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Inner Planets The inner four planets are called terrestrial planets
Inner Planets The inner four planets are called terrestrial planets

... has two moons Phobos and Deimos. Like our moon, the two moons keep the same side toward Mars as they revolve around the planet. They are small and appear to be captured asteroids. Mars has the largest volcanic mountain in the solar system, Mt. Olympus, which is 2.5 times the size of Mt. Everest. The ...
Instruction for making planet booklet
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... You should now have a booklet of the four rock planets, now you can start some research to complete the booklet. If you want to do the gas planets, unfold the booklet again and turn it around and refold so that Jupiter is on your front page. ...
Chapter 17 – Asteroids and Comets
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... thought that the Main Belt was the debris ring left over from a destroyed planet. But it’s much more likely that such a planet was, in fact, prevented from ever forming by Jupiter’s strong gravitational pull. There is no scientific explanation for Bode’s law, and it may well be a simple mathematical ...
Formation of the Solar System
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... Imagine an immense low-density cloud in the outer arms of our galaxy. This huge cloud of gas (mostly hydrogen with a little helium) and dust was originally so thin that it was virtually invisible. Millions of years passed, the cloud contracted, cooled and began to spin. Gravitational forces in this ...
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Astronomy 2: Exploring the Solar System

... Meteorite: A natural object originating in space that survives impact with Earth (or another body). Shooting/Falling Stars: What some people call meteors, but they are not stars, so this is a confusing term. Asteroid: Small, rocky objects in the inner solar system (primarily between Mars and Jupiter ...
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... As far as planets go, by far the frontrunner for life is our next-door neighbor, Mars. The red planet is the most Earthlike of solar system planets, with a comparatively similar size and temperature range as our own planet. Large bodies of water ice lie on Mars’ poles, and there’s a reasonable chanc ...
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... objects like it were not really planets at all because of their size and location in the solar system. The IAU decided that Pluto and objects like it should now be called dwarf planets. Astronomers continue to study the solar system. They use high-power, ground-based telescopes to discover new objec ...
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Chapter 9 - WordPress.com

... The sun rotates the same direction The planets rotate in the same direction Moons orbit in this direction Most planetary orbits are near circular 5. How does the nebular theory deal with exceptions? There are more leftover planetesimals than we see today. Most of them collided with the newly formed ...
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... 4. When a meteoroid enters Earth’s atmosphere, friction causes it to burn up and produce a streak of light called a(n) _______________ . 5. A chunk of ice and dust whose orbit is usually a long narrow ellipse is a(n) _______________. 6. If a meteoroid hits Earth’s surface, it is called a(n) ________ ...
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... lost volatiles (H2O, K, Cl, S etc.) during T-tauri phase and by subsequent evolution of parent body Accretion is fast, gas planets formed within few Ma, rocky ones a few 10 Ma. Lots of material exchange in Solar System, as planetary embryos destabilized by Jupiter. Primordial material does not remai ...
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... 4. When a meteoroid enters Earth’s atmosphere, friction causes it to burn up and produce a streak of light called a(n) _______________ . 5. A chunk of ice and dust whose orbit is usually a long narrow ellipse is a(n) _______________. 6. If a meteoroid hits Earth’s surface, it is called a(n) ________ ...
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Pocket Solar System - California Academy of Sciences
Pocket Solar System - California Academy of Sciences

... activity creates a simple model that more accurately illustrates the distances to planetary orbits relative to each other. One way to think about these concepts is to compare the relative distances of the other planets from the Sun to that of the Earth. Astronomers use the mean distance of the Earth ...
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Late Heavy Bombardment



The Late Heavy Bombardment (abbreviated LHB and also known as the lunar cataclysm) is a hypothetical event thought to have occurred approximately 4.1 to 3.8 billion years (Ga) ago, corresponding to the Neohadean and Eoarchean eras on Earth. During this interval, a disproportionately large number of asteroids apparently collided with the early terrestrial planets in the inner Solar System, including Mercury, Venus, Earth, and Mars. The LHB happened after the Earth and other rocky planets had formed and accreted most of their mass, but still quite early in Earth's history.Evidence for the LHB derives from lunar samples brought back by the Apollo astronauts. Isotopic dating of Moon rocks implies that most impact melts occurred in a rather narrow interval of time. Several hypotheses are now offered to explain the apparent spike in the flux of impactors (i.e. asteroids and comets) in the inner Solar System, but no consensus yet exists. The Nice model is popular among planetary scientists; it postulates that the gas giant planets underwent orbital migration and scattered objects in the asteroid and/or Kuiper belts into eccentric orbits, and thereby into the path of the terrestrial planets. Other researchers argue that the lunar sample data do not require a cataclysmic cratering event near 3.9 Ga, and that the apparent clustering of impact melt ages near this time is an artifact of sampling materials retrieved from a single large impact basin. They also note that the rate of impact cratering could be significantly different between the outer and inner zones of the Solar System.
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