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Meteorites
Meteorites

... viewing with their long tails visible with the naked eye. However, since they are composed primarily of ice and rock, fragments of comets do not reach the Earth’s surface intact. Asteroids are rocky or metallic bodies of sub-planetary size whose orbits are scattered throughout the solar system but m ...
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... The last of the Malawi junior school national curriculum lessons has been posted for entry onto the memory flash drive. The plan now is to complete by mid-March the whole of this curriculum. In order that we may put this project into some perspective for you, one appendix 1 is one of the actual 10,8 ...
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...  “Hot Jupiters” are seen orbiting close to their stars in extrasolar planetary systems.  Computer simulations show that the giant planets may not have formed where they exist now, but rather could have migrated to their positions due to gravitational influences. ...
The Sun
The Sun

... the sun can exist in its present stable state for 10 billion years. As the sun is already 4.5 billion years old, it is “middle-aged.” ...
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... Planets the Solar System’s Best Friend In our Solar System there are 8 planets Mercury. Venus, Earth, Mars, Jupiter, Uranus, and Neptune. Theses planets in some ways are very similar to the stars but in other way they might be more different then you might think. In our solar system we have planets ...
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... less than a second. Bits of rock or metal from asteroids may produce brighter, longer-lasting meteors. Rarely, a very bright meteor, called a fireball, lights up the sky for several seconds. An object with greater mass, perhaps 10 grams or more, may not be destroyed by Earth’s atmosphere. A meteorit ...
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... combined mass is slightly greater than the original nucleus B) a heavy nucleus breaks apart into a number of smaller nuclei whose combined mass are less than the original nucleus C) two or more nuclei fuse or stick together to form a heavier nucleus whose combined mass is slightly less than the orig ...
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... • Revolution and rotation of sun and planets are in pretty much the same direction because they all formed from the same rotating gas cloud. • Orbits of planets lie in a plane because the solar nebula collapsed in a disk and the planets formed in that disk. • Strange orbits/rotations of Venus, and U ...
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... If you are not here today due to Yom Kippur, there will be an opportunity to make up today’s quiz after class on Weds. An extra credit problem will be available on the course web site tonight or tomorrow morning. ...
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... 2. Mark (T/F) which of the following are correct variations of Newton’s three Laws of Motion: (1 point for each correct answer, -1 point for each incorrect answer) ___T___ For every action, there is an equal, but opposite reaction ___F___ The force on a body, times the body’s mass equals the acceler ...
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... construction process is mostly over, it is by no means complete. There are still many objects moving around the Solar System, some of which are on potential collision courses with the planets. In the outer reaches of the Solar System there are millions of lumps of rock, dust and ice up to a few kilo ...
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The Solar System Sections 16.1-16.8

... Formation of the Solar System • Began with a large, swirling volume of cold gases and dust – a rotating solar nebula • Contracted under the influence of its own gravity – into a flattened, rotating disk • Further contraction produced the protosun and eventually accreted the planets • As particles m ...
Planet Research Powerpoint
Planet Research Powerpoint

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Formation and evolution of the Solar System



The formation of the Solar System began 4.6 billion years ago with the gravitational collapse of a small part of a giant molecular cloud. Most of the collapsing mass collected in the center, forming the Sun, while the rest flattened into a protoplanetary disk out of which the planets, moons, asteroids, and other small Solar System bodies formed.This widely accepted model, known as the nebular hypothesis, was first developed in the 18th century by Emanuel Swedenborg, Immanuel Kant, and Pierre-Simon Laplace. Its subsequent development has interwoven a variety of scientific disciplines including astronomy, physics, geology, and planetary science. Since the dawn of the space age in the 1950s and the discovery of extrasolar planets in the 1990s, the model has been both challenged and refined to account for new observations.The Solar System has evolved considerably since its initial formation. Many moons have formed from circling discs of gas and dust around their parent planets, while other moons are thought to have formed independently and later been captured by their planets. Still others, such as the Moon, may be the result of giant collisions. Collisions between bodies have occurred continually up to the present day and have been central to the evolution of the Solar System. The positions of the planets often shifted due to gravitational interactions. This planetary migration is now thought to have been responsible for much of the Solar System's early evolution.In roughly 5 billion years, the Sun will cool and expand outward many times its current diameter (becoming a red giant), before casting off its outer layers as a planetary nebula and leaving behind a stellar remnant known as a white dwarf. In the far distant future, the gravity of passing stars will gradually reduce the Sun's retinue of planets. Some planets will be destroyed, others ejected into interstellar space. Ultimately, over the course of tens of billions of years, it is likely that the Sun will be left with none of the original bodies in orbit around it.
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