on it, can still ripen a bunch of grapes as though it had nothing else in the Universe to do. Galileo Galilei

Similar documents
Today. Solar System Formation. a few more bits and pieces. Homework due

What is it like? When did it form? How did it form. The Solar System. Fall, 2005 Astronomy 110 1

Astro 1: Introductory Astronomy

The Coriolis effect. Why does the cloud spin? The Solar Nebula. Origin of the Solar System. Gravitational Collapse

9. Formation of the Solar System

What does the solar system look like?

Lecture Outlines. Chapter 15. Astronomy Today 7th Edition Chaisson/McMillan Pearson Education, Inc.

1star 1 star 9 8 planets 63 (major) moons asteroids, comets, meteoroids

Astronomy. physics.wm.edu/~hancock/171/ A. Dayle Hancock. Small 239. Office hours: MTWR 10-11am

-Melissa Greenberg, Arielle Hoffman, Zachary Feldmann, Ryan Pozin, Elizabeth Weeks, Christopher Pesota, & Sara Pilcher

9/22/ A Brief Tour of the Solar System. Chapter 6: Formation of the Solar System. What does the solar system look like?

Clicker Question: Clicker Question: Clicker Question:

Comparative Planetology II: The Origin of Our Solar System. Chapter Eight

23.1 The Solar System. Orbits of the Planets. Planetary Data The Solar System. Scale of the Planets The Solar System

Prentice Hall EARTH SCIENCE

Chapter 8 Formation of the Solar System

Gravity: Motivation An initial theory describing the nature of the gravitational force by Newton is a product of the resolution of the

Chapter 06 Let s Make a Solar System

Which of the following statements best describes the general pattern of composition among the four jovian

Accretionary Disk Model

Brooks Observatory telescope observing this week

How did it come to be this way? Will I stop sounding like the

Prentice Hall EARTH SCIENCE

Formation of the Solar System. What We Know. What We Know

( ) a3 (Newton s version of Kepler s 3rd Law) Units: sec, m, kg

Cosmology Vocabulary

It Might Be a Planet If...

Announcements. HW #3 is Due on Thursday (September 22) as usual. Chris will be in RH111 on that day.

Comparative Planetology II: The Origin of Our Solar System. Chapter Eight

Astronomy 1 Winter Lecture 11; January

Ag Earth Science Chapter 23

MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question.

Making a Solar System

Chapter 4 The Solar System

Radioactive Dating. U238>Pb206. Halflife: Oldest earth rocks. Meteors and Moon rocks. 4.5 billion years billion years

Jovian Planet Properties

The Formation of the Solar System

Chapter 15: The Origin of the Solar System

Chapter 8 Lecture. The Cosmic Perspective Seventh Edition. Formation of the Solar System

Moon Obs #1 Due! Moon visible: early morning through afternoon. 6 more due June 13 th. 15 total due June 25 th. Final Report Due June 28th

1 of 5 5/2/2015 5:50 PM

Agenda. International Space Station (ISS) International Space Station (ISS) Can we see light from first stars? 9. Formation of the Solar System

Solar System Formation

Class 15 Formation of the Solar System

Planetary Interiors. Earth s Interior Structure Hydrostatic Equilibrium Heating Constituent Relations Gravitational Fields Isostasy Magnetism

Galaxies: enormous collections of gases, dust and stars held together by gravity Our galaxy is called the milky way

The Solar System - I. Alexei Gilchrist. [The Story of the Solar System]

Formation of the Solar System Chapter 8

Vagabonds of the Solar System

12/3/14. Guiding Questions. Vagabonds of the Solar System. A search for a planet between Mars and Jupiter led to the discovery of asteroids

Astronomy Wed. Oct. 6

Chapter Outline. Earth and Other Planets. The Formation of the Solar System. Clue #1: Planetary Orbits. Clues to the Origin of the Solar System

The Big Bang Theory (page 854)

The Solar System consists of

Chapter 9 Remnants of Rock and Ice. Asteroids, Comets, and Pluto

Comparative Planetology I: Our Solar System

The History of the Earth

Earth s Formation Unit [Astronomy] Student Success Sheets (SSS)

Pearson Education Limited Edinburgh Gate Harlow Essex CM20 2JE England and Associated Companies throughout the world

Chapter 23: Touring Our Solar System

Our Planetary System & the Formation of the Solar System

Currently, the largest optical telescope mirrors have a diameter of A) 1 m. B) 2 m. C) 5 m. D) 10 m. E) 100 m.

The History of the Solar System. From cloud to Sun, planets, and smaller bodies

Astronomy (Geology 360, Physics 360) take-home test. There is no class on Monday March 16th

Origin of the Solar System

Solar System Formation

HNRS 227 Fall 2006 Chapter 13. What is Pluto? What is a Planet? There are two broad categories of planets: Terrestrial and Jovian

9.2 - Our Solar System

CHAPTER 11. We continue to Learn a lot about the Solar System by using Space Exploration

The Solar System. Sun. Rotates and revolves around the Milky Way galaxy at such a slow pace that we do not notice any effects.

Solar System. Sun, 8 planets, hundred moons, thousand.dwarf.planets million asteroids, billion comets etc.

Physics Homework 5 Fall 2015

Physics Homework 5 Fall 2015

Earth Science 11 Learning Guide Unit Complete the following table with information about the sun:

Celestial Objects. Background Questions. 1. What was invented in the 17 th century? How did this help the study of our universe? 2. What is a probe?

Solar System Formation

Astronomy 241: Foundations of Astrophysics I. The Solar System

5. How did Copernicus s model solve the problem of some planets moving backwards?

Outline. Question of Scale. Planets Dance. Homework #2 was due today at 11:50am! It s too late now.

Name Class Date. For each pair of terms, explain how the meanings of the terms differ.

OUR SOLAR SYSTEM. James Martin. Facebook.com/groups/AstroLSSC Twitter.com/AstroLSSC

Astr 1050 Wed., March. 22, 2017

Planetarium observing is over. Nighttime observing starts next week.

Astronomy 103: First Exam

Which of the following planets are all made up of gas? When a planets orbit around the Sun looks like an oval, it s called a(n)

3. The name of a particularly large member of the asteroid belt is A) Halley B) Charon C) Eris D) Ceres E) Triton

Phys 214. Planets and Life

Formation of the Solar System

Opaque Atmosphere. Astronomy 210. Question. Why would it be useful to place telescopes in. Section 1 MWF Astronomy Building. space?

Solar System Junk however, a large number of bodies were left over as Junk or the debris of planet building

The Solar System. Tour of the Solar System

Overview of Solar System

Notes: The Solar System

Phys 214. Planets and Life

Ch 23 Touring Our Solar System 23.1 The Solar System 23.2 The Terrestrial Planet 23.3 The Outer Planets 23.4 Minor Members of the Solar System

ASTRONOMY SNAP GAME. with interesting facts

1. Solar System Overview

Starting from closest to the Sun, name the orbiting planets in order.

Why are Saturn s rings confined to a thin plane? 1. Tidal forces 2. Newton s 1st law 3. Conservation of energy 4. Conservation of angular momentum

1 Solar System Debris and Formation

Transcription:

The Sun, with all the planets revolving around it, and depending on it, can still ripen a bunch of grapes as though it had nothing else in the Universe to do. Galileo Galilei

What We Will Learn Today Where did asteroids and comets come from? What was the early Solar System like? How did our Moon form? How do we know the age of our solar system?

Patterns Explained So Far The nebular model seems to work Sun dominates the Solar System 99.9% of mass, ~ 100% of light All planets roughly confined to a disk All planets orbits are prograde The orbits have low eccentricity Most planets rotate prograde Most moons orbit & rotate prograde Two types of planets exist Terrestrial close to Sun and Jovian farther out

Unexplained Patterns The many asteroids and comets in our solar system Why do they live in specific zones? Why did they not condense into planets? The exceptions observed Retrograde orbits of Venus and Uranus Retrograde orbits of several moons, including one large moon Earth s relatively large moon

The Asteroid Belt Occupies the region between Mars and Jupiter The terrestrial planets cleared their orbits either by assimilation or ejection Asteroids are planetesimals that never became a planet Jupiter s gravity prevented condensation Found a home in this large vacant space The asteroids collectively are only a small fraction of the mass of a terrestrial planet Probably were of planet mass early on Most assimilated into planets or ejected out

The Kuiper Belt Comets initially inhabited the entire solar system Ice-rich planetesimals Out to beyond Neptune s orbit Beyond Neptune s orbit, they remained in stable orbits around the Sun Short-period comets come from the Kuiper belt Including Halley s comet (P = 76 years)

The Oort Cloud Comets that started among Jovian planets or wandered too close were swallowed or ejected Scattering is a lot more probable than collisions Close encounters banished them to the outer reaches of the solar system No preferential direction of scattering Not confined to the disk, Oort cloud is spherical Contains many billions of comets 50,000 AU away Have not been observed, except when they come close to the Sun

The Early Solar System Fireworks Heavy Bombardment First few hundred million years Left marks we clearly see on many planets and moons today Enriched terrestrial planets with water and hydrogen compounds Fig 8.10

Captured Moons While capture does not explain the solar system formation, it is responsible for the orbits of several moons Captures are low probability Extended atmosphere slowed object down Multi-object interaction allowed capture Only works for small objects Consistent with observations Captured moons can have high inclinations and retrograde orbits

Formation of Our Moon Video from Kokubo et al (2000) Fig 8.12

Support for Collision Theory Our moon is too large to have been captured Composition of Earth and Moon different Can t have condensed from the same matter Moon s overall composition is similar to Earth s crust Explains high density of the Earth Explains a large moon Supported by computer simulations Collision also thought to explain Venus, Uranus retrograde orbits Pluto s large moon and retrograde orbit

Review of Solar System Formation Fig 8.13

When Did the Solar System Form? Radioactive dating of the oldest rocks Spontaneous radioactive decay Converts a proton into a neutron, releasing an electron Creates an isotope of a lower atomic number element Random process, but overall rate very predictable for an element Half-life: Time after which half of the original atoms have decayed Fig 8.14

Radioactive Dating Rocks from Moon have roughly equal 238 U and 206 Pb Half-life of this decay is 4.5 billion years So, these rocks are about 4.5 billion years old Check multiple isotope aging to ensure consistency Oldest rocks on Earth are about 4 billion years old Most pristine rocks of the solar system are asteroids The oldest ones of these have an age of about 4.55 billion years Beginning of accretion in the solar nebula The planets formed within 10s of million years They are about 4.5 billion years old Solar model shows that the Sun is 4 5 billion years old Consistent with radioactive dating