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Day 1 Notes
Day 1 Notes

... The Greek philosopher Aristarchus (312-230 BC) Sun ...
Powerpoint Notes on Meteors, Asteroids and Comets
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... our atomosphere and burns up, producing a streak of light time lapse photo of meteor shower Meteorite – a meteor so large it does not completely burn up and strikes the surface. ...
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... planetesimals in its vicinity. The asteroid belt objects have their orbits “pumped up” into more and more eccentric orbits. Some were absorbed by Jupiter, and some got ejected from the Solar System. This process reduced the “feeding zone” of Mars. Perturbations also lead to higher velocity collision ...
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... Our solar system was formed more than 4.5 billion years ago. As the Sun burst into existence, the leftover material combined to form eight planets and numerous other planetary bodies: moons, asteroids, and comets. Closest to the Sun are the inner planets (terrestrial planets) and further away are th ...
Gravity in the Solar System Quiz
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... with no activity. Scientist believe that in order for the cloud to start becoming active a near by super nova might have exploded and sent a shock wave through the cloud, which triggered it to start collapsing on itself. Large masses in space have a natural spin. As a result of the cloud collapsing ...
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... 34. In terms of stars, explain the meaning of E = mc2. When hydrogen is fused into helium, some of the mass within the atoms is lost. This mass is transformed into huge amounts of energy, which the star emits as light, heat and other radiation. 35. What is meant by axial tilt? The angle at which the ...
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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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