How Much Rock is in an Icy Moon? (Student Page)
 Grade Level Grades K-4 Grades 5-8 Grades 9-12 Solar System Body Our Solar System Sun Mercury Venus Earth Earth's Moon Mars Asteroids Meteors & Meteorites Jupiter Europa Saturn Uranus Neptune Dwarf Planets Comets Kuiper Belt & Oort Cloud Beyond Our Solar System Mission Akatsuki Cassini Earth Science Missions Galileo Hubble Space Telescope Juno LADEE Lunar Reconnaissance Orbiter Mars Exploration Rovers Mars Reconnaissance Orbiter Mars Science Laboratory/Curiosity MAVEN Pioneer 10 Pioneer 11 Venus Express Voyager 1 Voyager 2 Topic Space Math Water in the Solar System Windy Worlds: Gas Giants, Atmospheres and Weather
 How Much Rock is in an Icy Moon? (Student Page) Download This Lesson Topic: Grade Level: 5-8 Body: Jupiter, Saturn, Uranus, Neptune Mission: Science Education Standards: Earth and Space Science -- Content Standard D Properties and Changes of Properties in Matter A substance has characteristic properties, such as density, a boiling point and solubility, all of which are independent of the amount of the sample. A mixture of substances often can be separated into the original substances using one or more of the characteristic properties. Earth in the Solar System: The Earth is the third planet from the sun in a system that includes the Moon, the sun, seven other planets and their moons, and smaller objects, such as asteroids and comets. Structure of the Earth System: Water, which covers the majority of the Earth's surface, circulates through the crust, oceans, and atmosphere in what is known as the "water cycle." Water evaporates from the Earth's surface, rises and cools as it moves to higher elevations, condenses as rain or snow, and falls to the surface where it collects in lakes, oceans, soil, and in rocks underground. Water is a solvent. As it passes through the water cycle it dissolves minerals and gases and carries them to the oceans. Short Description: In order to determine the percentages of rock and ice in a number of the satellites (moons) of the outer planets (Jupiter, Saturn, Uranus, Neptune, and Pluto), students construct a graph of the amount of rock versus the density of the moon, using a simple equation. They then determine the percentage of rock from the densities of several moons and enter the answers in a table.