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	<title>Earth Archives - Planet Facts</title>
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	<description>Fun and Interesting Information About the Nine Planets</description>
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	<title>Earth Archives - Planet Facts</title>
	<link>https://planetfacts.org/category/our-solar-system/earth/</link>
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	<item>
		<title>Regolith</title>
		<link>https://planetfacts.org/regolith/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Wed, 21 Sep 2011 11:02:43 +0000</pubDate>
				<category><![CDATA[Asteroid]]></category>
		<category><![CDATA[Earth]]></category>
		<category><![CDATA[Moon]]></category>
		<category><![CDATA[Planets]]></category>
		<category><![CDATA[Scientific Terms]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=1955</guid>

					<description><![CDATA[<p>A regolith is a collective term referring to the blanket of powdery materials that cover the surface of several celestial bodies such as the earth, moon, and asteroids among many others. This blanket has a powdery appearance and texture because it is composed of fine debris such as soil, shattered rock, dust, and other small [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/regolith/">Regolith</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
]]></description>
										<content:encoded><![CDATA[<p><a href="https://planetfacts.org/wp-content/uploads/2011/03/Regolith.jpg"><img fetchpriority="high" decoding="async" class="alignright size-full wp-image-1956" title="Regolith 400" src="https://planetfacts.org/wp-content/uploads/2011/03/Regolith-400.jpg" alt="" width="400" height="266" srcset="https://planetfacts.org/wp-content/uploads/2011/03/Regolith-400.jpg 400w, https://planetfacts.org/wp-content/uploads/2011/03/Regolith-400-300x199.jpg 300w" sizes="(max-width: 400px) 100vw, 400px" /></a>A <strong>regolith</strong> is a collective term referring to the blanket of powdery materials that cover the surface of several celestial bodies such as the earth, moon, and asteroids among many others. This blanket has a powdery appearance and texture because it is composed of fine debris such as soil, shattered rock, dust, and other small objects that tend to land on the surface of these celestial bodies. <span id="more-1955"></span></p>
<p>On earth, the regolith is typically called soil and is made from natural processes such as the weathering of rocks. The soil in this case is vital to the survival of the organisms residing in the planet because it is where plants grow and where human beings build. In the case of the moon however and other objects in outer space that have no known signs of life on them, the regolith serves no other known function except to reflect light from the surface. The regolith from these celestial bodies comes mostly from the debris left over from impacts with meteors or asteroids. Because most of these bodies do not have an atmosphere surrounding them, the impact is often very hard and even small meteorites can cause damage or leave debris.</p>
<p>The moon’s regolith in particular is called lunar regolith and was found to be around 20 meters only at its thickest portions. The composition is mainly rocks and minerals along with glass particles from impacts with asteroids. A famous photo of the lunar regolith was taken during the Apollo 11 mission and showcases the footprint of renowned astronaut Neil Armstrong.</p>
<p>The post <a href="https://planetfacts.org/regolith/">Regolith</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<item>
		<title>Prime Meridian</title>
		<link>https://planetfacts.org/prime-meridian/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Tue, 06 Sep 2011 05:30:53 +0000</pubDate>
				<category><![CDATA[Earth]]></category>
		<category><![CDATA[Measurements]]></category>
		<category><![CDATA[Scientific Terms]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=2073</guid>

					<description><![CDATA[<p>The prime meridian is considered as the middle point of earth. It is also commonly known as the Greenwich Meridian and is a component that forms the International Date Line, which then divides the Western and Eastern Hemispheres of the Earth. It is generally known as zero degrees longitude or vertical line of reference in [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/prime-meridian/">Prime Meridian</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
]]></description>
										<content:encoded><![CDATA[<p><a href="https://planetfacts.org/wp-content/uploads/2011/09/Prime-Meridian.jpg"><img decoding="async" src="https://planetfacts.org/wp-content/uploads/2011/09/Prime-Meridian-300x251.jpg" alt="" title="Prime Meridian" width="300" height="251" class="alignright size-medium wp-image-2479" srcset="https://planetfacts.org/wp-content/uploads/2011/09/Prime-Meridian-300x251.jpg 300w, https://planetfacts.org/wp-content/uploads/2011/09/Prime-Meridian.jpg 449w" sizes="(max-width: 300px) 100vw, 300px" /></a>The <strong>prime meridian</strong> is considered as the middle point of earth. It is also commonly known as the Greenwich Meridian and is a component that forms the International Date Line, which then divides the Western and Eastern Hemispheres of the Earth. <span id="more-2073"></span></p>
<p>It is generally known as zero degrees longitude or vertical line of reference in the world map. It was established through scientific intervention and conventions. Throughout time, the prime meridian has taken different places and exact locations. The established and modern prime meridian is now based in the royal observatory in Greenwich, a part of the legal territories of England, in the year 1884.</p>
<p>The modern and current zero degrees meridian, which is based on the Royal Observatory, in Greenwich, is the common referent point in navigation, either by air, or sea. It was chosen as the official prime meridian through the means of an international convention through the efforts of the then United States President Chester Arthur, with the help of 25 delegates from various nations. At those times, over two-thirds of the world has made Greenwich as the point of reference for the prime meridian. It was only the nation of France who abstained and did not vote for the said convention’s beliefs. Since then, France still used Paris as the point of navigation for more decades.</p>
<p>As additional information, the Royal Observatory, where the prime meridian is based on, was established by a certain Sir George Airy in the year 1851. It is now converted as a museum and at night, it beams a light northward through a laser, to mark the prime meridian.</p>
<p>The post <a href="https://planetfacts.org/prime-meridian/">Prime Meridian</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<title>Plasmasphere</title>
		<link>https://planetfacts.org/plasmasphere/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Sun, 28 Aug 2011 10:53:39 +0000</pubDate>
				<category><![CDATA[Atmosphere]]></category>
		<category><![CDATA[Earth]]></category>
		<category><![CDATA[Scientific Terms]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=2042</guid>

					<description><![CDATA[<p>The plasmasphere is that region of dense, cold plasma surrounding the Earth. It is a part of the plasma-containing magnetosphere and is located just outside the upper ionosphere, extending to about 8000 to 25,000 miles into space. This donut-shaped volt of energy around our planet is the result of a process jumpstarted by the Sun’s [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/plasmasphere/">Plasmasphere</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
]]></description>
										<content:encoded><![CDATA[<p><img decoding="async" src="https://planetfacts.org/wp-content/uploads/2011/04/Plasmasphere.jpg" alt="" title="Plasmasphere" width="350" height="253" class="alignright size-full wp-image-2043" srcset="https://planetfacts.org/wp-content/uploads/2011/04/Plasmasphere.jpg 350w, https://planetfacts.org/wp-content/uploads/2011/04/Plasmasphere-300x216.jpg 300w" sizes="(max-width: 350px) 100vw, 350px" />The <strong>plasmasphere</strong> is that region of dense, cold plasma surrounding the Earth. It is a part of the plasma-containing magnetosphere and is located just outside the upper ionosphere, extending to about 8000 to 25,000 miles into space. This donut-shaped volt of energy around our planet is the result of a process jumpstarted by the Sun’s ultraviolet light.<span id="more-2042"></span></p>
<p>The upper portion of the Earth’s atmosphere is ionized with electrons liberated by the ultraviolet light of the Sun from neutral atmospheric particles, resulting into a gas now known as plasma, which is composed of both positive and negatively charged particles. </p>
<p>The positively charged particles are known as ions, while the negatively charged ones are termed electrons. Electrons are very low in mass, but tend to have high levels of energy. For this reason, the Earth’s gravity soon loses hold on them and they begin to gradually escape, leaving the ions to form a growing net of positive electric charge in the ionosphere while forming their own region of negatively charged space right above it. This negatively charged space will then keep the wayward electrons from moving any further from the Earth’s atmosphere.</p>
<p>The electrons retain their energy, and eventually attract the remaining lighter ions of hydrogen, helium and oxygen to leave the ionosphere as well. These camaraderie of escaping particles will then build up until a balance is achieved wherein there is as much plasma that flows into the ionosphere as there is that flows without. This process of exchange between particles forms the colder region of plasma known as the plasmasphere.</p>
<p>The post <a href="https://planetfacts.org/plasmasphere/">Plasmasphere</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<title>Parallax</title>
		<link>https://planetfacts.org/parallax/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Tue, 23 Aug 2011 06:05:45 +0000</pubDate>
				<category><![CDATA[Distance]]></category>
		<category><![CDATA[Earth]]></category>
		<category><![CDATA[Measurements]]></category>
		<category><![CDATA[Moon]]></category>
		<category><![CDATA[Physics]]></category>
		<category><![CDATA[Scientific Terms]]></category>
		<category><![CDATA[Space Tools]]></category>
		<category><![CDATA[Stars]]></category>
		<category><![CDATA[Sun]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=2026</guid>

					<description><![CDATA[<p>The Sun, Moon, stars and other celestial objects are beyond the reach of any instrument that can be used by observers here on Earth. Measuring the distance of a celestial object from the Earth might seem to be complicated. But measuring the distance of these remote entities have been simplified by the concept of parallax. [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/parallax/">Parallax</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
]]></description>
										<content:encoded><![CDATA[<p><a href="https://planetfacts.org/wp-content/uploads/2011/04/Parallax.gif"><img loading="lazy" decoding="async" class="alignright size-full wp-image-2027" title="Parallax 400" src="https://planetfacts.org/wp-content/uploads/2011/04/Parallax-400.gif" alt="" width="400" height="204" srcset="https://planetfacts.org/wp-content/uploads/2011/04/Parallax-400.gif 400w, https://planetfacts.org/wp-content/uploads/2011/04/Parallax-400-300x153.gif 300w" sizes="auto, (max-width: 400px) 100vw, 400px" /></a>The Sun, Moon, stars and other celestial objects are beyond the reach of any instrument that can be used by observers here on Earth. Measuring the distance of a celestial object from the Earth might seem to be complicated. But measuring the distance of these remote entities have been simplified by the concept of <strong>parallax</strong>.<span id="more-2026"></span> This term is often used relating to optical instruments like binoculars and microscopes. Visualizing a parallax can be easily done by placing the thumb in one’s line of sight and view a distant object using one eye at a time. A distant object seems to shift location when the observer switches from one eye to another.</p>
<p>Parallax provides astronomers with a simple method of calculating the distance of many celestial objects. As the Earth revolves around the Sun, celestial objects seem to be located at different positions when observed month after month. When a star is observed during June and December, observers can make use of two different viewpoints or lines of sight to the star to measure the distance. These two lines of sight intersect at the star being observed, forming an angle and half of this angle is the parallax.  Typically, the distance is measured in parsecs by getting the inverse of the observed parallax measured in arc seconds.</p>
<p>There are different kinds of parallax, namely, stellar, solar, lunar, diurnal, and dynamic or moving cluster. It is important to keep in mind that parallax decreases with distance and can only be used to measure celestial objects at a maximum distance of 100 parsecs. The use of this concept in astronomy is extended with much precision through the use of the Hipparcos satellite.</p>
<p style="text-align: center;"><strong>Geometric Technique &#8211; Parallax</strong></p>
<p style="text-align: center;"><iframe loading="lazy" title="YouTube video player" width="600" height="400" src="http://www.youtube.com/embed/SqI67fkdiL8" frameborder="0" allowfullscreen></iframe></p>
<p>The post <a href="https://planetfacts.org/parallax/">Parallax</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<title>Obliquity</title>
		<link>https://planetfacts.org/obliquity/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Sun, 14 Aug 2011 19:32:48 +0000</pubDate>
				<category><![CDATA[Earth]]></category>
		<category><![CDATA[Phenomena]]></category>
		<category><![CDATA[Physics]]></category>
		<category><![CDATA[Planets]]></category>
		<category><![CDATA[Rotation]]></category>
		<category><![CDATA[Scientific Terms]]></category>
		<category><![CDATA[Space Tools]]></category>
		<category><![CDATA[Stars]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=1708</guid>

					<description><![CDATA[<p>There are many terms in astronomy, and there is no doubt about that. One of which is the concept of Obliquity, more commonly known as the axial tilt. The angle between a certain rotational axis of an object and the specific perpendicular line in regards to the object’s orbital plane is better known as its [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/obliquity/">Obliquity</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
]]></description>
										<content:encoded><![CDATA[<p><a href="https://planetfacts.org/wp-content/uploads/2011/03/Obliquity.jpg"><img loading="lazy" decoding="async" class="alignright size-full wp-image-1709" title="Obliquity 400" src="https://planetfacts.org/wp-content/uploads/2011/03/Obliquity-400.jpg" alt="" width="400" height="266" srcset="https://planetfacts.org/wp-content/uploads/2011/03/Obliquity-400.jpg 400w, https://planetfacts.org/wp-content/uploads/2011/03/Obliquity-400-300x199.jpg 300w" sizes="auto, (max-width: 400px) 100vw, 400px" /></a>There are many terms in astronomy, and there is no doubt about that. One of which is the concept of <strong>Obliquity</strong>, more commonly known as the axial tilt.</p>
<p>The angle between a certain rotational axis of an object and the specific perpendicular line in regards to the object’s orbital plane is better known as its obliquity.<span id="more-1708"></span> In the solar system, the axial tilt of the earth is known formally as the obliquity of the ecliptic, since the name of the planet’s orbital plane is called the ecliptic plane. In formulas, it is represented by the Greek Character “Ε” or <em>epsilon</em>.</p>
<p>Apart from this, a planet’s axial tilt causes the seasons like spring or winter. This is due to the change of orientation of a planet’s obliquity, though the actual angular degree of tilt does not change, and the rotation moves until it reaches 360 degrees or one complete revolution. Thus, specifying which season it is now.</p>
<p>The planet earth has an approximate axial tile of 23.4 degrees. The axis stays tilted in the direction pointing to the stars for the entire year. This implies that a certain hemisphere &#8212; or half of the earth is in the direction towards the sun, half a year or half an orbit later, the other half will be now in the sun’s direction. Also, the current hemisphere that is facing the sun tends to have longer hours of sunlight.</p>
<p>The post <a href="https://planetfacts.org/obliquity/">Obliquity</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<title>Extraterrestrial Life</title>
		<link>https://planetfacts.org/extraterrestrial-life/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Wed, 27 Jul 2011 18:19:54 +0000</pubDate>
				<category><![CDATA[Earth]]></category>
		<category><![CDATA[Extraterrestrial]]></category>
		<category><![CDATA[Mars]]></category>
		<category><![CDATA[Space Theory]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=1102</guid>

					<description><![CDATA[<p>All of us may have considered what if we aren?t the only intelligent form of life in the universe. What if, light years away, are living beings who think and act like us? Or maybe beings with way, way advanced technology, and are studying us from afar? Some people doubt the existence of extraterrestrial life, [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/extraterrestrial-life/">Extraterrestrial Life</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
]]></description>
										<content:encoded><![CDATA[<p><a href="https://planetfacts.org/wp-content/uploads/2011/03/Extraterrestrial-firworks.jpg"><img loading="lazy" decoding="async" class="alignright size-medium wp-image-1103" title="Extraterrestrial firworks 400" src="https://planetfacts.org/wp-content/uploads/2011/03/Extraterrestrial-firworks-400-300x199.jpg" alt="" width="300" height="199" srcset="https://planetfacts.org/wp-content/uploads/2011/03/Extraterrestrial-firworks-400-300x199.jpg 300w, https://planetfacts.org/wp-content/uploads/2011/03/Extraterrestrial-firworks-400.jpg 400w" sizes="auto, (max-width: 300px) 100vw, 300px" /></a>All of us may have considered what if we aren?t the only intelligent form of life in the universe. What if, light years away, are living beings who think and act like us? Or maybe beings with way, way advanced technology, and are studying us from afar? Some people doubt the existence of <strong>extraterrestrial life</strong>, but we also don?t have any evidence that life elsewhere in the universe do not exist.<span id="more-1102"></span></p>
<p>Are we really alone? According to the latest study, most people in the United States (more than 60% of the study) believe in extraterrestrial life. The universe is just too big for Earth to be the sole planet to support life. In fact, we can look to <figure id="attachment_2386" aria-describedby="caption-attachment-2386" style="width: 200px" class="wp-caption alignleft"><img loading="lazy" decoding="async" src="https://planetfacts.org/wp-content/uploads/2011/04/Martian_face_viking_cropped.jpg" alt="" title="Martian_face_viking_cropped" width="200" height="175" class="size-full wp-image-2386" /><figcaption id="caption-attachment-2386" class="wp-caption-text">Face on Mars?</figcaption></figure>Earth?s closest neighbor, Mars. There is enough evidence that life was present on Mars, maybe a billion years ago. Traces of water and proper setting for life have been found, so it may have possible supported life billions of years ago.</p>
<p>Astrobiology, a study of possible life outside Earth, is an authentic and formalized field of science. NASA has funded programs to find extraterrestrial life in the universe. So far, the science has still a lot to learn and discover, and we can only speculate for now.</p>
<p>The post <a href="https://planetfacts.org/extraterrestrial-life/">Extraterrestrial Life</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<title>Latitude</title>
		<link>https://planetfacts.org/latitude/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Tue, 28 Jun 2011 07:37:45 +0000</pubDate>
				<category><![CDATA[Earth]]></category>
		<category><![CDATA[Measurements]]></category>
		<category><![CDATA[Scientific Terms]]></category>
		<category><![CDATA[Space Tools]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=1364</guid>

					<description><![CDATA[<p>Two different numbers, namely the Latitude and the Longitude, usually characterize various locations on Earth. This helps people in determining specific locations on the map, and the respective distances between two points on the Earth. Visualize the Earth as a see through sphere. Looking through the Earth one may observe an equatorial plane, with a [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/latitude/">Latitude</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
]]></description>
										<content:encoded><![CDATA[<p><img loading="lazy" decoding="async" class="alignright size-full wp-image-1365" title="Latitude" src="https://planetfacts.org/wp-content/uploads/2011/03/Latitude.gif" alt="" width="400" height="313" srcset="https://planetfacts.org/wp-content/uploads/2011/03/Latitude.gif 400w, https://planetfacts.org/wp-content/uploads/2011/03/Latitude-300x234.gif 300w" sizes="auto, (max-width: 400px) 100vw, 400px" />Two different numbers, namely the <strong>Latitude</strong> and the Longitude, usually characterize various locations on Earth. This helps people in determining specific locations on the map, and the respective distances between two points on the Earth. <span id="more-1364"></span></p>
<p>Visualize the Earth as a see through sphere. Looking through the Earth one may observe an equatorial plane, with a middle point, or center of the sphere or Earth. In order to indicate the Latitude of any point on the top of the Earth, you can draw a line from the center of the sphere to the point of interest.</p>
<p>Thus, the angle of the point with respect to the equator is the Latitude. North of the equator, the latitude is positive, south of the equator, the latitude is negative. Thus, it is because of this angle, along with the longitude, that reading the map has become easier and more effective to use.</p>
<p>No longer are the days in which maps would roughly present distances based on mere perception, and not clear measurement. With the Longitude and Latitude, one will be able to specifically pinpoint with only slight error a certain point on Earth. This has been a helpful yet innovative tool over the years.</p>
<p>The post <a href="https://planetfacts.org/latitude/">Latitude</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<title>Tidal Force</title>
		<link>https://planetfacts.org/tidal-force/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Sun, 19 Jun 2011 23:57:25 +0000</pubDate>
				<category><![CDATA[Earth]]></category>
		<category><![CDATA[Gravity]]></category>
		<category><![CDATA[Moon]]></category>
		<category><![CDATA[Physics]]></category>
		<category><![CDATA[Planets]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=2296</guid>

					<description><![CDATA[<p>Tidal force is a secondary effect of gravitational force and its most common manifestation, at least on the planet Earth, are tides. Tidal force, by technical definition is the differential force of gravity which arises because the force exerted on one body by another is not constant across the diameter in that the side which [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/tidal-force/">Tidal Force</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
]]></description>
										<content:encoded><![CDATA[<p><img loading="lazy" decoding="async" class="size-full wp-image-2297 alignright" title="Tidal Force 2" src="https://planetfacts.org/wp-content/uploads/2011/04/Tidal-Force-2.jpg" alt="" width="400" height="191" srcset="https://planetfacts.org/wp-content/uploads/2011/04/Tidal-Force-2.jpg 405w, https://planetfacts.org/wp-content/uploads/2011/04/Tidal-Force-2-300x142.jpg 300w" sizes="auto, (max-width: 400px) 100vw, 400px" /><strong>Tidal force</strong> is a secondary effect of gravitational force and its most common manifestation, at least on the planet Earth, are tides. Tidal force, by technical definition is the differential force of gravity which arises because the force exerted on one body by another is not constant across the diameter in that the side which is the nearest to the second body is subject to more gravitational force compared to the side farther away.<span id="more-2296"></span></p>
<p>If a body is rigid or the complete opposite – flimsy, tidal forces can tear the body in half. However, the Earth is an elastic sphere and the tidal force from the moon, in a way, distorts its shape although the mass or volume is not affected at all. Bulges' indicate this change in shape &#8212; an indication of the changes in the ocean levels due to tides, specifically.</p>
<p>The moon pulls on the planet as a whole, although its effect on solid Earth is only minimal – a few centimeters. It has more effect on the atmosphere and the hydrosphere. The oceans get attracted to the moon, causing high tides. However, it is noticeable that the nearer oceans are pulled more than the father oceans located at the side facing away wherever the moon is.</p>
<p>Tidal force also has a more general usage in astronomy, referring to the phenomenon where a body is subject to the gravitational force of a second body, while being subject to the gravitational force of a third body simultaneously, as in the case of the moon being primarily influenced by the Earth's gravity (due to its proximity) while being affected by the sun's gravitational pull as well.</p>
<p>The post <a href="https://planetfacts.org/tidal-force/">Tidal Force</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<title>Volatiles</title>
		<link>https://planetfacts.org/volatiles/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Mon, 23 May 2011 00:58:40 +0000</pubDate>
				<category><![CDATA[Earth]]></category>
		<category><![CDATA[Elements]]></category>
		<category><![CDATA[Physics]]></category>
		<category><![CDATA[Planets]]></category>
		<category><![CDATA[Space Tools]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=2243</guid>

					<description><![CDATA[<p>Photo by: RJHall Creative Commons Volatiles are chemical elements and compounds that have small boiling points and are found or connected to the atmosphere and crust of both a moon and a planet. Elements such as hydrogen, nitrogen, carbon dioxide, ammonia, and methane are types of volatiles. Water is also a perfect example as well [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/volatiles/">Volatiles</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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										<content:encoded><![CDATA[<div class="imagebox"><a href="https://planetfacts.org/wp-content/uploads/2011/04/Volatiles.png"><img loading="lazy" decoding="async" src="https://planetfacts.org/wp-content/uploads/2011/04/Volatiles.png" alt="" title="Volatiles" width="300" height="278" class="alignright size-full wp-image-2244" srcset="https://planetfacts.org/wp-content/uploads/2011/04/Volatiles.png 551w, https://planetfacts.org/wp-content/uploads/2011/04/Volatiles-300x277.png 300w" sizes="auto, (max-width: 300px) 100vw, 300px" /></a><br />
Photo by: <a rel="nofollow" href="http://en.wikipedia.org/wiki/Volatiles">RJHall</a> <a rel="nofollow" href="http://creativecommons.org/licenses/by/2.0/deed.en">Creative Commons</a>
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<p><strong>Volatiles</strong> are chemical elements and compounds that have small boiling points and are found or connected to the atmosphere and crust of both a moon and a planet. Elements such as hydrogen, nitrogen, carbon dioxide, ammonia, and methane are types of volatiles. Water is also a perfect example as well as other compounds of hydrogen, oxygen, nitrogen, silver, carbon and sulfur dioxide. <span id="more-2243"></span></p>
<p>As one looks closely to the crust of both the moon and the earth, he will find these elements in huge extents. Those volatiles that have very low melting points are classified glasses such as helium and hydrogen. The volatiles that have more than 100k melting points are called asices. </p>
<p>The moon is said to have a minimum of volatiles because its crust has oxygen but small amounts of nitrogen, carbon and hydrogen. Scientists made a recent discovery when they studied the components of silver found in Earth rocks and meteorites. With their findings they were able to make a calculation regarding the creation of Earth. They found out that when the Earth was created, volatiles such as water and other major ones may have been present in its crust and atmosphere, therefore refuting the theory that it was comets that gave these volatiles. </p>
<p>On the other hand, elements that have high boiling points are called refractory elements and are composed of aluminum, titanium, calcium, uranium, and other elements not usually found on earth which include tungsten, thorium, gadolinium, europium and zirconium.</p>
<p>The post <a href="https://planetfacts.org/volatiles/">Volatiles</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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		<title>Terrestrial Planet</title>
		<link>https://planetfacts.org/terrestrial-planet/</link>
		
		<dc:creator><![CDATA[riztys]]></dc:creator>
		<pubDate>Sat, 07 May 2011 19:13:16 +0000</pubDate>
				<category><![CDATA[Earth]]></category>
		<category><![CDATA[Mars]]></category>
		<category><![CDATA[Mercury]]></category>
		<category><![CDATA[Planets]]></category>
		<category><![CDATA[Venus]]></category>
		<guid isPermaLink="false">http://planet-facts.com/?p=2300</guid>

					<description><![CDATA[<p>A terrestrial planet is a planet which has solid surfaces and is primarily composed of silicate racks and/or metals. There are 4 known terrestrial planets in our solar system – Mercury, Venus, Earth and Mars, which are all inner planets and one terrestrial dwarf planet, Ceres, located in the asteroid belt. These planets share similar [&#8230;]</p>
<p>The post <a href="https://planetfacts.org/terrestrial-planet/">Terrestrial Planet</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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										<content:encoded><![CDATA[<p><a href="https://planetfacts.org/wp-content/uploads/2011/04/Terrestrial-3.png"><img loading="lazy" decoding="async" src="https://planetfacts.org/wp-content/uploads/2011/04/Terrestrial-3.png" alt="" title="Terrestrial 3" width="350" height="143" class="alignright size-full wp-image-2301" srcset="https://planetfacts.org/wp-content/uploads/2011/04/Terrestrial-3.png 800w, https://planetfacts.org/wp-content/uploads/2011/04/Terrestrial-3-300x122.png 300w" sizes="auto, (max-width: 350px) 100vw, 350px" /></a>A <strong>terrestrial planet</strong> is a planet which has solid surfaces and is primarily composed of silicate racks and/or metals. There are <em>4 known terrestrial planets</em> in our solar system – <em>Mercury, Venus, Earth and Mars</em>, which are all inner planets and one terrestrial dwarf planet, Ceres, located in the asteroid belt. These planets share similar characteristics such as proximity to the soon, few or no moons, absence of planetary rings such as Saturn's, relatively weaker magnetic fields and closely spaced orbits. They are also relatively smaller compared to the &#8216;<em>gas giants' Jupiter, Saturn, Uranus and Neptune</em>, which are located beyond the asteroid belt or &#8220;outer planets&#8221;.</p>
<p>Terrestrial planets have similar structures – a core composed of heavy metals which is usually iron, solid surfaces of craters, canyons, mountains and volcanoes and secondary atmospheres (generated through volcanic activity and comet impacts), as opposed to the gas giants which has primary atmospheres (captured directly from the original nebula). Note that while the moon has similar structure, it doesn't have an iron core. <em>Plutoids</em> are also similar to terrestrial planets in that they have solid surfaces; but instead or rocky surfaces, they are composed of icy materials.</p>
<p><em>Mercury</em> is one dense planet composed of iron and nickel, with a very thin atmosphere. Venus has a thick atmosphere, mostly of carbon dioxide, which causes a greenhouse effect. Earth has the highest density among these planets with an atmosphere composed of elements that are conducive for human habitation and Mars has a rocky red surface and a thin atmosphere. Note that among these 4, only Earth and Mars has moons; Earth has one and Mars has two). Extra-solar terrestrial planets are the subject of much interest, as people naturally want to know of the existence of other planets that are habitable for humans, or for the theoretical extraterrestrial beings.</p>
<p>The post <a href="https://planetfacts.org/terrestrial-planet/">Terrestrial Planet</a> appeared first on <a href="https://planetfacts.org">Planet Facts</a>.</p>
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