographical axis of the Earth and inflates it along the equator.


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54] The diameter of the Earth along the equator is 43 kilometres (27mi) large beneath the diameter of the pole from pole to pole.


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[55] So, the highest distance from the center of gravity of the Earth on the Earth's surface is the highest horn of the Chimbarazo volcano located on the equator.


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56] [57] [58] [59] The average diameter of the ideal-sized spheres is 12,742 kilometres (7,918mi).


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The value of the diameter in the local topography differs from the standard spherical diameter values, even if we consider the world around the world, the value of this deviation is only slightly compared to the radius of the Earth: the maximum deviation value is only 0.17%, found in the Mariana sector (which is 10,911 metres (35,797ft) from sea surface. Below), and on the other hand at Mount Everest (8,848 metres (29,029ft) which is elevated above sea surface) the deviation value is 0.14%.


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[n3] Geodesy reveals that the sea on Earth would take its actual size if there were no land and other senses such as waves and winds, and it is defined by geoid.


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More precisely, the amount of geoid will be equal to the gravitational value at the average sea level level.


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Chemical composition. Earth's mass is about 5.97 x 1024 kilograms (5,970 yatograms).


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The highest of all the ingredients it comprises are iron (32.1%), oxygen (30.1%), silicon (15.1%), magnesium (13.9%), sulfur (2.9%), nickel (1.8%), calcium (1.5%), and aluminum (1.4%), other than 1.2%. Among them is the presence of various other elements.


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As a result of the separation of mass, it is estimated that the center area of the Earth is mainly composed of iron (88.8%), accompanied by a small amount of nickel (5.8%), sulfur (4.5%), and in addition, the presence of other elements less than 1%.


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62] Typically, all of the elements in the rocks of the Earth's crust are of oxide type: but the important exception is the presence of chlorine, surfur, and fluorine, and usually in a rock they are less than 1% of the total volume.


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99% of the total crust is formed by 11 types of oxides, the main ingredients of which are silica, alumina, iron oxide, lime, magnesia (magnesium oxide), potash and soda.


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[61] [62] [63] Internal structure The internal structure of the Earth is divided into several layers like other multinational planets, the structure of the layers depends on their chemical and physical (rheological) characteristics.


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The outermost layer is a chemically distinct solid silicate crust, the bottom of which is a solid mantle or gurgled with greater viscosity.


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The crust is separated from the gurmundala by part of the Mohorovičić discontinuity (Mohorovičić discontinuity).


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The thickness of the crust varies from about 6 kilometers below the ocean and about 30-50 km in the continent.


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The crust and, together with it, the cold, firm upward gurgles are called the lithosphere and those parts of the lithosphere where the tectonic plates are in a compressed state.


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The next layer of the lithosphere is the asthenosphere, it has a lower viscosity than its upper layer, and located above it can move the lithosphere.


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410 keys from the surface. Mm. From 660 k.s. Mm. In depth significant changes in the crystal structure of the gurumandala are observed, here the transformation is found in an expanse of the region, which separates the upright gurmondala and the lower gurmundala.


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Beneath the gurdala, there is a liquid extraterrestrial of highly viscosity, which is located above a solid underlying terrain.


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64] The angular velocity of rotation of the Earth's inland may be slightly higher than that of the rest of the terrain, with an increase of 0.1—0.5° per year.


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[65] The magnitude of the innermost terrestrial circumference is five percent compared to the Earth's circumference.


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External formation. At the time of the origin of the Earth it was a hot gas ingot.


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From the heated state it is cooled and condensed.


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At this time, heavy ingredients are deposited towards its center and light ingredients are deposited in layers from bottom to top according to varying mass.


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One of all these layers of the earth is known as a collar.


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At the top is the equestrian layer.


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The upper part of the horsetail is called the crust.


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Do towards the bottom side of the crust. Mm. In growth, temperatures rise to 30 degrees Celsius.


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68] The upper part of the crust consists of external objects such as mountains, plateaus, plains, etc.


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The external structure of the Earth is equipped with varied landforms on the earth's surface.


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The main landforms of the Earth are not equal everywhere on the surface.


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There are many differences in shape, nature and structure.


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Somewhere on the surface there are high mountains, somewhere mountains, somewhere plateaus.


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Judging geographically, the entire landscape of the Earth can be divided into 3 parts.


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69] These are (1) Mountains (2) Plateau (3) Plains.


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The mountain is a rock stone with a wide and steep slope of at least 1000 meters above sea level.


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Usually 600 to 1000 m. The high, short, well-groomed rock stupa is called a hill.


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The height of the mountain can be up to several thousand meters above sea level.


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The mountain terrain is usually of a friendly nature, with a very steep slope and usually climbing.


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Some mountains, like Kilimanjaro in East Africa, lie disproportionately.


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Again, some mountains like the Himalayan Mountains cover a wide area with many different horns.


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69] The vast plains that play high from the mountain but with steep slopes high from the plains are called plateaus.


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The height of the plateau can range from a hundred meters to several thousand meters.


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The height of the largest plateau on Earth is 4,270 to 5,190 meters.


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69] A plain land with gentle slopes slightly elevated above sea level is called plain.


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Plains have been created as a result of erosion and storage action of various geospatial processes such as rivers, glaciers and air.


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Plains for gentle slope and low roughness are very useful for farming, living, road construction.


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So the most frequent settlements have been developed on the plains.


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69] Heat is the origin of the Earth's internal heat in combination with the remaining part of the heat caused by the planet's degradation (about 20%) and the heat resulting from radioactivity (80%).


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70] The most heat-producing isotopes on Earth are potassium-40, uranium-238 and thorium-232 [71]. Temperatures in the center of the Earth can reach 6,000°C (10,830°F) or higher, [72] and pressure can reach 360 giga Pascals.


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73] Since the main cause of most heat generation is radioactivity, scientists claim that at the beginning of Earth's history, before the half-life reduction of radioactive isotopes, Earth's heat generation capacity was even greater.


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About 3 billion years ago, heat was generated almost twice as much as the present time, resulting in the process of formation of volcanic convection and geological leafs accelerated, and at the same time some rare volcanic rocks such as comatite, which are rarely formed at present.


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70] [74] The average heat loss from Earth is 87 mW/m2, with a worldwide heat loss standard of 4.42 × 1013W.


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75] A portion of the thermal energy in the center is transported towards the crust by the gravitational thermal rock, that is, a type of convection method, the flow of heat to the top of the surface through high-temperature rocks.


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These thermal rocks can cause flooding of hotspots and volcanic rocks.


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76] Earth's heat is further emitted through the cracks of tectonic plates, in places where the middle-sea rig has risen upwards. [


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The latest means of heat loss is through the lithosphere in the transport system, and most of it is through the ocean surface since the thickness of the ocean crust is less than the continental crust.


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[77] The geological plates are solid rigid layers on the outer side of the Earth's structure, known as the lithosphere, are divided into several pieces, these are tectonic leaf or geotextile leaf.


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These sheets are solid segments that can move subject to one another, from a total of three types of leaf ranges, these leaf limits are: the exponential limit, in which case the two sheets move inversely towards each other, in this case the two sheets move inversely. Stays and variable limits, when two tectonic leaves move against each other in parallel.


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Earthquakes, eruptions, mountain formation, and oceanic sector formation occur as a result of the action of these three types of leaf range.


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79] The geospatial leaves move over the region of the asthenosphere, which is the harder but less viscous part of the upward girdle, which can circulate and move along with the leaves.


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80] With the transmission of geosynthetic plates from one place to another, subduction of the oceanic crust occurs under pressure on the front of the creatic leaves at the perpendicular boundary.


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At exactly the same time, the influx of the material of the gurman causes the formation of a mid-sea rig as a result of the action of the divergent


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The combination of these processes recycles the oceanic crust and sent it back to Gurumunda.


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As a result of this recycle, most of the oceanic crust are aged no more than 100 million years.


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The oldest oceanic crust is located in Western Pacific with an estimated age of 200 million years.


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81] [82] When compared where the oldest continental crust ages around 4030 million years.


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83] The seven major tectonic or geometric leaves are Pacific, North American, Eurasian, African, Antarctic, Indo-Australian, and South American.


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Some of the other major leafs are Arabian leaf, Caribbean leaf, Nazca leaf located on the western coast of South America and the Scotia leaf in the South Atlantic Ocean.


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Between 50 and 55 million years ago, the Australian leaf became firmly attached to the Indian leaf.


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The fastest moving leaf is the oceanic leaf, such as cocos leaf, with a speed of 75 ml/year [84] and the Pacific leaf, which runs at a speed of 52-69 ml/year.


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On the other hand, the slowest circulating leaf is the Eurasian leaf, its normal circulation velocity is 21 ml/year.


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[85] [86] Surface Right|Thumb |The present earth looks like this - if it does not contain water.


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(Click/or enlarge to see its “rotation” in 3D globe form.


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The total surface size of the Earth is about 510 million square keys. Mm. (or 197 million square miles).


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[87] Of which, 70.8%, [87] or 361.13 million square keys. Mm. (139.43 million square miles), is the bottom of the sea surface and this part covered by sea water.


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88] Beneath the sea surface is the most numerous terraces, mountains, volcanoes, [55] marine sectors, underwater canyons, marine plateaus, deep marine plains, and a world-wide mid-sea rig system.


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And the remaining 29.2% share or 148.94 class keys. Mm. The terrain that is not covered by water (or 57.51 million square miles) is modified from place to place and includes mountains, deserts, plains, plateaus and other landforms.


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Removal and sedimentation, various volcanic eruptions, flooding, soil meteorism, glacial erosion, reef growth and meteor infestation, etc., are all the functional processes through which the Earth's surface surface is constantly changing with the passage of geological time.


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89] [90] The continental crust was found in low-density material, volcanic rocks such as: granite and andesite.


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The least found is basalt, which is volcanic rock of greater density, is the main component of the formation of the oceanic crust.


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91] In the case of sedimentary rock formation, the silt is sequentially accumulated and pressurized at one time to another rock and then coagulated together.


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About 75% of the continental crust is covered by sedimentary rock, although it accounts for only 5% of the Earth's total crust.


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92] And the third type of rock found on Earth is metamorphic rock, formed by the conversion of volcanic rock and sedimentary rock under high pressure, high heat, or by the simultaneous action of both.


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Quartz, feldspar, amphibol, mica, pyroxine, and olivin are all silicate minerals found in the world.


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93] Commonly found carbonate minerals include both calcite (which is found in limestone) and dolomite.


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[94] The height of the earth's surface can vary to a minimum of −418 meters with the Dead Sea and the highest elevation can be 8,848 meters at the peak of the Himalayan Mountains.


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The average height of the Earth's surface above sea level is 840 meters.


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95] The pedosphere is the highest layer outside the continental surface of the Earth and issues related to the processes of soil and soil formation inherent in it.


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10.9% of the total land area is arable, 1.3% of which are permanent crops.


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96] [97] Approximately 40% of the earth's surface surface is used as vegetation and wasteland, while Aureka is known from the calculation of 1.3 x 106 kW. M.2 is herbaceous land and 3.4 x 106 keys. M.2 is the coastline.


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[98] The abundance of water on the surface of the aquarium Earth is the unique feature that distinguishes this “blue planet” from other planets in the solar world.


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The oceans included in the Earth's climate, but logically all the water on the Earth's surface includes the oceans, lakes, rivers, and even water at 2,000 meters below the ground.


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The deepest of the water lying below the surface is the Challenger Deep of the Mariana sector in the Pacific Ocean with a depth of 10,911.4 meters.


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[n7] [99] The estimated mass of the oceans is approximately 1.35×718 metric tons, roughly 1/4400 fractions of the Earth's total mass.


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The total surface area of the oceans is 3.618×108 km. The average depth is 3682 m, and the average depth is 3682 meters, as a result, it has a size of 1.332×79 kW. M.3.


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100] If the height of the surface of the Earth's oceans was equal everywhere as smooth spheres, then the depth of the Earth's oceans would have been 2.7 to 2.8 km. Mm. [ 101] [102] About 97.5% of the Earth's total water is saline; the remaining 2.5% is fresh water.


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Most of the freshwater, about 68.7%, is present in ice caps as well as glaciers.


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103] The average salinity of the Earth's oceans is about 35 grams of salt per kilogram of salted water (3.5% salt).


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[104] Much of this salt has been attached to water as a result of eruption events or emitted from cold volcanic rock.


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[105] The oceans are also a base of dissolved atmospheric gases, which are vital for sustaining various aquatic life.


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[106] Sea water has a significant impact on the world's climate, where it acts as a large thermal base.


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[107] Any change in the temperature distribution of the oceans could significantly alter the Earth's climate, for example El Niño.


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[108] Atmosphere is a lining of atmospheric gases that may have gathered around an object of sufficient mass.


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Due to the gravity of the object, this gasponge is bound around it.


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If the gravity of the object is high enough and the ambient temperature is low, this collar can last a long time.


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In the field of planets, different types of gases can be seen gathering.


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That is why the atmosphere of the planet is relatively dense and deep in general.


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The earth retains the mixed layer of various gases that surround the Earth by its force of gravity, called the Earth's atmosphere or atmosphere.


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This atmosphere protects the existence of organisms on Earth by absorbing ultraviolet rays coming from the sun.


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In addition, by retaining heat (in response to the greenhouse) keeps the surface evaporated and prevents a drop in night temperatures over the day.


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8.5 What. Mm. The altitude scaled atmosphere is applying average atmospheric pressure to the Earth's surface is 101.325 kilos of pascals.


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70] It is formed by 78% nitrogen and 21% oxygen, with little water vapor, carbon dioxide and other gaseous elements.


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The change in the height of the troposphere occurs with the change of latitude, the value of which can be 8 kW in the polar part. Mm. And 17 keys in the equator. Mr.


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However, some deviations in this quality occur due to weather and seasonal changes.


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109] The Earth's biosphere has significantly altered its atmosphere.


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The production of oxygen in the photosynthesis process developed 2.7 billion years ago, forming today's main nitrogen-oxygen atmosphere.


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31] As a result of this, the development of aerobic organisms is accelerated and, indirectly, it helps in the process of ozone layer formation, this is due to the subsequent change from atmospheric O2 to O3.


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The weight layer helps in the development of life on the ground, by blocking the ultraviolet rays of solar radiation.


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110] Other atmospheric activities that are urgent for life retention include the circulation of water vapor, the supply of superfluous gases, burning down before small meteorites hit the Earth's surface, and controlling the temperature.


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[111] The latest action is known as greenhouse reaction: Some gaseous molecules identified in the atmosphere absorb the heat energy radiated from the surface and then radiate inside the atmosphere, raising the average temperature of the atmosphere.


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Water vapor, carbon dioxide, methane, nitrous oxide, and weight are the main greenhaze gases in the atmosphere.


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Without this heat retention phenomenon, the average temperature on the surface would be -18°C, on the contrary, the current temperature is +15°C, [112] and if it were not in its present state, life would not have developed on Earth.


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113] In May 2017, a flickering of light was observed for a sudden transient of a million miles away from a satellite in orbit, later reportedly it happened by reflecting light from ice crystals contained in the atmosphere.


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[114] [115] Weather and climate The Earth's atmosphere has no precise boundaries, gradually becoming thinner and lighter, merging with outer space.


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The atmosphere has a mass of three-quarters of its total within the first 11km (6.8mi).


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The name of its lowest layer is the troposphere.


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Under the influence of heat from the sun, this layer and the ground surface beneath it are heated, resulting in the expansion of the air.


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This low density air rises upwards and occupies its place is cold, high-density air.


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The result is the creation of airflow, which takes place in different places the weather and climate by rearranging the temperature.


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116] The main airflow stream includes Ion Wind, between 30° and 60° along the mid-latitude of the western winds (westerlies), 30° below the equator.


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[117] Ocean currents are important regulators of climate determination, thermohaline flow (thermohaline circulation) which distributes heat energy from equatorial ocean regions to cold-polar regions.


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118] The water vapor that is generated by evaporation from the surface is carried out in different parts of the atmosphere following some arrangement.


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When the atmospheric environment allows hot, humid air to rise upwards, the water condenses and falls sharply towards the surface.


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[116] Most of the water is then pushed to the lower ground through the river canal and re-reaches the sea, or it accumulates in a lake.


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This water cycle is a very important process for sustaining life on land and is the key factor for landscaping of different formations on the surface during a geological period.


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The layout of precipitation falls varies widely, the dimensions of which can be from several meters per year to less than one millimeter.


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The difference in airflow, positional characteristics and temperature - determines the average amount of precipitation falling in a region.


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119] The amount of solar energy on the Earth's surface tends to decline as latitude values continue to rise.


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At high latitudes, sunlight reaches the surface of the lower corners, and it has to cross the thick layer of the atmosphere.


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As a result, the average annual air temperature drop from the sea plane at a latitude change per degree from the equator was about 0.4°C (0.7°F).


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120] The earth surface can be subdivided into certain axis lines where a fairly similar climate prevails.


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These climates that prevail from the equator to the polar region are the tropical climate (or equatorial), the subtropical climate (subtropical), the temperate climate and the climate of the polar regions of the Earth.


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121] This latitude has some drawbacks to the rule: the climate is regulated if there is a sea where nearby.


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For example, the Scandinavian Peninsula (Scandinavian Peninsula) is much more tolerable climate than in northern Canada, located in its homologous northern latitudes.


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Helps maintain a wind-tolerable environment.


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The airborne side of the land feels a much more tolerable state than its airflow direction.


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In the northern hemisphere of the Earth, winds flow from west to east, and the west bank tends to be softer than in the east bank.


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It can be seen in the east of North America and in Western Europe, on both sides of the sea as well as the gentle climate, while the friend's climate is seen on the other side towards its eastern shore.


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[122] In the southern hemisphere, winds flow from east to west, and the climate in the East Bank tends to be gentle.


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The distance from the sun to the earth varies.


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The Earth is closest to the Sun (in Anusurabindu) in January, which is summer in the southern hemisphere.


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The Earth is at the farthest distance from the sun (at the opposition) in July, which is summer in the northern hemisphere, and only 93.55% of the solar radiation from the sun falls compared to Antarabindu in any specific square area of the land.


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Despite this, the size of the land in the northern hemisphere is much larger, which becomes heated much easier than in the plains.


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Thus, summers tend to be 2.3°C (4°F) warmer in the Northern Hemisphere, even in conditions of a similar environment than in the southern hemisphere.


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123] The climate is much colder for land higher than sea level because there is a lower air density.


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The widely used Köppen climate classification (Köppen climate classification) is divided into five large categories (moist tropical, dry, humid mid-latitudes, continental and cold poles), which are subsequently further divided into several subdivisions.


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[117] In the KOPPAN system, monitoring on temperature and precipitation, providing values for different geographies.


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The highest air temperature on Earth was measured at 56.7°C (134.1°F) in Death Valley, in Furnesa Creek, California, in 1913.


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124] The lowest temperature ever measured directly on Earth was −89.2°C (−128.6°F) at Vostok Station in 1983.


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[125] But the lowest temperature measured using remote sensors on the satellite was −94.7°C (−138.5°F) in East Antarctica.


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126] This temperature record is the only few measurements that began to be taken in value from the beginning of the 20th century using modern equipment and, fortunately, it does not reveal the full level of Earth's temperature.


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The upper atmosphere. The upper atmosphere of the troposphere is usually divided into the stratosphere, mesosphere and thermosphere.


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[111] Each layer has different lapse rates, indicating the change in temperature with a change in height.


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Since then, the exosphere joins from light to magnetic atmosphere, where geomagnetic fields interact with the solar wind.


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127] The stratosphere contains the weight layer, that is, the material that protects the surface from being the hands of the sun's superfluous rays and, therefore, is of great importance for the earth animal world.


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The Karman line, thus, can be defined as 100 keys to the surface of the earth. Mm. Above, and this is the effective boundary line between Earth's atmosphere and space.


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128] Heat energy increases the kinetic energy inside some of the outer edges of the atmosphere, and at one point they are able to break down the Earth's gravitational energy into space.


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As a result of this incident, the atmosphere gradually but regularly lost in space.


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Since the molecular mass of free hydrogen is the lowest, it can be easily released extremely quickly, and it exits into outer space at a higher rate than other gases.


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129] The loss of hydrogen gas in space is one of the factors behind the change in Earth's atmosphere, and it occurs primarily from an oxidation reaction to its current degradation reaction.


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Photosynthesis causes oxygen, but it is assumed that elements emitted as a result of oxidation, such as hydrogen, are the main prerequisites behind the storage of oxygen at a massive rate in the atmosphere.


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130] Therefore, the fact of hydrogen being released from the atmosphere may have an impact on the motion-nature of the evolution that life has taken place on Earth.


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131] Most of the oxygen-rich atmosphere currently turns hydrogen into water, before it gets a chance to get rid of the atmosphere.


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Instead, most of the hydrogen lost is generated as a result of methane burned in the higher atmosphere.


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[132] Gravity field The gravitational force of the earth is the acceleration due to the mass of the object acting on one object with the earth.


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On the surface of the surface, the gravity acceleration is about 9.8m/s2 (32ft/s2).


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Due to differences in the topography, geology and deep geological formation of a place, there is a change in the quality of the earth's gravitational force in local and large areas, which is called gravitational disruption.


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[133] The magnetic field is generated by the main part of the Earth's magnetic field at its geocentre, in the process of dynamo, thermally and technically, changes in the kinetic energy generated by the convection system are transported into electromagnetic energy and magnetic energy.


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The magnetic field spreads from the geocentre to the outside of the Earth, penetrating the gorge, to the surface of the Earth, where it is roughly a dipole.


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The location of the poles of the dipole is close to the geographical pole of the Earth.


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Along the equator on the surface, the magnetic force of the magnetic field is 3.05 × 10-5 Tesla, while the global magnetic dipole moment is 7.91 × 1015 Tesla m3.


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[134] The magnetic force flowing from the geocentre to the convection system does not circulate around in an orderly manner; the position of the magnetic pole changes and periodically changes its alignment.


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This results in sacular changes in the original magnetic field and magnetic field reversal occurs within an irregular period of time, on average once every million years.


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The closest catastrophe occurred about 700,000 years ago.


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[135] [136] The magnetosphere is defined by the expansion of the Earth's magnetic field in space.


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The ions and electrons of the solar wind are interrupted by the Earth's magnetosphere; under the pressure of the solar wind, the length of the magnetosphere on the light side of day is compressed, approximately up to 10 times the radius of the Earth, and makes the magnetosphere in the dark direction extend lengthwise.


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[137] This is because the velocity of the solar wind is much higher than the velocity at which the waves move towards the solar wind, a supersonic heavy-hit mixes the magnetosphere towards daylight into the solar air.


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[138] The magnetosphere consists of inert particles; in this way, it is filled with low-energy particles that follow the lines of the magnetosphere as the Earth rotates; [139] [140] The ring current is defined. Thus, it is filled with medium-energy particles that The Earth's geomagnetic field flows in harmony with the field, but also dominates its flow path in spite of the magnetic field, [141] and Van Ellen. The radiation belt is formed by high-powered particles, whose motion is mainly of random type, but in no case its location in the magnetic chamber. Incorporated.


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137] [142] When magnetic storms and substorms occur, extracted particles emerge from the outer side of the magnetosphere, and especially from the magnetotile, which may be directed towards the ionosphere, where atmospheric impurities are agitated and infused, resulting in arora.


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[143] The annual and daily motion of the earth is called the rotational motion of the earth around its own axis.


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This motion takes place in a counterclockwise direction from west to east.


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The axis of the earth's daily motion intersects the surface in the North Pole and South Pole region.


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The period of rotation of the Earth subject to the sun — this is called the average solar day—is 86,400 seconds average solar time (86,400.0025 SI seconds).


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144] This is because Earth's solar days are slightly larger today than in the 19th century because of the Tidal deceleration, each day changing and getting bigger from 0 to 2 sim milliseconds.


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[145] [146] Periods of Earth's daily motion are calculated subject to stationary stars, which are referred to as the International Earth Rotation and Reference Sistem Service (I.E. E. R. S) is called its stellar day, which is 86,164.0989 seconds average solar day (UT1), or 23hr 56min 4.0989 seconds.


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147] [n8] The duration of the Earth's rotation subject to the average equinox period, was previously mistakenly prevalent as a sidereal day, with a value of 86,164.0905 seconds with an average solar time (UT1) (23h 56min 4.0905sec) as 1982.


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[147] As a result, the astral day is about 8.4 milliseconds shorter than the astral day.


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[148] I. E. R. Calculation of the value of the average solar day length by S. The I. Eck was found from 1623 to 2005 [149] and from 1962 to 2005.


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150] Except for meteorites and low orbital satellites of Earth's atmosphere, the apparent original motion of celestial bodies is observed in the west side of the Earth's sky with a speed rate of 15°/hr = 15'/min.


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Objects that are close to the celestial equator are equal to the apparent circumference of the sun or moon every two minutes; from the surface of the earth, the apparent sizes of the sun and the moon are approximately equal.


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151] [152] The annual speed that results in the Earth being smaller or larger day and night and changing seasons is called the annual motion of the Earth.


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The Earth orbits the Sun at an average distance of about 150millionkm (93millionmi) per 365.2564 average solar days consecutive, or in one solar year.


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This provides for an apparent value of the sun's advance in the east subject to other stars with a rate of about 1°/day, that is, the apparent circumference of the sun or moon every 12 hours.


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Due to this speed, it takes an average of 24 hours—on a solar day—to complete a full rotation of the Earth's axis, so that the sun can return to the meridian again.


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Earth's average orbital speed is 29.78km/s (107,200km/h; 66,600mph), which is fast enough, at this speed the distance equal to the Earth's circumference, about 12,742km (7,918mi), can be overcome in just seven minutes, and the distance from Earth to the Moon is 384,000km (239,000mi), can be overcome in about 3.5 hours. In a.m.


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70] The rotation of the Moon and the Earth follows the same bericenter, subject to the stars surrounding it every 27.32 days. [


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When calculating the joint common orbit of the Earth and the Moon around the Sun, this period is called lunar month, from one full moon to another full moon, which is 29.53 days.


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If b is calculated subject to the north pole, then the motion of the Earth, the motion of the moon, and their orbital inclination will be counterclockwise.


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If the sun or the top of the earth is seen from a convenient position, it would seem, the Earth is orbiting the sun in the opposite direction clockwise.


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The rotating floor and the axial floor are not perfectly aligned in a linear way: the Earth's axis is curved approximately 23.44 degrees along the perpendicular to the Earth-Sun circumference path (transverse), and the Earth-Moon floor is curved up to about ±5.1 degrees compared to the Earth-Sun floor.


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If this was not curved, then there would be an adoption every two weeks, either lunar eclipse or solar eclipse.


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70] [153] The radius of the impact of the gravitational force of the Hill Sphere, or Earth, is about 1.5million kilometres (930,000mi).


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[154] [n9] This is the maximum distance to which the gravitational impact of the Earth is stronger than the farther away sun and other planets.


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Every object within this radius is obliged to orbit the Earth, or they can be knocked out due to the force of gravity of the Sun.


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Earth, as well as the solar world, is positioned in the Milky Way Galaxy and orbiting from its centre across nearly 28,000 light years.


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Its location is about 20 light years above the galactic floor of the Orion arm.


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[155] Noise and seasonal changes in the orbit. The axial slope of the Earth is approximately 23.439 281°, [147] whose orbital axis, is all set towards the B-pole.


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Due to the fact that the axial slope or axis line of the Earth is tilted, the amount of sunlight that comes to a particular place does not remain the same throughout the year, its value varies.


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This results in seasonal changes in nature and climate, the beginning of summer in the northern hemisphere when the sun is looking directly towards the crotch line and the onset of winter in the same place as the sun is looking towards the capricorn line in the southern hemisphere.


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In summer, the days are much longer, and the sun is at the very top of the sky.


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In winter, on the other hand, the climate becomes colder and the days at this time are shorter.


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In the temperate latitudes of the north, the sun rises in the latitudine-point part of the summer to the right east of the north and sits on the right west side of the north, which is exactly the opposite of winter.


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The sun rises in the latitudine-point part of the summer in the south to the right east, in temperate latitudes of the south and sits on the right west side of the south.


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Above the Arctic Circle, an extreme condition stands where daylight does not reach some times of the year, only the North Pole has this condition around 6 months above, known as polar nights.


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In the southern hemisphere, this phenomenon during this time remains completely opposite, the position and diocese of the South Pole are in a completely opposite direction to the position of the North Pole.


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Six months later, this pole feels the midnight sun, where one is a day 24 hours long, the same time the opposite happens at the South Pole.


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From astronomical practice, four seasons can be calculated according to the infinite-point—this is the point from which the axial slope of the earth's axis line is to calculate how close the sun is or how far away from the sun—and according to the equator, when the direction of the axial slope and the direction of the sun are parallel.


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In the northern hemisphere, the winter solstice is currently on December 21; the summertime equinox is around June 21, the spring equinox is around March 20 and the hemant-time equinox is September 22 or 23.


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The opposite happens in the southern hemisphere, where the summer and winter equinox are shifted among themselves, and the days of the spring equinox and autumn equinox also change among themselves.


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[156] The values of the axial slope of the Earth have remained irreversible for a much longer period of time relative.


Question: How many types of methods are there in the world in total?

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On average, at 18.6 years, the axial slope of the Earth occurs, usually with very slight, irregular motion observed.


Question: How many types of methods are there in the world in total?

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[157] Also the direction of the Earth's axis (not the value of its angle) varies over time, with the circle of its auscultation ending in full once every 25,800 years; this aonymotion serves as the reason for the separation of the tropical year from the stellar year.


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Both of these speeds are created due to the different religious attractions of the sun and moon along the skyline of the Earth.


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Both of the poles can also be spaced a few meters across the surface area.


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This pole motion has several, periodic elements, which can be described together as coacypirodic motion.


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In addition to the annual component of this speed, the 14 month bike also has one more element known as the Chandler Uble.


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Small growths also occur day and night due to the annual motion of the Earth.


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[158] At present, the Earth is located in Mucosurbindu at around January 3rd, and in Apsurbindu around July 4th.


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These days vary over time due to various phenomena of auscultation and axial, following a pattern of cyclic known as the Milankovitch bicycle.


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Due to this variable distance of the Earth and the Sun, the solar energy reaching the Earth's surface increases by about 6.9% [n10] to the molecule.


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This is because the southern hemisphere tends to the sun just when it reaches the closest point to the Earth and the Sun, throughout the year the southern hemisphere of the Earth receives a little more heat than its northern hemisphere from the sun.


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The significance of this phenomenon is very insignificant in comparison with the increase in the total energy volume due to the axial slope of the Earth, and most of the extra energy consumes sea water contained in the southern hemisphere.


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159] Habitability on which the animal world can survive is said to be habitable, even if life does not occur on that planet.


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On Earth there is an abundance of water —which creates a soothing environment for the interconnection and assimilation of complex organic compounds, and at the same time provide the energy necessary for metabolic processes.


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160] The distance from the Earth to the Sun, as well as its axial centrifuge, orbital rotation speed, axial slope, geospatial history, tolerable atmosphere, and magnetism are all working together to maintain the current climate and environment on the surface.


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[161] The biosphere biosphere (English: Biosphere) is the sum of the entire ecosystems of the Earth.


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It can be called the area of life on Earth, a connected process (dissociated from the solar and cosmic radiation and heat inside the Earth) and largely autonomous.


Question: How many types of methods are there in the world in total?

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In other words, biosphere refers to the aggregate of air, land, water and living objects located on the outer layer of the Earth.


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The relationship of the biosphere with the existence of life itself.


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While the breadth of the biosphere is captured as high as 20 kilometers below the height of the Himalayas, most of the life can be seen in the marine depths below 500 metres from the height of the Himalayas.


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Biokul began to live here 4.1 billion years ago.


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The animal world on the planet builds a habitable ecosystem, sometimes all of this together is called a “biosphere.”


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It is believed that the formation of the Earth's biosphere began about 3.5 billion years ago.


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31] This biosphere is divided by several biomes, with a large number of similar plants and animals living in the same biome.


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On land, the biome can be divided mainly from the difference in latitudes, from altitude above sea level and from humidity.


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In the case of terrestrial bios in the Arctic region or Antartic circle, fauna and flora in higher latitudes or extremely arid areas do not exist or are overgrown regions; species diversity is most commonly seen in the humid lowlands of the equator.


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162] In July 2016, scientists conducted an audit on all living organisms on Earth identified 355 sets of genes as the Last Universal Common Encester.


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[163] Natural resources and land use people have used Earth's natural resources for various purposes.


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Among those that are considered unviable resources, such as fossil fuels, are only renewed in terms of geological time.


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The ghost is extracted a huge assortment of fossil fuels.


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Among them, coal, petroleum and natural gas are notable.


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These reserves are used by people not only in energy production, but also as raw materials for the production of chemical products.


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It has also formed mineral ore reserves in the crust through the ore creation process.


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These ores have been formed as a result of lava, erosion and leafy geological formation.


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165] These ore reserves are regarded as a concentrated source of many metals and other beneficial basic substances.


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Earth's biosphere produces a lot of biologic material for humans, including food, wood, medicines, oxygen, and various organic wastes to be recycled.


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Land-based ecosystems depend on the upstream of soil and on clean water, and marine ecosystems depend on nutrients mixed in it that reaches sea water washed from the land.


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[166] According to 1980 calculations, 5,053 megahectares (50.53 million k.h. The area of Earth's surface was forests and forests, 6,788 megahectares (67.88 million k.m.). The area was grassland and woodland, and 1,501 megahectares (15.01 million kW). 2) The area was a field of cultivation of foodstuffs.


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[167] The estimated amount of irrigated land in 1993 was 2,481,250 square kilometres (958,020 sqmi).


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[168] People build houses using building materials to live on land.


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Natural and environmental problems are seen in extreme weather such as tropical cyclones, hurricanes, or typhoons in one of the largest areas of the Earth's surface, which have a profound impact on living conditions in all those areas.


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From 1980 to 2000, an average of 11,800 people died each year in this type of incident.


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169] There are numerous places where earthquakes, landslides, tsunamis, eruptions, tornadoes, land dislocations, strong snowfalls, floods, droughts, wildfires and other climate change and natural disasters occur.


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Air and water pollution in various places are caused by human caused pollution, resulting in acid rain and toxic elements, deforestation due to deforestation (more livestock land, deforestation, desertification, destruction of animals, extinction of species, soil degradation, land destruction and erosion.


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There is a scientific consensus that global terrestrial warming is triggered by the reduction of carbon dioxide emissions emitted as a result of the industrialization of the human race.


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It is thought that this has resulted in climate change such as melting glaciers and ice levels, with more extreme temperature limits being seen, as well as significant changes in weather and increasing global average sea level height.


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[170] Human geography is a biography of the study and practice of cartography, map-making, and geography is the study of land, properties, dwelling and phenomena on Earth, at the same time it has historically evolved into a rule depicting the Earth.


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Surveying, Hall Position and Distance Measurement System, and Navigation is a well-developed measurement system through which position and direction can be measured, cartography and geography as well as providing necessary information and accurate diagnosis.


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As of October 31, 2011, the amount of human numbers on Earth has gone up to an estimated seven billion.


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[171] Prophecies indicate that by 2050, the world's population will amount to 9.2 billion.


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[172] It is believed that the largest population will grow in developing countries.


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The density of the human population is not equal everywhere in the world, but an overwhelming part lives on the Asian continent.


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By 2020, 60% of the world's people are expected to live in city areas, rather than rural areas.


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173] It is calculated that eight-one-half of the earth's surface is suitable for human habitation — since four parts of the Earth's surface are surrounded by the sea, only one part of it is land.


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Half of this land area covers deserts (14%), [174] high mountains (27%), [175] or other unsuitable bass areas.


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The permanent establishment on the highest north side of the world is Alerte, which is located on Ellesmere Island in Nunavut, Canada [176] (82°28′ north), the permanent establishment on the highest south side of the Earth is Amundsen- Scott South Pole Station, in Antarctica, just around the South Pole, (90°south).


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Independent sovereign countries claim to be almost all of the land on the planet with the exception of only a few parts, excluding parts of Antertica, a few volumes of land along the west bank of the Danube River, the undisclosed area “Bir Towil” along the border between Egypt and Sudan.


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As of 2015, there are 193 sovereign states on earth which are incorporated as a member country of the United Nations, there are also two observer states and 72 dependent territories and limited recognized states.


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[168] Never on earth created a single sovereign government that had a cut over the whole world, though or some nation-states fought for world domination and failed.


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177] The United Nations acts as a world-wide inter-state body, it has been established with the aim of intervening in disputes arising between countries, so that armed disputes do not occur.


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178] The UN mainly serves as a forum for international diplomacy and international law.


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If the Member States gives consent, it also takes action for armed intervention.


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179] The first man to orbit the Earth was Yuri Gagarin, on April 12, 1961.


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[180] As of 30July 2010, in total, about 487 people have traveled into space and Earth orbit, and, among them, Barr John walked on the ground of the Moon.


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[181] [182] In general, people currently stationed at the International Space Station are the only people stationed in space.


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The workforce of the station is composed of six people who are changed every six months.


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[183] The farthest distance humans have traveled from the world is 400,171 k.m. Mr., which was achieved in the Apollo 13 expedition in the 1970s.


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[184] The moon is a relatively large rocky natural satellite of about a quarter of the radius-prominent moon on Earth.


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Considering the size of the planet, it is the largest moon in the solar system; although Caron is relatively larger than its dwarf planet Pluto.


Question: How many types of methods are there in the world in total?

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The natural satellites of other planets, like the Earth, are also referred to as the “moon.”


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The moon is the only natural satellite on Earth and the fifth largest satellite in the solar world.


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The average distance from the center of the Earth to the center of the moon is 384,403 kilometers (238,857 miles) which is about 30 times the diameter of the Earth.


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The moon has a diameter of 3,474 kilometers (2,159 miles), which is slightly more than a quarter of Earth's diameter.


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That means, the volume of the moon is 50% of the Earth's volume.


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The gravity force on its surface is one-sixth of the gravity force on the surface of the earth.


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If someone weighs 120 pounds on the surface of the Earth, then the weight on the surface of the moon would be just 20 pounds.


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It completes a full rotation around the Earth every 27.3 days.


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Every 29.5 consecutive days, the same activity occurs again.


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This periodic rotation of the lunar column occurs due to periodic changes in the geometry of the Earth-Moon-Sun tantra.


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The gravitational attraction and centrifugal force generated by the rotation of the Earth and the Moon subject to a common axis known as Bericenter are largely responsible for the creation of tide-kilns on Earth.


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Due to the amount of energy that is absorbed to create tide-kilns, the voltage energy decreases in the orbit that the Earth-Moon has centered on the bericenter.


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Due to this, the distance between these two astrologers increases to 3.8 cm each year.


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As long as the influence of the moon on the Earth is completely mitigating, the moon will continue to move away and the moon's orbit will stabilize on the day the mitigation occurs.


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As a result of the action of the gravitational force of the Earth and the Moon, tide-kilns are formed on Earth.


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This analogous phenomenon produces the moon's tidal locking: the same amount of time it takes for the moon to rotate on its own axis is required for rotation to Earth's orbit.


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Thereby it has the same surface all the time towards the earth.


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During the rotation of the Moon's Earth, its different parts are illuminated by sunlight, resulting in the moonlight; the darkest part of it is separated from the illuminated part by the solar terminator.


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As a result of tide-kiln phenomena caused by the attraction action of the Earth and the Moon, the moon moves away from Earth at a rate of about 38 mm/year per year.


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Over the mimion years, this tiny change—and the increase in Earth day to 23 microseconds/year—has finally made a larger change.


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185] During the Devonian time, for example (about 410 million years ago) it took 400 days to complete a year, whereas each day was 21.8 hours.


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186] The moon has played a vital role in developing life, helping to achieve Earth's climate change.


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Data obtained from fossils and computer simulations suggest that the axial slope of the Earth remains unstable due to tide-kiln phenomena with the moon.


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[187] Some astronomers assume that, without the constant torque applied by other planets and the Sun along the Earth's equatorial slope, the Earth's axis of rotation would have been of a random and unstable nature, noticing chaotic changes every million years, which can be seen in the case of Mars.


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188] When viewed from the surface of the Earth, the Moon and the Sun look like spherical wheels of approximately the same size at an equal distance.


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The angular size (or cubic angle) of these two objects coincides because, although or the Sun is about 400 times larger than the Moon, at the same time the Sun is located 400 times farther from the Earth than the Moon.


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152] [152] This results in the adoption of the full and annular (ring-like) sun into the earth.


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The most accepted theory in practice about the formation of the Moon is the mass-effect theory, which states that it has formed as a result of a collision with a cosmic particle called 'thea' of equal shape to Mars.


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This doctrine explains (among other things) the relative lack of iron and volatile elements on the Moon, and its structure is almost identical to the nature of the earth's crust.


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[189] Asteroids and artificial satellites. Asteroids are objects composed mainly of rocks that rotate in the center of its star.


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In our solar system, asteroids are the most known objects of the class called Minor Planetoid.


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They are smaller than smaller planets such as Mercury.


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Most asteroids rotate the Sun in certain elliptical orbits from the asteroid belt located between Mars and Jupiter.


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The asteroids are thought to be the remains of the protoplanetary disc.


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It is said that the remnants of the embryos that were created during the initial period of the formation of the solar system in the region of the asteroid belt did not have the opportunity to coincide with the planet due to the gravitational axis divergence caused by Jupiter's obsession.


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And these remnants are the cause of the origin of the asteroid belt.


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Some asteroids also have moons.


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Earth has at least five co-orbital asteroids, including the asteroids “3753 Cruithne) and “2002 AA29” (2002 AA29).


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190] [191] A Trojan asteroid is rotating along the “2010 TK7” (2010 TK7) path to the independent cryconical bindi path in the Earth's orbit around the Sun.


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192] [193] Every twenty years the smallest near-Earth asteroid “2006 RH120” (2006 RH120) complicates the Earth-lunar system.


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During this process, it can make the earth rotate in a shorter period than the applicable time.


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[194] Artificial satellites are satellites invented in the scientific process launched into space.


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It is similar to the moon but the only difference is that the moon is derived from nature and artificial satellites created by humans.


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As of June 2016, there were 1,419 man-made functional artificial satellites in Earth's orbit.


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[195] There are also currently more than 16,000 volumes of disabled satellites and space waste, including Vanguard-1, the most ancient artificial satellite.


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[n 11] The largest artificial satellite on Earth is the International Space Center.


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Cultural and historical views. The ideal astronomical symbol of the Earth is a cross sign inside the circle,; [196] which denotes the four corners of the earth.


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Various doctrines about this planet are prevalent in human culture.


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The world is sometimes expressed as a person as God.


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In many cultures the earth is the deity, considered the primary god of childbearing, [197] and in the middle of the 20th century, Gaia theory compared the earth's environment and life to a single self-regulating organism leading to the sustainability of habitation.


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198] [199] [200] In the mythology caused by many religions, it is said that a supernatural god or godparents created the world.


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197] Scientific findings have resulted in some culturally altered human views regarding this planet.


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The concept of flat earth in the west [201] has changed to the concept of spherical earth; which was introduced by Pythagoras in the sixth century BC.


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202] In addition, before the 16th century, the Earth was believed to be the center of the universe in the geocentric model; later scientists first showed through theoretical analysis that it was a rotating object and comparable to other planets in the solar world.


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203] Analyzing the biblical genealogy of the Earth's age, James Usher, and a few other Christian scholars and clergymen, until the 19th century, Westerners assumed that the age of the Earth was several thousand years.


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Arriving in the 19th century, scientists realized that the age of the Earth is at least several million years.


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[204] In 1864, Lord Kelvin calculated using thermodynamics to show that the age of the Earth is between 20 million and 400 million years, which gave rise to controversy; but later in the late 19th century and early 20th centuries the reliable method of determining the age of the Earth was the discovery of radioactivity and radiometric dating. After it is proved that the age of the Earth is more than a billion years.


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[205] [206] Human perception of Earth is re-changed when people first saw Earth from orbit in the 20th century, and especially after seeing images taken on Apollo space missions.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

Malaysia Airlines Flight 370 (MH370/MAS70) is a regular passenger air flight that was lost from the sky on its way from Kuala Lumpur, Malaysia to Beijing, China.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

On March 8, 2014, a Malaysian Airlines-operated Boeing 777-200ER plane was displaced except hours of flying from Kuala Lumpur.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

The plane had a total of 239 passengers, including 12 staff and 227 passengers from 15 countries, most of whom are Chinese.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

As of March 24, it has not been traced or any debris has been discovered anywhere.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

However, searches have continued to be urgency in various ways.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

On March 16, investigators reported that the plane was likely to be hijacked.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

[1] On March 24, it was announced by the Malaysian government that (perhaps) the plane fell from the sky on the south side of the Indian Ocean, and none of its passengers survived.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

[2] Less than an hour after the plane took off, contacted Kuala Lumpur Airport's Air Traffic Control.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

The control room's contact with the aircraft was severed after entering Kamau's airspace in the south of Vietnam just an hour after flying.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

In the beginning, more than 12 countries collectively conducted searches for the missing aircraft across the Malacca Way and the South China Sea in a total area of 27,000 square nautical miles (93,000 square kilometers; 36,000 square miles).


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

3] [4] While searches were initially conducted dominating Vietnam, the chances of finding a plane in Vietnam decreased on March 11, and searchers began investigating whether the plane landed on land.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

Authorities on March 12 began searches in the Andaman Sea northwest of the Malacca Praneli.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

[5] [6] [7] [8] On March 13, the US official said that they hope to expand the flight path approved by the search work authorities to the Indian Ocean as well.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

That's because U.S. investigators believe the plane could turn west around the Malay Peninsula [9] [10] and they also said the plane could have flown into the sky for another 4/5 hours after it first disappeared from the radar.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

11] [12] On March 15, Malaysian Prime Minister Najib Razak announced a press conference, and he said, based on satellite and radar information, the plane had disconnected from the radar without anyone thought.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

'The plane changed direction and tried to move towards India, over Malaysia, 'he said.


Question: when did Malaysia Airlines Flight 370 get lost in the sky?

Malaysia Airlines Flight 370

Anyone staying inside the plane has eliminated the trunk.