'Impact craters' presentation slideshows

3-6 Asteroids

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Intro to Astronomy

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Solar Debris

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Part 4: Our Solar System, Life in the Universe

Part 4: Our Solar System, Life in the Universe. Monday, April 7 Reading: Chapter 15 (12 th Edition of the textbook) Solar System: Introduction and Formation; Other Solar Systems Wednesday, April 9 Reading: Chapter 18 (planets)

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The Moon and Mercury: Airless Worlds

Note that the following lectures include animations and PowerPoint effects such as fly ins and transitions that require you to be in PowerPoint's Slide Show mode (presentation mode). The Moon and Mercury: Airless Worlds. Chapter 21. Guidepost.

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General Features

General Features. Mass: M Earth = 6 x 10 27 g Radius: R Earth = 6378 km Density: ? = 5.5 g/cm 3 Age: 4.6 billion years Orbital period = 365 days Rotation period = 1 day. Clicker Question:. A moon covered with numerous and very old craters created by meteorite impacts likely

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Our Moon and other moons of the Solar System

Our Moon and other moons of the Solar System. Starter 1/25/13. What do you already know about our Moon?. What is a moon?. A moon is a natural satellite of a planet or dwarf planet There are over 170 moons around the planets and dwarf planets in our solar system. Planets and numbers of moons.

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7 th Grade Science State Assessment Review

7 th Grade Science State Assessment Review. https://sas.elluminate.com/p.jnlp?psid=2014-02-07.0836.M.CE19F434D56E599313E9D05729AAD2.vcr&sid=559. Standard 4 Earth and Space Science.

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EARTH'S MOON: LUNA

EARTH'S MOON: LUNA. Origin of the Moon.

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Starry Monday Today!

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Mount Everest stands out at the center of the left image. Glaciers ... At 5,895 m, Mount Kilimanjaro is the highest point in Africa. Kilimanjaro is composed of three volcanoes, ...

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Terrestrial Planetary Geology: Moon, Mercury, Venus & Mars

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Impact Craters and Age - Review

Impact Craters and Age - Review. Finding ages of objects. Absolute ages are assessed through radioactive decay (1/2 lives) Carbon 14, half-life of 5700 years Uranium 238, half-life of 700 million years! Requires lab analysis of physical samples. How it works.

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Chapter 3 The Solar System

Chapter 3 The Solar System. Section 2 Inner Planets Notes 3-2. Inner Planets. Terrestrial Planets: Similar to Earth Solid rock with a metal core No rings Number of moons varies from 2 to zero Covered with impact craters

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Impact Craters

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How do you think these craters were formed?

How do you think these craters were formed?. Impact Craters. What factors do you think affect the appearance and size of craters & ejecta ?. Why do we study craters?. How should we study impact craters?. SEVEN CROSSCUTTING CONCEPTS OF THE FRAMEWORK. Patterns Cause and Effect

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Craters on the Moon

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January 22

January 22. Learning targets. I will be able to describe the formation of the moon I can explain what causes tides. Agenda. Kick off question: Why is the moon important? Time for Reading Assignment (silent reading) if needed

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