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Slide 1
Slide 1

Chapter 2 Universe and Planetary Geology
Chapter 2 Universe and Planetary Geology

... definition, our Solar System has eight planets: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune. In the new scheme, Pluto will be one of several "dwarf planets" in the Solar System; but "dwarf planets" are not considered true planets. The controversy over Pluto's status as a planet ...
locations, origins and histories of biogenic substances?
locations, origins and histories of biogenic substances?

Saturn - Wikispaces
Saturn - Wikispaces

... Saturn can be seen by the naked eye Flattest planet in the Solar System Orbits the sun once every 29.4 Earth years ...
Existence of collisional trajectories of Mercury, Mars and Venus with
Existence of collisional trajectories of Mercury, Mars and Venus with

... becomes a red giant). The most precise long-term solutions for the orbital motion of the Solar System are not valid over more than a few tens of millions of years9,10. A numerical integration of the Solar System’s motion over 5 Gyr can thus only be considered as a random sample of its possible evolu ...
Asteroids and Meteorites
Asteroids and Meteorites

planetinvasionwebquest[1]. - teachingandlearningwithtech
planetinvasionwebquest[1]. - teachingandlearningwithtech

... What is the size of the planet? What is the length of days and years? Find 3 interesting facts about Jupiter. Find at least 1 similarity and one 1 difference between Jupiter and Earth. http://starchild.gsfc.nasa.gov/docs/StarChild/solar_system_level1/j upiter.html http://www.enchantedlearning.com/su ...
File
File

... – It is very unlike the other planets in composition, size, and orbit. – Pluto has a highly elliptical orbit, like comets. – It spends most of its orbital time well beyond Neptune, in the Kuiper belt. – Pluto's composition is like that of Kuiper belt objects. – Its look-alike neighbors are not class ...
Astronomy lab: Planets
Astronomy lab: Planets

Comets - Cloudfront.net
Comets - Cloudfront.net

... • The comet, discovered the previous year by astronomers Carolyn and Eugene Shoemaker and David Levy, was observed by astronomers at hundreds of observatories around the world as it crashed into Jupiter's southern hemisphere. ...
Comets
Comets

... • The comet, discovered the previous year by astronomers Carolyn and Eugene Shoemaker and David Levy, was observed by astronomers at hundreds of observatories around the world as it crashed into Jupiter's southern hemisphere. ...
ES21- Astronomy Of The Solar System
ES21- Astronomy Of The Solar System

... Welcome to AST101 – Astronomy of the Solar System hybrid course. The course is based on sets of lecture notes (as Microsoft Word documents), corresponding slides (as Microsoft PowerPoint files) and a packet of laboratory modules. The lecture notes and slides can be accessed through the course websit ...
Gas Planets
Gas Planets

... Saturn‘s most striking features are its rings, which show an impressive radial extent – but only a surprisingly small thickness of 10 – 100 m (right, eith the moon Dione immediately above). Galileo Galilei was the first to observe them (in 1610), but Christiaan Huygens discovered their nature as a d ...
Moons and Rings of Outer Planets
Moons and Rings of Outer Planets

... What is the Roche limit? A. The mass a planet must exceed to have satellites. B. The minimum mass for a planet to be composed of hydrogen. C. The maximum orbit distance for a moon before being captured by the Sun’s gravity. D. The distance at which a moon held together by gravity will be broken apar ...
10 Comets, Dwarf Planets, Asteroids and Meteoroids
10 Comets, Dwarf Planets, Asteroids and Meteoroids

... Older theory: Pluto formed as a satellite of Neptune and was ejected by interaction with a massive planetesimal. Mostly abandoned today because such interactions are unlikely. ...
23.1 The Solar System
23.1 The Solar System

... began to collide and clump together through a process known as accretion. The colliding matter formed small, irregularly shaped bodies called planetesimals. As the collisions continued, the planetesimals grew larger, as shown in Figure 3C on page 647. They acquired enough mass to exert a gravitation ...
Jupiter
Jupiter

Dense (> 3000 kg/m 3 )
Dense (> 3000 kg/m 3 )

... Besides the planets, the solar system includes satellites of the planets, asteroids, comets, and trans-Neptunian objects. Seven large planetary satellites (one of which is our Moon) are comparable in size to the planet Mercury. The remaining satellites of the solar system are much smaller. ...
Space and Planetary Environment
Space and Planetary Environment

... dust grains that are captured by Earth’s gravitational field and enter the atmosphere to be destroyed by air drag. Occasionally, larger meteorites able to reach the surface occur. Most items of space debris in LEO are, however, artificial. The large pieces of space debris are accurately tracked usin ...
Astronomy 3.0.2 - Session 1
Astronomy 3.0.2 - Session 1

... spherical heads of different sizes and colors. Stick four or five small-headed pins and four or five large-headed pins into separate corks. Pinheads can be any color, but a variety of colors is best, so that students can tell their “planets” apart. For example, you might include a large pinhead in g ...
Solar System: Small Bodies
Solar System: Small Bodies

... Astronomers once thought that the Main Belt was the debris ring left over from a destroyed__________. It’s much more likely that such a planet was, in fact, prevented from ever forming by Jupiter’s strong gravitational pull. In total, the mass of all the asteroids is less than that of Earth's moon. ...
Phys 214. Planets and Life
Phys 214. Planets and Life

Comet - Physics
Comet - Physics

... Orbits are millions of years. None come from interstellar space. These come from the Oort cloud. Collisions are a possibility, but more than likely these orbits started this way (we will see how later). • Although collisions are possible, they are not likely. There is just too much space out there. ...
Decadal Survey Moon Summary
Decadal Survey Moon Summary

... Further characterization of current or paleo-dynamos in the cores of the terrestrial planets and satellites of the outer solar system may significantly increase our knowledge of magnetic field generation and evolution in planetary cores. Planetary exospheres, those tenuous atmospheres that exist on ...
Lecture 1
Lecture 1

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Nice model



The Nice model (/ˈniːs/) is a scenario for the dynamical evolution of the Solar System. It is named for the location of the Observatoire de la Côte d'Azur, where it was initially developed, in Nice, France. It proposes the migration of the giant planets from an initial compact configuration into their present positions, long after the dissipation of the initial protoplanetary gas disk. In this way, it differs from earlier models of the Solar System's formation. This planetary migration is used in dynamical simulations of the Solar System to explain historical events including the Late Heavy Bombardment of the inner Solar System, the formation of the Oort cloud, and the existence of populations of small Solar System bodies including the Kuiper belt, the Neptune and Jupiter Trojans, and the numerous resonant trans-Neptunian objects dominated by Neptune. Its success at reproducing many of the observed features of the Solar System means that it is widely accepted as the current most realistic model of the Solar System's early evolution, though it is not universally favoured among planetary scientists. One of its limitations is reproducing the outer-system satellites and the Kuiper belt (see below).
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