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Planets And Solar System Essay Research Paper

Planets And Solar System Essay, Research Paper


“A planet is a celestial body that revolves around a


central star and does not shine by its own light ” (Grolier,


1992). The only planetary system that is known to man is our


solar system. It is made up of nine planets which range in size


and make-up. The nine major planets in our solar system are


Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune and


Pluto. There are also many other minor planets which are also in


our solar system, but they are unimportant compared to the nine


major planets. In this paper I will discuss the planets and how


they are each unique.


Mercury which is the planet that is closest to the sun is


the first planet I will discuss. Mercury is the smallest of the


inner planets. It is speculated that the heat from the sun made


it impossible for the gases present to become part of the


planetary formation. The surface of Mercury is extremely hot.


It is approximately 470 degrees celsius on the surface and is


thought to be even hotter at the two ” hot spots.” These ” hot


spots ” are on opposite ends of the equator. It is the heat of


the surface that makes it impossible for Mercury to have any type


of atmosphere.


Mercury orbits the sun once every 88 days and has a true


rotation period of 58.6 days. ” It is the closest planet to the


sun and therefore orbits faster than any other planet ”


(Thompson/Turk, 542, 1993). It is said that Mercury rotates


three times for every two trips around the sun, so that during


Planets 3


every alternate perihelon passage the same face points directly


at the sun. ” Geologically, the most remarkable features of


Mercury are compressional cliffs or faults, just the sort of


wrinkles that might form in the crust if the interior of the


planet shrank slightly ” (Morrison, 74, 1993). It is speculated


that it was the solidification of Mercury’s metallic core that


caused this global shrinkage. Mercury is also ” . . . enriched


in metal or depleted of rock ” (Morrison, 74, 1993). It is also


believed that some of the inner core of Mercury is still in a


fluid state.


Scientists also believe that Mercury’s surface is made partially


of silicate rock. The best way to describe Mercury is, ” . . .


small, heavily cratered and airless ” (Morrison, 71, 1993).


Venus is the second closest planet to the sun and is said to


” . . . most closely resemble Earth in size, density, and


distance from the sun ” (Thompson/Turk, 542, 1993). Venus is


known to most scientists as the sister planet to the Earth. It


is called this because it closely resembles the Earth’s mass,


density and diameter. The only thing different is that Venus ”


is shrouded in thick clouds that completely hide the surface of


the planet ” (Grolier, 1992). The surface temperature is also


much warmer than that of Earth.


Venus completes one revolution around the sun in 224.7 days.


This makes the Venusian day equal to 117 earth days. It is


thought that this slow rotation may be the reason why Venus has


no magnetic field.


Planets 4


The atmosphere of Venus made up of 98% carbon dioxide and


2% Nitrogen. This atmosphere also has the presence of helium,


neon and argon. This is yet another thing which makes Venus


different from Earth.


The surface of Venus is quite a bit like that of the Earth.


The surface has volcanoes and smooth plains. ” Much of the


volcanic activity on Venus takes the form of Basaltic eruptions


that inundate large ares, much as the mare volcanism flooded the


impacted basins on the near side of the moon ” (Morrison, 93,


1993). One thing that differs from Earth is that there is no


water liquid on the Venusian surface.


Some of the scientific data that follows was taken out of


Cattermole’s book. The mean distance from the sun is 108.20 Km.


The equatorial diameter is 12,012 Km and the equatorial rotation


is 243 days. Finally the mass of Venus is 4.87*10^24


(Cattermole, 63, 1993). Venus, although different than Earth, is


still our sister planet.


Mars is the fourth furthest away from the sun and is


recognized by its reddish color. Mars is also very much like the


Earth. ” More than any other planet in the solar system, Mars


has characteristics that make it an Earth-like world “(Grolier,


1992).


One thing that is very similar to Earth is the rotation


period. Mars rotation period is only thirty seven minutes longer


than the Earth’s. This would explain why Mars has significant


seasonal changes just as Earth does. It is believed that the


Planets 5


difference between winter and summer on Mars is even greater than


on Earth.


Mars is extremely hard to understand due to the effect of


blurring that is caused by the two atmospheres of Mars.


Scientists do know, however, that Mars is relatively small and


that changes take place in the surface features when the seasons


change. It is also known that dust storms are prevalent and


leaves the surface of Mars covered by a red haze.


Mars has a very thin atmosphere which is composed of carbon


dioxide, nitrogen, argon, water vapor and oxygen. Mars also has


no magnetic field. ” Because the atmosphere of mars is so thin,


wind velocities up to seve

ral hundred Km per hour are required to


raise the dust particles during a dust storm, and these fast-


moving particles erode structures with a sand-blasting effect ”


(Grolier, 1992). Therefore, the surface is basically plain-like


and covered with large craters. There are also some areas where


the rock is ” jumbled.” The poles of Mars are iced over and the


temperature is about 160 – 170 degrees K. Mars also has its


share of volcanoes. Most of these volcanoes are shield


volcanoes. The surface is littered with winding channels that


resemble river channels that have dried up over time. Scientists


believe that water once existed and caused the formation of these


channels. It is said that, ” Mars remains the best candidate for


life in the solar system outside of the Earth,” and that is what


makes Mars so interesting to scientists.


Jupiter is the fifth planet and is the most massive of all


Planets 6


the planets in this solar system. ” Its mass represents more


than two-thirds of the total mass of all the planets, or 318


times the mass of the Earth. Jupiters density is quite low at


1.3 g/cubic cm.


The atmosphere of Jupiter contains water, ammonia, methane


and carbon. It is thought by scientists that there are three


cloud layers. The wind activity on Jupiter is quite fierce and


moves in jet streams parallel to the equator. The weather on


Jupiter is still very hard for scientists to understand. There


is not enough information to truly understand how the weather is


on this planet.


Jupiter is most known by the normal citizen by the rings it


has. These ” rings are very diffuse. The ring particles must


generally be about as big as the wavelength of light, that is,


only a few microns ” (Grolier, 1992). That is why these rings


are faint or diffuse. The rings are what Jupiter is known for.


Saturn is a planet which is also known for its rings and


when viewed has a yellow or grayish color. The color is from the


gaseous atmosphere and the dust particles in that atmosphere.


The atmosphere is mostly a clear hydrogen-helium atmosphere.


There are also traces of methane, phosphine, ethane, and


acetylene. This atmosphere is much different than that of the


Earth’s.


Saturn orbits the sun with a period of 29.4577 tropical


years. It is 1.427 billion Km away from the sun and is therefore


a cold planet. It has an equatorial diameter of 120,660 Km which


Planets 7


makes it the second largest planet in our solar system.


The next planet is Uranus. The main problem scientists have


with Uranus is that, “the lack of visible surface features means


that it is difficult to measure the rotation period of Uranus


“(Hunt/Moore, 388, 1983). Uranus has an equatorial diameter of


51,000 Km which is almost four times as much as Earth. The


atmosphere is mostly methane gas and therefore the planet has a


red tint or a blueish green color. Uranus also has rings but


unlike Saturn these rings have almost no small particles.


Scientists are not as concerned with this planet.


Neptune is the last of the gaseous planets in our solar


system. Its atmosphere is much like Uranus’s because it is


mostly helium and hydrogen. It also contains methane. Neptune


has a diameter of 49,500 Km and a mass 17.22 times that of the


Earth. It has an average density of 1.67 /cm^3 (Grolier, 1992).


Neptune also has rings like its other gaseous partners, but they


are very faint. Not a great deal is known about Neptune. It is


widely studied by scientists and that makes it an important


planet.


The final planet, which is also the smallest, and the


furthest away from the sun is Pluto. This planet is very hard to


see therefore not a lot is known about its physical


characteristics. Scientists do know that it has a thin methane


atmosphere. Little is known about this planet because it is so


far away from the Earth and the sun. Scientists are always


learning new things and more data will arise in the future.


Planets 8


As one can see the planets of most importance are the ones


closest to the sun and Earth. Little is known about the far off


planets therefore it is hard to give them full recognition. Much


is known about Mercury, Venus, Earth, Mars, Jupiter and Saturn.


The other three planets are not as well known as these six are.


Whether more planetary systems exist doesn’t really matter.


There are still plenty of things we don’t understand about our


own solar system. Scientists will have their work cut out for


them in the future. Each and every planet has distinct


differences and that helps show us how truly great God is. The


planets will never fully be understood and will always be a great


topic of discussion.


Planets 9


Works Sited


Cattermole, P. (1995). Earth and Other Planets. New York:


Oxford University Press.


Grolier Electronic Publishing, Inc. (1992).


Hunt, G. & Moore, P. (1983). Atlas of the Solar System.


Chicago: Rand Mc Nally & Company.


Morrison, D. (1993). Exploring Planetary Worlds. New


York: Scientific American Library.


Thompson, G. & Turk, J. (1993). Earth Science and the


Environment. New York: Saunders College Publishing & Harcourt


Brace College Publishers.

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