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13 Formation
13 Formation

Planets in the Solar System - Etiwanda E
Planets in the Solar System - Etiwanda E

... and small amounts of helium.  Saturn is 30% less dense than water…Saturn would float in an ocean!  Winds blow at high speeds on Saturn and can reach up to 1,100 miles an hour.  Saturn is very cold and its average temperature is about –130 degrees Celsius. ...
Moons of Jupiter Age of Surface
Moons of Jupiter Age of Surface

... Roche’s limit and the Rings Large objects cannot form in this region, or get broken up even if they do form. 4. Why can’t the material in the rings collect to form moons? a. There is not enough material b. The rings are too thin c. The rings are inside the Roche limit d. The rings are not made of s ...
Astro Ch 19 planets
Astro Ch 19 planets

Life on Jovian Moons
Life on Jovian Moons

... Many of the larger Jovian moons orbit nearly in the equatorial plane of Jupiter, and in the same direction ...
Comets - Cloudfront.net
Comets - Cloudfront.net

The Solar System (Planetary Debris) - NATSCI-A7
The Solar System (Planetary Debris) - NATSCI-A7

... everything became the planets and the moons. There are other remnants from the solar nebula that are called planetary debris. These are what we know as asteroids, meteoroids and comets. ...
Earth_and_Space_Science
Earth_and_Space_Science

Article - public.iastate.edu
Article - public.iastate.edu

File - We All Love Science
File - We All Love Science

... orbit inclined 44° – Because of these, and its own orbit and size, the International Astronomical Union defined Pluto and other like bodies as dwarf planets – Plutoids: dwarf planets that orbit our Sun ...
Presentation 3
Presentation 3

... solar system. It is in the farther part of our solar system. It's orbit period expands from 10,000 years too 20,000 years. The gravitational effects which would explain the improbable orbital configuration of transNeptunian objects that orbit mostly around the Kuiper belt. The Kuiper belt is home to ...
Document
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kindergarten - Math/Science Nucleus
kindergarten - Math/Science Nucleus

answer key
answer key

... Neptune’s small icy moons, only it’s orbiting the Sun instead of a planet. These moons would grow tails if they ever got as close to the sun as comets get!) - When a comet is 3-4 AU from the Sun, however, its icy surface becomes too warm to remain stable. Part of it becomes gaseous and expands into ...
PTYS/ASTR 206 – Section 2 – Fall 2004 Activity #1: 8/25/04
PTYS/ASTR 206 – Section 2 – Fall 2004 Activity #1: 8/25/04

... A) They have more elliptical orbits B) Their orbits are not as inclined with respect to the ecliptic plane C) They do not form dust tails D) The process of naming them is different. #23. What peculiar feature accompanies Io in its orbit around Jupiter? A) a torus or ring of ionized sulfur, oxygen, a ...
Jupiter - barransclass
Jupiter - barransclass

... and have the party of a lifetime at the Intergalactic casino. Either way you’ll leave Jupiter with new memories and stories to tell for years! You’re going to need them for the trip back...am I right? Contact your local travel agency to get more information on travel days and times! Hope to see you ...
Georgia Performance Standard Or QCC Objective
Georgia Performance Standard Or QCC Objective

... S6E1 – Students will explore current scientific views of the universe and how those views evolved. a) Relate the Nature of Science to the progression of basic historical scientific models (geocentric, heliocentric) as they describe our solar system, and the Big Bang as it describes the formation of ...
The Solar System - Solon City Schools
The Solar System - Solon City Schools

Motions of the Planets
Motions of the Planets

... Both models were riddled with mistakes. The major problems were: ...
Solar System Webquest - Planets, Moons, +
Solar System Webquest - Planets, Moons, +

... 1. How many planets (not including Dwarf Planets) are there in our Solar System? ...
The Sun - ic crosia
The Sun - ic crosia

...  Earth is the third planet from the Sun  It is only planet which supports a variety of life  It’s called the ‘ goldilocks planet ‘, because it’s not too hot and not to cold  it is the densest major body in the solar system. This means that it's the most "compact" of all the planets  it is 4.5 ...
Lesson 3 The Solar System
Lesson 3 The Solar System

... planet. Other dwarf planets include Ceres and Eris. Ceres is found in the asteroid belt between Mars and Jupiter. Eris is slightly larger than Pluto and even farther from the Sun. ...
ppt
ppt

... the asteroid belt (beyond Mars, but within Jupiter) performs a flyby at Jupiter – Configuration 1: What ΔV is required to escape the solar system? – Configuration 2: What ΔV is required for an orbit with a peri-helium smaller than 1 AU? – Show that configuration 2 occurs less often than configuratio ...
Exercise 2
Exercise 2

... Since the original nebula was not homogeneous, it meant that some regions in the disk contained different material than other regions. For example, rock and metal have much higher condensation temperatures (temperatures at which solids can form) than ices, so they are more stable closer to the Sun. ...
The Solar System
The Solar System

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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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