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Asteroids
Asteroids

... that 4.6 billion years ago, when our solar system was being formed, a tenth planet tried to form between Mars and Jupiter. However, Jupiter’s gravitational forces were too strong, so the material was unable to form a planet. Even if a planet had formed, it wouldn’t have been anything to write home a ...
Comets - Cloudfront.net
Comets - Cloudfront.net

University of Manchester Primary PGCE Appendix I
University of Manchester Primary PGCE Appendix I

File
File

... 1. The planets most unlike the Earth are the gas giants (Jupiter, Saturn …) They are unlike in all regards,  Composition (made of gas)  Size (much larger than Earth)  distance from Sun (much further away)  Temperature (much colder)  (other reasons…?) 2. The planet(s) most similar to Earth is…. ...
Pluto and Comets
Pluto and Comets

... Neptune, why doesn’t it ever collide with Neptune? A. They do collide every few thousand years. B. Neptune is primarily made of gases, so Pluto would pass right through it. C. Pluto’s orbit is steeply tilted with respect to Neptune’s, so they never actually cross. D. The synchronized timing of their ...
Powerpoint - u.arizona.edu
Powerpoint - u.arizona.edu

... Neptune • Neptune is the 8th (usually) planet from the sun. (Sometimes it passes in back of Pluto, making it the 9th planet.) • Neptune is the 4th largest planet. • Neptune is a giant gas planet. • Methane makes Neptune appear blue. This makes it very cold on Neptune. • Neptune has 8 moons. • Neptu ...
The Planets
The Planets

... What are the planets?  There are eight planets in our Solar System:  Mercury  Venus  Earth ...
Planet Saturn
Planet Saturn

... combined. The particles range in size from a couple centimeters to over a kilometer in size. The rings are very thin. Although they reach diameters in the hundred thousands kilometers, they are no more than 1.5 km thick. So how can such a thin layer of ice pieces be so beautiful? The ice creates a r ...
Planet Saturn
Planet Saturn

... combined. The particles range in size from a couple centimeters to over a kilometer in size. The rings are very thin. Although they reach diameters in the hundred thousands kilometers, they are no more than 1.5 km thick. So how can such a thin layer of ice pieces be so beautiful? The ice creates a r ...
Kuiper belt objects - Rosemary`s ePortfolio
Kuiper belt objects - Rosemary`s ePortfolio

... It was named by an 11-year-old girl who suggested the name to her grandfather About 2/3 of the diameter of Earth’s moon 248-year-long elliptical orbit Can travel as far as 49.3 AUs from the Sun A thin atmosphere is created around it when it gets close to the sun in its orbit because its surface ices ...
Objects in Space
Objects in Space

... Meteoroid: is a small rock or particle of debris in our solar system. They range in size from dust to around 10 meters in diameter (larger objects are usually referred to as asteroids). Meteor: A meteoroid that burns up as it passes through the Earth’s atmosphere is known as a meteor. If you’ve ever ...
The Juno Investigation of Water in Jupiter
The Juno Investigation of Water in Jupiter

... –  beyond  the  search  for  life   –  Oxygen  is  the  3rd  most  abundant  element   –  Likely  the  most  common  mul,-­‐element  molecule   ...
nov14
nov14

... Why do you think weather patterns on Jupiter can last for centuries, while those on Earth rarely last for more than a few days? ...
Moons of the Solar System
Moons of the Solar System

... crash into Mars in 40 or 50 million years, or the planet’s gravity might break Phobos apart, creating a thin ring around Mars. Of the terrestrial (rocky) planets of the inner solar system, nei ther Mercury nor Venus has any moons at all, Earth has one, and Mars has its two small moons. In the outer ...
Understanding the Outer Planets and Planetary Atmospheres
Understanding the Outer Planets and Planetary Atmospheres

... thin and composed of dust-like small particles. Saturn’s rings are broad, bright, and opaque. Uranus has narrow, dark rings among broad lanes of dust that are invisible from Earth. Neptune’s rings include incomplete arcs restricted to a small section of their ...
1 Astronomical Fundamentals of Time
1 Astronomical Fundamentals of Time

mayreview3
mayreview3

Our Solar System
Our Solar System

... •  Planets are categorized as terrestrial and Jovian planets. The terrestrial planets are small inner planets, and Jovian planets are large outer planets. •  The terrestrial planets are rocky, dense, made of heavy elements, and the Jovian planets are gaseous and made of hydrogen, helium or ice. •  A ...
THE ITASEL PROJECT: (ITALIAN SEARCH FOR …
THE ITASEL PROJECT: (ITALIAN SEARCH FOR …

Ten Important Comet Facts
Ten Important Comet Facts

... 2. Comets are composed of ices, dust and rocky debris carried from the early formation of the solar system about 4.5 billion years ago. 3. Comets are remnants from the cold, outer regions of the solar system. They are generally thought to come from two areas - the Oort Cloud and the Kuiper Belt. Bot ...
Week of: October 8, 2011
Week of: October 8, 2011

Earth_Universe02
Earth_Universe02

... • Discovered in 1930 • Highly elongated orbit causes it to occasionally travel inside the orbit of Neptune, where it resided from 1979 thru February 1999 • Moon (Charon) discovered in 1978 • Average temperature is -210ºC ...
Cruising the Solar System
Cruising the Solar System

Chapter 7: A Planetary Overview
Chapter 7: A Planetary Overview

... 1. According to the core-accretion model of planetary formation, planets start as small chunks of rock, dust, and debris and grow through accretion and collisions. However, planets like Jupiter would take longer to form than the lifespan of the accretion disk around the star. 2. According to the dis ...
Homework 3
Homework 3

... relative radii of each object with respect to each other. In this case, we can adopt the books values of the size of the Sun and Jupiter in terms of Earth radii. The radius of the sun is 108 earth radii, while Jupiter is 11.2 times larger than the Earth. Then we can find the number of Earths that fi ...
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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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