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How Did Our Moon Form and What`s Been Happening Since?
How Did Our Moon Form and What`s Been Happening Since?

... Venus, Earth, Mars) … it’s “lighter”. Less iron than Earth Moon is unusually big for a satellite Earth/Moon system has a lot of angular momentum (spin + orbital motion) Chemical composition similar to Earth’s mantle A tilted orbit relative to Earth’s path around the Sun ...
Earth, Space and all that jazz… A long time ago, in the second
Earth, Space and all that jazz… A long time ago, in the second

... Earth, Space and all that jazz… A long time ago, in the second century, There was a Greek astronomer called Claudius Ptolemy. Who came up with a theory called the geocentric model, Which made the Earth the focal point and centre of it all. Centuries went past before some began to doubt. ‘We simply d ...
post-class version, 374 KB - Department of Physics and Astronomy
post-class version, 374 KB - Department of Physics and Astronomy

... Solar system overview (chapter 6, today) Solar system formation or origin (chapter 6, Wednesday) ...
Chapter 20 Questions
Chapter 20 Questions

... 1. What does the term AU stand for? 2. What measurements are used to indicate the distance between stars? 3. What are the names of the 2 groupings of planets? 4. What are 3 differences between the inner and outer planets? 5. What are the inner planets called or classified as? 6. What is the order of ...
How do the planets stay in orbit around the sun?
How do the planets stay in orbit around the sun?

... cloud of gas and dust which spun around a newly forming star, our sun, at its center. The planets all formed from this spinning diskshaped cloud, and continued this rotating course around the sun after they were formed. The gravity of the sun keeps the planets in their orbits. They stay in their orb ...
Volcanoes and Igneous Activity Earth - Chapter 4
Volcanoes and Igneous Activity Earth - Chapter 4

... • Original crust (highlands) • As Moon formed, its outer shell melted, cooled, solidified, and became the highlands • About 4.5 billion years old ...
what is in the solar system? - Istituto Comprensivo Nord di Prato
what is in the solar system? - Istituto Comprensivo Nord di Prato

... Europa, Ganymede, Io and Callisto. you can see even erupting volcanoes! ...
Ch 20: A Family of Planets
Ch 20: A Family of Planets

... – Low air pressure adds to low temps—liquid water boils away ...
Study Guide for Quiz on Astronomy: The Moon, Sun and Stars
Study Guide for Quiz on Astronomy: The Moon, Sun and Stars

... 17. How is distance measured in the universe? __________________________________________ 18. In which galaxy do we live? __________________________________What kind of galaxy is it? ___________ At what location in our galaxy is our solar system?________________________ 19. Which planet is considered ...
Asteroids February 23 − Why is the solar system spinning & disk shaped?
Asteroids February 23 − Why is the solar system spinning & disk shaped?

... • larger bodies had more gravitational attraction ...
Solar System Cornell Notes - CE Williams Middle School
Solar System Cornell Notes - CE Williams Middle School

... meteorite - when a meteor is so large that it doesn't completely vaporize in Earth's atmosphere and reaches Earth's surface. asteroid - large pieces of rock with same composition of planets. Large What is the asteroid belt between Mars and Jupiter believed to be from unformed Kuiper Disk? planet. Li ...
NAME - wths
NAME - wths

... Reading Guide – Chapter 27 The Planets and the Solar System Before you read each section, look over the questions that you are to answer. Then, once you know what you are reading for, begin to read the section. As you are reading, answer the questions. ...
Chapter 7 Study notes
Chapter 7 Study notes

... You should remember that: 1. The more mass an object has the more gravity that it has 2. Gravity is what hold planets in their orbits 3. Planets orbit in an elliptical path 4. We live in the Milky Way galaxy ____________________________________________________ You should be able to explai n: 1. How ...
Benchmark Number:
Benchmark Number:

... A celestial body that appears as a fuzzy head usually surrounding a bright nucleus, that has a usually highly eccentric orbit, that consists primarily of ice and dust, and that often develops one or more long tails when near the sun. ...
EARTH AS A PLANET TEST REVIEW
EARTH AS A PLANET TEST REVIEW

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... in space, has large impact basins (mare) filled with black volcanic basalt flows. The crater with the pronounced ejecta rays at the bottom of the image is Tycho ...
Planet Facts
Planet Facts

... Planet Notes Presentation from http://teachers.greenville.k12.sc.u s/sites/ceckles/Pages/Assignment s.aspx By Chance Eckles ...
Astronomy Name Solar System Objects Quiz Study Guide 1. Solar
Astronomy Name Solar System Objects Quiz Study Guide 1. Solar

... 2. Where are the best places to find meteorites? Why there? 3. Describe at least THREE characteristics of meteorites? 4. The largest asteroid is _________. 5. How are comets named? 6. How are meteorites named? 5. Planet trivia match (Use can use your Solar System Fact Sheet) 1. Planet most like our ...
The SLAM Impact Experiment: Overview and - SwRI
The SLAM Impact Experiment: Overview and - SwRI

... but “it is patently not the case” that all rocks would have been reset or “pulverized to fine powder” (Hartmann et al., 2000 [presumably one of his co-authors])  comminution by a couple generations of large-crater saturation is NOT like modern churning of uppermost meters of regolith ...
Chapter 7 – Our Planetary System 7.1 Studying the Solar System
Chapter 7 – Our Planetary System 7.1 Studying the Solar System

... Nearly identical in __________________ to Earth; surface hidden by clouds ...
Slide 1
Slide 1

... • Fragments of rock made of material similar to the material that formed the planets. – More than 50,000 asteroids have been found in our solar system. ...
Study Guide for Midterm 2 Midterm 1 Exam procedures
Study Guide for Midterm 2 Midterm 1 Exam procedures

... • Rocks from each brought back by Apollo astronauts. • Age dating • Chemical composition • Tidally locked to Earth • Formation of Moon • Giant Impact is current favorite theory… collision between Earth & Mars-sized object. ...
Solar System Study Guide
Solar System Study Guide

... * solar system- a sun and all the objects that move around it * orbit- the path that one object in space takes around another object in space * gravity- the force that pulls objects toward each other * asteroid belt- the group of rocks that separates the inner from the outer planets * planet- a larg ...
The Gas Giants
The Gas Giants

Earth Science, 10th edition Chapter 21: Touring Our Solar System I
Earth Science, 10th edition Chapter 21: Touring Our Solar System I

... b. Gray, unconsolidated debris c. Composed of 1. Igneous rocks 2. Breccia 3. Glass beads 4. Fine lunar dust d. "Soil-like" layer e. Produced by meteoric bombardment C. Lunar History 1. Hypothesis suggests that a giant asteroid collided with Earth to produce the Moon a. Older areas have a higher dens ...
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Late Heavy Bombardment



The Late Heavy Bombardment (abbreviated LHB and also known as the lunar cataclysm) is a hypothetical event thought to have occurred approximately 4.1 to 3.8 billion years (Ga) ago, corresponding to the Neohadean and Eoarchean eras on Earth. During this interval, a disproportionately large number of asteroids apparently collided with the early terrestrial planets in the inner Solar System, including Mercury, Venus, Earth, and Mars. The LHB happened after the Earth and other rocky planets had formed and accreted most of their mass, but still quite early in Earth's history.Evidence for the LHB derives from lunar samples brought back by the Apollo astronauts. Isotopic dating of Moon rocks implies that most impact melts occurred in a rather narrow interval of time. Several hypotheses are now offered to explain the apparent spike in the flux of impactors (i.e. asteroids and comets) in the inner Solar System, but no consensus yet exists. The Nice model is popular among planetary scientists; it postulates that the gas giant planets underwent orbital migration and scattered objects in the asteroid and/or Kuiper belts into eccentric orbits, and thereby into the path of the terrestrial planets. Other researchers argue that the lunar sample data do not require a cataclysmic cratering event near 3.9 Ga, and that the apparent clustering of impact melt ages near this time is an artifact of sampling materials retrieved from a single large impact basin. They also note that the rate of impact cratering could be significantly different between the outer and inner zones of the Solar System.
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