The Planets. The Terrestrial Planets. Admin. 9/19/17. Key Concepts: Lecture 13. Formulae (will be displayed for you in Midterm 1):

Size: px
Start display at page:

Download "The Planets. The Terrestrial Planets. Admin. 9/19/17. Key Concepts: Lecture 13. Formulae (will be displayed for you in Midterm 1):"

Transcription

1 Admin. 9/19/17 1. Class website 2. Optional Discussion sections: Tue. ~11.30am (period 5), Bryant 3; Thur. ~12.35pm (end of period 5 and period 6), start in Pugh 170, then Bryant 3 [only Tue. discussion this week] 3. Office hr: Tuesday pm; Wed pm, Bryant 302 (but me if coming on Wed.). [only Tue. office hr. this week] 4. Reading this week: Chapters 0, 1, , 4.1, 5, 6 5. Midterm 1: Thur. Sept. 21st, in class BRING YOUR UF ID TO THE EXAM. For review go to Discussion Sections or Office Hrs. Best preparation is to review class notes (up to & including Lecture 12) and homework & quizzes, then also the textbook. You will not be able to use a calculator or refer to your class notes in the exam. You will receive a list of formulae (see next slide). Exam is multiple choice, similar to HWs. Bring a pencil. 6. Observing project deadline: Thursday Oct. 26th 2017, however, you are strongly advised to complete observing by Fri. Oct. 6th. 7. me Astro-news, jokes, tunes, images: ast1002_tan-l@lists.ufl.edu 8. Printed class notes? Name tags? Key Concepts: Lecture 13 Terrestrial Planets: Overview - How do the properties of planets depend on their mass? Mercury Formulae (will be displayed for you in Midterm 1): Speed = distance / time Angular size: θ = size / distance Kepler s 3rd Law: P 2 = a 3 [ Newton s version of Kepler s 3rd: P 2 a 3 /(m 1 +m 2 ) ] Newton s 2nd Law: F = m a Newton s Law of Gravity: F m 1 m 2 / r 2 The Planets The Terrestrial Planets Density = mass / volume Volume of a sphere = (4/3)πr 3 Surface area of sphere = 4πr 2 Frequency: f = 1/Period Speed of wave (light) = frequency x wavelength: c = f λ

2 Mercury - Overview Closest planet to the Sun: a=0.4au Only a little bigger than the Moon Property Mercury Earth Radius 2430 km 6378 km Mass 3.3 x Kg 6.0 x kg Density 5430 kg/m kg/m 3 Escape Speed 4.3 km/sec 11.2 km/sec Atmosphere (Very thin!!) Sodium, Potassium Nitrogen, Oxygen Magnetic Field 3.0 x 10-7 T 4.0 x 10-5 T Basically no atmosphere Orbit and Rotation Orbital Period = 88 days Most eccentric orbit of any planet 46 million km to 70 million km Sunlight varies by factor of 2.3 [INVERSE SQUARE LAW FOR FLUX Flux from Sun = Luminosity/(4πr 2 ), where r is distance from Sun; we will discuss later in class] Was found to precess more than Newton s Laws would predict Planet Vulcan? Never found Einstein's Theory of Relativity is the explanation (more later in the class) Rotation = 59 days Rotates 3 times in 2 orbits This synchronization is due to tidal effects from Sun Exploration of Mercury Telescopic Observations Very difficult to observe since it is always near the Sun Giocanni Schiaparelli made a map of subtle dark and bright areas (1877) Space craft exploration Mariner 10 ( ) Messenger (2008+) Structure of Mercury No seismic data Small planet - interior will be relatively cool and solid Large metal core Density roughly equal to Earth Mercury has less gravity so material will be compressed less Thus metallic core should be relatively larger than Earth s Thin solid mantle

3 Surface of Mercury Similar to Moon Lots of impact craters Surface is very old No plate tectonics Craters flatter & have thinner ejecta rims than lunar craters - due to higher gravity on Mercury than on the Moon Some large filled basins similar to lunar Maria (but not as extensive) Less cratered and younger Probably filled with lava from mantle - after large impact Scarps - Cracks and cliffs in the crust; Young - few craters cut them; Probably due to Mercury shrinking as its core cooled not due to plate tectonics Scarp Water on Mercury? Polar craters never have sunlight in them Radar maps from the Earth see: Pole is a bright region of planet Could be frozen water Mercury s Atmosphere North Pole Very, Very thin!!! Basically no atmosphere, because very hot surface with low escape velocity. Large temperature changes: Day = 700K; Night = 90K Small amounts of some elements are trapped from solar wind Sodium and Potassium (gas phase metals) most abundant in the atmosphere From surface impacts or solar wind - Overview Smaller than Earth Two very small moons Property Earth Radius 3397 km 6378 km Mass 6.4 x kg 6.0 x kg Density 3040 kg/m kg/m 3 Escape Speed 5.0km/sec 11.2 km/sec Atmosphere Carbon dioxide, Nitrogen Nitrogen, Oxygen

4 Early Earth-Based Telescopic Exploration of Giovanni Schiaparelli mapped bright and dark regions saw polar caps which changed with seasons Surface colors appeared to change Plant life? identified long narrow features (channels - canale) Percival Lowell ( ) Built observatory in Flagstaff to study Thought the canals were used by a civilization to bring water to a desert planet Spirit & Opportunity Spirit travelled ~5 miles; Opportunity ~15miles Evidence liquid water was once on Space Craft Exploration of [You do not need to remember all the details of these missions] 1965 Mariner 4, 6 & 7 flew by Craters 1971 Mariner 9 orbited and mapped in detail Valleys and volcanoes July 20, 1976 Viking 1 landed on Searched for life Pathfinder (1997) placed a small rover on to study the chemistry of its rocks Rovers, Spirit and Opportunity (2004) Phoenix lander (2008) Curiosity (2012) Astro News

5 Curiosity Structure of Relatively low density compared to earth Small dense core Thick mantle global surveyor found a very weak magnetic field (1997) Liquid/rotating core

6 The Surface of It really is red Due to iron oxide (Rust!) Lots of loose rocks and sand Loose sand from wind erosion blows and drifts around rocks Loose rocks from impacts flooding etc. The Surface of No evidence of plate tectonics (e.g., no horizontal motion of the crust) Impact craters Surface is old and heavily cratered Some are eroded Volcanoes on Volcanism is not as wide spread on as on Earth A few large Volcanoes Olympus Mons 24 km high (78000ft) 500 km in diameter All located on Tharsis bulge Why so big? lower gravity hot spot stayed in one place - no continental drift thicker mantle to hold it up The Surface of - Valleys Valles Marineris 4000 km long 2-7 km deep Large crack Due to stretching and cracking when Tharsis bulge formed Not due to water flow

7 Surface of Flood Plains and River Systems Many flood plains and river systems Liquid water certainly flowed over much of Many are old (~4 billion years) i.e. cratered. Liquid water on today? Possible recent flows of water Wind Features Sand dunes and erosion features Wind erosion features are due to loose dust blowing around objects These are very wide spread Seasonal dust storms occur with very high winds when is warmest The Face on One Viking orbiter image revealed a mountain that looked somewhat like a monkey face Commented on in a NASA press release Immediately seized by tabloids Taken by some as proof that an advanced civilization existed on Example of how our minds find familiar patterns Resolution: each pixel = 43m

8 The Face with Global Surveyor Resolution: each pixel = 1.5m The Atmosphere of Low density: only 1% of Earth s atmosphere CO 2 (95%), Nitrogen(3%), O 2 (.15%) Due to lack of large scale volcanism to return CO 2 to atmosphere Weak greenhouse effect Temperature range: 150K to 295 K Only about +5C warmer than without Large dust storms When Mariner 9 arrived surface completely covered by dust Explanation of color changes rather than plants Seasonal: occur when is heated most by the Sun Ice Caps on The Moons of Northern ice cap is much larger than southern ice cap We re not sure why. Composed of C0 2 ice & some water ice Size varies with season Seasons on are due to its axial tilt and somewhat elliptical orbit tilt of orbital axis is primary cause CO 2 in northern hemisphere completely sublimes in summer leaving mostly water has two very small moons Phobos and Deimos 27 and 15 km across Do not look like our Moon Too small for their gravity to make them round Cratered and very irregular Origin May be fragments from a moon-asteroid collision Phobos Deimos

9 Open Questions About Are there still active volcanoes? Where has the water gone? How much sub-martian water is there? Could there be life hiding some place on? Humans to? Discussed in class Life on? Viking landers performed experiments to test for presence of microbial life - inconclusive. Claims of microbial structures in a Martian meteorite: inconclusive.

Venus - Overview. Exploration of Venus. Admin. 9/26/17. Second planet from Sun Earth s sister planet

Venus - Overview. Exploration of Venus. Admin. 9/26/17. Second planet from Sun Earth s sister planet Admin. 9/26/17 1. Class website http://www.astro.ufl.edu/~jt/teaching/ast1002/ 2. Optional Discussion sections: Tue. ~11.30am (period 5), Bryant 3; Thur. ~12.35pm (end of period 5 and period 6), start

More information

Lecture Outlines. Chapter 10. Astronomy Today 8th Edition Chaisson/McMillan Pearson Education, Inc.

Lecture Outlines. Chapter 10. Astronomy Today 8th Edition Chaisson/McMillan Pearson Education, Inc. Lecture Outlines Chapter 10 Astronomy Today 8th Edition Chaisson/McMillan Chapter 10 Mars Units of Chapter 10 10.1 Orbital Properties 10.2 Physical Properties 10.3 Long-Distance Observations of Mars 10.4

More information

Chapter 17: Mercury, Venus and Mars

Chapter 17: Mercury, Venus and Mars Chapter 17: Mercury, Venus and Mars Mercury Very similar to Earth s moon in several ways: Small; no atmosphere lowlands flooded by ancient lava flows heavily cratered surfaces Most of our knowledge based

More information

Mars: The Red Planet. Roman God of war Blood Reflects 30% of its incident sunlight 2 small moons : Phobos and Deimos

Mars: The Red Planet. Roman God of war Blood Reflects 30% of its incident sunlight 2 small moons : Phobos and Deimos Mars: The Red Planet Roman God of war Blood Reflects 30% of its incident sunlight 2 small moons : Phobos and Deimos Property Earth Mars Radius 6378km 3394km ~ 0.51R E Mass 5.97x10 24 kg 6.42x10 23 kg =

More information

What are terrestrial planets like on the inside? Chapter 9 Planetary Geology: Earth and the Other Terrestrial Worlds. Seismic Waves.

What are terrestrial planets like on the inside? Chapter 9 Planetary Geology: Earth and the Other Terrestrial Worlds. Seismic Waves. Chapter 9 Planetary Geology: Earth and the Other Terrestrial Worlds What are terrestrial planets like on the inside? Seismic Waves Vibrations that travel through Earth s interior tell us what Earth is

More information

Introduction to Mars PTYS/ASTR 206 3/22/07

Introduction to Mars PTYS/ASTR 206 3/22/07 Introduction to Reading Assignment Finish Chapter 13 Announcements Quiz today Will cover all material since the last exam. This is Chapters 9-12 and the part of 13 covered today. Exam #2 next Thursday

More information

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

MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. ASTRO 102/104 Prelim 2 Name Section MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. 1) This is version E of the exam. Please fill in (E). A) This

More information

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

MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. ASTRO 102/104 Prelim 2 Name Section MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. 1) This is version B of the exam. Please fill in (B). A) This

More information

Lecture #11: Plan. Terrestrial Planets (cont d) Jovian Planets

Lecture #11: Plan. Terrestrial Planets (cont d) Jovian Planets Lecture #11: Plan Terrestrial Planets (cont d) Jovian Planets Mercury (review) Density = 5.4 kg / liter.. ~ Earth s Rocky mantle + iron/nickel core Slow spin: 59 days (orbital period = 88 days) No satellites

More information

Mars ( ) The Sun and Planets Lecture Notes 6. Spring Semester 2018 Prof Dr Ravit Helled

Mars ( ) The Sun and Planets Lecture Notes 6. Spring Semester 2018 Prof Dr Ravit Helled The Sun and Planets Lecture Notes 6. Spring Semester 2018 Prof Dr Ravit Helled Mars ( ) Mars is the fourth planet from the Sun and the outermost terrestrial planet. It has a density of 3.93 g/cm3, which

More information

Learning Objectives. they differ in density, composition, atmosphere, surface age, size, geological activity, magnetic field?

Learning Objectives. they differ in density, composition, atmosphere, surface age, size, geological activity, magnetic field? The Red Planet Learning Objectives! Contrast the Terrestrial Planets and the Moon. Do they differ in density, composition, atmosphere, surface age, size, geological activity, magnetic field?! Why is Mars

More information

11/4/2015. Venus and Mars. Chapter 13. Venus and Mars. The Rotation of Venus. The Atmosphere of Venus. The Surface of Venus

11/4/2015. Venus and Mars. Chapter 13. Venus and Mars. The Rotation of Venus. The Atmosphere of Venus. The Surface of Venus Venus and Mars Two most similar planets to Earth: Chapter 13 Venus and Mars Similar in size and mass Same part of the solar system Atmosphere Similar interior structure The Rotation of Venus Almost all

More information

The Main Points. The View from the Surface. Geology of Mars. Lecture #20: Reading:

The Main Points. The View from the Surface. Geology of Mars. Lecture #20: Reading: Surface of Mars Lecture #20: Geology and Geologic Processes View from the Surface History/Evolution of the surface Reading: Chapter 9.4 The Main Points Mars has had a geologically active past that has

More information

Chapter 9 Planetary Geology: Earth and the Other Terrestrial Worlds

Chapter 9 Planetary Geology: Earth and the Other Terrestrial Worlds Chapter 9 Planetary Geology: Earth and the Other Terrestrial Worlds 9.1 Connecting Planetary Interiors and Surfaces Our goals for learning What are terrestrial planets like on the inside? What causes geological

More information

Image of the Moon from the Galileo Space Craft

Image of the Moon from the Galileo Space Craft Image of the Moon from the Galileo Space Craft Moon: Overview Due to its size (diameter 3476 km, Mercury s diameter is 4880 km) and composition, the moon is sometimes considered as a terrestrial planet

More information

Unit 3 Lesson 4 The Terrestrial Planets. Copyright Houghton Mifflin Harcourt Publishing Company

Unit 3 Lesson 4 The Terrestrial Planets. Copyright Houghton Mifflin Harcourt Publishing Company Florida Benchmarks SC.8.N.1.5 Analyze the methods used to develop a scientific explanation as seen in different fields of science. SC.8.E.5.3 Distinguish the hierarchical relationships between planets

More information

Mercury and Venus 3/20/07

Mercury and Venus 3/20/07 Announcements Reading Assignment Chapter 13 4 th Homework due today Quiz on Thursday (3/22) Will cover all material since the last exam. This is Chapters 9-12 and the part of 13 covered in the lecture

More information

Quiz 3 is available for pickup in front

Quiz 3 is available for pickup in front Quiz 3 is available for pickup in front Extra credit corrections: for up to 4 of the questions you missed: Look up or figure out the correct answer. Write a sentence or two explaining what you did wrong

More information

Physics Homework Set 3 Fall 2015

Physics Homework Set 3 Fall 2015 1) Mercury presents the same side to the Sun 1) A) every third orbit. B) every 12 hours. C) all the time, just like our Moon. D) every other orbit. E) Twice every orbit. 2) Both the Moon and Mercury are

More information

Red Planet Mars. Chapter Thirteen

Red Planet Mars. Chapter Thirteen Red Planet Mars Chapter Thirteen ASTR 111 003 Fall 2006 Lecture 11 Nov. 13, 2006 Introduction To Modern Astronomy I Introducing Astronomy (chap. 1-6) Planets and Moons (chap. 7-17) Ch7: Comparative Planetology

More information

Mars. Mars is the fourth planet from the Sun and the outermost of the four terrestrial worlds in the Solar System. It lies outside Earth s orbit.

Mars. Mars is the fourth planet from the Sun and the outermost of the four terrestrial worlds in the Solar System. It lies outside Earth s orbit. Mars Mars is the fourth planet from the Sun and the outermost of the four terrestrial worlds in the Solar System. It lies outside Earth s orbit. Mars s orbital eccentricity is 0.093, much larger than that

More information

Life in the Universe. Key Concepts: Lecture 35: Admin. 11/21/17. All Formulae (for final):

Life in the Universe. Key Concepts: Lecture 35: Admin. 11/21/17. All Formulae (for final): Admin. 11/21/17 Key Concepts: Lecture 35: 1. Class website http://www.astro.ufl.edu/~jt/teaching/ast1002/ 2. Optional Discussion sections: Tue. ~11.30am (period 5), Bryant 3; Thur. ~12.30pm (end of period

More information

Overview of Solar System

Overview of Solar System Overview of Solar System The solar system is a disk Rotation of sun, orbits of planets all in same direction. Most planets rotate in this same sense. (Venus, Uranus, Pluto are exceptions). Angular momentum

More information

Lecture #10: Plan. The Moon Terrestrial Planets

Lecture #10: Plan. The Moon Terrestrial Planets Lecture #10: Plan The Moon Terrestrial Planets Both Sides of the Moon Moon: Direct Exploration Moon: Direct Exploration Moon: Direct Exploration Apollo Landing Sites Moon: Apollo Program Magnificent desolation

More information

The Main Point. Basic Properties of Mars. Observations. Lecture #19: Mars

The Main Point. Basic Properties of Mars. Observations. Lecture #19: Mars Mars: Overview General properties Telescopic observations Space missions Atmospheric Characteristics Reading: Chapters 7.1 (Mars), 9.4, 10.4 Lecture #19: Mars The Main Point Changes in the Martian surface

More information

Chapter 9 Lecture. The Cosmic Perspective Seventh Edition. Planetary Geology: Earth and the Other Terrestrial Worlds Pearson Education, Inc.

Chapter 9 Lecture. The Cosmic Perspective Seventh Edition. Planetary Geology: Earth and the Other Terrestrial Worlds Pearson Education, Inc. Chapter 9 Lecture The Cosmic Perspective Seventh Edition Planetary Geology: Earth and the Other Terrestrial Worlds Planetary Geology: Earth and the Other Terrestrial Worlds 9.1 Connecting Planetary Interiors

More information

Opposition and Conjunction

Opposition and Conjunction Opposition and Conjunction Summary 1. Mars is 52% further the Sun having an orbital period of nearly 2 Earth years 2. Mars is much smaller than the Earth being roughly 53% the size, 11% the mass of the

More information

Welcome to Class 12: Mars Geology & History. Remember: sit only in the first 10 rows of the room

Welcome to Class 12: Mars Geology & History. Remember: sit only in the first 10 rows of the room Welcome to Class 12: Mars Geology & History Remember: sit only in the first 10 rows of the room What are we going to discuss today? How easily could humans live on Mars? Is there water on Mars? PRS: If

More information

MARS. The Red Planet

MARS. The Red Planet MARS The Red Planet About the Planet Common Name: Mars Mythological Name(s): - Greek: Ares - Roman: Mars Mars is named after the Roman God of War A few Pictures... Distance, Size, and Gravity Compared

More information

Name. Physical Science Astronomy Exam II. Questions 1-18 have to do with the terrestrial planets, choose your answer from the list below:

Name. Physical Science Astronomy Exam II. Questions 1-18 have to do with the terrestrial planets, choose your answer from the list below: Name Physical Science 113 - Astronomy Exam II Questions 1-18 have to do with the terrestrial planets, choose your answer from the list below: 1. The smallest terrestrial planet. A) Mercury B) Venus C)

More information

Learning Objectives. they differ in density (composition, core), atmosphere, surface age, size, geological activity, magnetic field?

Learning Objectives. they differ in density (composition, core), atmosphere, surface age, size, geological activity, magnetic field? Mercury and Venus Learning Objectives! Contrast the Earth, the Moon, Venus and Mercury. Do they differ in density (composition, core), atmosphere, surface age, size, geological activity, magnetic field?!

More information

This evening s announcements

This evening s announcements This evening s announcements Homework 3 is graded and available for pickup at entry Quiz 4 will be held this Wednesday, March 12. Coverage: Feb. 25: origin of the solar system (chapter 6) Feb. 27: Earth,

More information

Exam# 2 Review. Exam #2 is Wednesday November 8th at 10:40 AM in room FLG-280

Exam# 2 Review. Exam #2 is Wednesday November 8th at 10:40 AM in room FLG-280 Exam# 2 Review Exam #2 is Wednesday November 8th at 10:40 AM in room FLG-280 Bring Gator 1 ID card Bring pencil #2 with eraser No use of calculator or any electronic device during the exam We provide the

More information

Terrestrial Atmospheres

Terrestrial Atmospheres Terrestrial Atmospheres Why Is There Air? An atmosphere is a layer of gas trapped by the gravity of a planet or moon. Here s Earth s atmosphere viewed from orbit: Why Is There Air? If atoms move faster

More information

DeAnza College Fall 2017 Third Midterm Exam. 1. Use only a #2 pencil on your Parscore sheet, and fill in the bubbles darkly and completely.

DeAnza College Fall 2017 Third Midterm Exam. 1. Use only a #2 pencil on your Parscore sheet, and fill in the bubbles darkly and completely. FAMILY NAME : (Please PRINT!) GIVEN NAME : (Please PRINT!) Signature: ASTRONOMY 4 DeAnza College Fall 2017 Third Midterm Exam Instructions: 1. Use only a #2 pencil on your Parscore sheet, and fill in the

More information

ASTRO 120 Sample Exam

ASTRO 120 Sample Exam ASTRO 120 Sample Exam 1) If a planet has a reasonably strong magnetic field, we know that a. It is made entirely of iron b. There is liquid nitrogen below the surface c. It can harbor life d. It has a

More information

What You Already Know

What You Already Know Mars: The Red Planet What You Already Know The Sun is a star, a huge ball of very hot gas that gives off energy. Our Sun is an average star. It is located at the center of the solar system, which consists

More information

PTYS/ASTR Section 2 - Spring 2007 Practice Exam 2

PTYS/ASTR Section 2 - Spring 2007 Practice Exam 2 PTYS/ASTR 206 - Section 2 - Spring 2007 Practice Exam 2 Note: The exam is scheduled for Thursday, March 29, 2007. It will be held in-class; you will have 75 minutes to finish the exam, though many of you

More information

The Solar System 6/23

The Solar System 6/23 6/23 The Solar System I. Earth A. Earth is the prototype terrestrial planet 1. Only planet in the solar system (we know of so far) with life 2. Temperature 290 K B. Physical Characteristics 1. Mass: 6

More information

2. Terrestrial Planet G 9. Coulomb Force C 16. Babcock model Q. 3. Continuous Spectrum K 10. Large-impact hypothesis I 17.

2. Terrestrial Planet G 9. Coulomb Force C 16. Babcock model Q. 3. Continuous Spectrum K 10. Large-impact hypothesis I 17. Astronomy 1 S 16 Exam 1 Name Identify terms Label each term with the appropriate letter of a definition listed 1. Spectral line R 8. Albedo H 15. helioseismology E 2. Terrestrial Planet G 9. Coulomb Force

More information

Hubble Telescope Picture of Mars

Hubble Telescope Picture of Mars Information of Mars Mars is the fourth planet from the Sun and is commonly referred to as the Red Planet. The rocks and soil have a red or pink hue due to the iron oxiode (rust) they contain. Hubble Telescope

More information

Earth, the Lively* Planet. * not counting the life on the planet!

Earth, the Lively* Planet. * not counting the life on the planet! Earth, the Lively* Planet * not counting the life on the planet! What We Will Learn Today What are planet Earth s features? What processes shape planetary surfaces? How does Earth s surface move? How did

More information

Lecture 10: Terrestrial planets. Astronomy 111 Monday October 2, 2017

Lecture 10: Terrestrial planets. Astronomy 111 Monday October 2, 2017 Lecture 10: Terrestrial planets Astronomy 111 Monday October 2, 2017 Reminders Online homework #5 due Monday at 3pm Terrestrial Planets ASTR111 Lecture 10 Terrestrial planets Mercury Venus Earth Mars The

More information

Astronomy Ch. 10 Mars Review. MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question.

Astronomy Ch. 10 Mars Review. MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. Name: Period: Date: Astronomy Ch. 10 Mars Review MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. 1) Why was the summer of 2003 a fine time for Mars

More information

I always wanted to be somebody, but I should have been more specific. Lilly Tomlin Reading has been updated. (All of Chaps. 9& 10) Friday, first sit

I always wanted to be somebody, but I should have been more specific. Lilly Tomlin Reading has been updated. (All of Chaps. 9& 10) Friday, first sit I always wanted to be somebody, but I should have been more specific. Lilly Tomlin Reading has been updated. (All of Chaps. 9& 10) Friday, first sit for passing back HW, then with chart. Water on the Moon?

More information

Astronomy 1 Fall 2016

Astronomy 1 Fall 2016 Astronomy 1 Fall 2016 Announcements: 1. Midterm exam on Thursday (in this room) 2. Oct 21 st - 26 th : Sections replaced by evening observing) Lecture 8: October 18, 2016 Previously on Astro 1 Solar System

More information

Mars s atmosphere. continued. Dust devil on as seen by rover Spirit 3/27/07

Mars s atmosphere. continued. Dust devil on as seen by rover Spirit 3/27/07 Mars continued Mars s atmosphere Dust devil on as seen by rover Spirit Announcements Reading Assignment for 1 st lecture after the exam Chapter 14 All previous assignments have been graded and handed back

More information

Astronomy 1140 Quiz 3 Review

Astronomy 1140 Quiz 3 Review Astronomy 1140 Quiz 3 Review Anil Pradhan October 27, 2017 I The Inner Planets 1. What are the terrestrial planets? What do they have in common? Terrestrial planets: Mercury, Venus, Earth, Mars. Theses

More information

Mars Opposition Friday 27 th July 2018

Mars Opposition Friday 27 th July 2018 Mars Opposition Friday 27 th July 2018 Mars is about 6,780 kilometres in diameter or roughly half the size of the Earth whose diameter is 12,742km. As they orbit the Sun, the minimum distance between the

More information

Inner Planets (Part II)

Inner Planets (Part II) Inner Planets (Part II) Sept. 18, 2002 1) Atmospheres 2) Greenhouse Effect 3) Mercury 4) Venus 5) Mars 6) Moon Announcements Due to technical difficulties, Monday s quiz doesn t count An extra credit problem

More information

Astronomy 1140 Quiz 3 Review

Astronomy 1140 Quiz 3 Review Astronomy 1140 Quiz 3 Review Anil Pradhan October 26, 2016 I The Inner Planets 1. What are the terrestrial planets? What do they have in common? Terrestrial planets: Mercury, Venus, Earth, Mars. Theses

More information

9. Moon, Mercury, Venus

9. Moon, Mercury, Venus 9. Moon, Mercury, Venus All the heavier elements were manufactured by stars later, either by thermonuclear fusion reactions deep in their interiors or by the violent explosions that mark the end of massive

More information

UNIT 3: Chapter 8: The Solar System (pages )

UNIT 3: Chapter 8: The Solar System (pages ) CORNELL NOTES Directions: You must create a minimum of 5 questions in this column per page (average). Use these to study your notes and prepare for tests and quizzes. Notes will be turned in to your teacher

More information

Geologic Features of Mars

Geologic Features of Mars Name Purpose Geologic Features of Mars To learn to identify landforms on the surface of Mars and the geological processes that produced them. Introduction In many ways, Mars is similar to Earth. The same

More information

7.1 Earth as a Planet 7.2 Mercury and the Moon 7.3 Mars 7.4 Venus 7.5 Earth as a Living Planet

7.1 Earth as a Planet 7.2 Mercury and the Moon 7.3 Mars 7.4 Venus 7.5 Earth as a Living Planet Chapter 7: Earth and the Terrestrial Worlds 7.1 Earth as a Planet 7.2 Mercury and the Moon 7.3 Mars 7.4 Venus 7.5 Earth as a Living Planet All picture credits: 2015 Pearson Education, Inc unless stated

More information

Today. Events. Terrestrial Planet Atmospheres (continued) Homework DUE. Review next time? Exam next week

Today. Events. Terrestrial Planet Atmospheres (continued) Homework DUE. Review next time? Exam next week Today Terrestrial Planet Atmospheres (continued) Events Homework DUE Review next time? Exam next week Planetary Temperature A planet's surface temperature is determined by the balance between energy from

More information

The Inner Planets. Chapter 3 Lesson 1. Pages Workbook pages 51-52

The Inner Planets. Chapter 3 Lesson 1. Pages Workbook pages 51-52 The Inner Planets Chapter 3 Lesson 1 Pages 152-159 Workbook pages 51-52 Create the Foldable on pg 159 The solar The planets system The four inner planets Compare and Contrast Question What are planets?

More information

How can solid rock be bent, squished, stretched, and cracked?

How can solid rock be bent, squished, stretched, and cracked? AST 105 Intro Astronomy The Solar System MIDTERM II: Tuesday, April 5 4 Processes that Shape Surfaces Volcanism Eruption of molten rock onto surface Impact cratering Impacts by asteroids or comets Tectonics

More information

ASTR 380 Possibilities for Life in the Inner Solar System

ASTR 380 Possibilities for Life in the Inner Solar System ASTR 380 Possibilities for Life in the Inner Solar System ASTR 380 Midterm Test Results Generally people did well: 100-90 = A = 19 people 89 80 = B = 19 people 79 70 = C = 9 people 69 60 = D = 0 < 60 =

More information

The Moon. Tides. Tides. Mass = 7.4 x 1025 g = MEarth. = 0.27 REarth. (Earth 5.5 g/cm3) Gravity = 1/6 that of Earth

The Moon. Tides. Tides. Mass = 7.4 x 1025 g = MEarth. = 0.27 REarth. (Earth 5.5 g/cm3) Gravity = 1/6 that of Earth The Moon Mass = 7.4 x 1025 g = 0.012 MEarth Radius = 1738 km = 0.27 REarth Density = 3.3 g/cm3 (Earth 5.5 g/cm3) Gravity = 1/6 that of Earth Dark side of the moon We always see the same face of the Moon.

More information

Announcements. NRAO REU program Feb 1, summerstudents

Announcements. NRAO REU program Feb 1, summerstudents Announcements NRAO REU program Feb 1, 2019 https://science.nrao.edu/opportunities/student-programs/ summerstudents AFRL Scholars program Jan 16, 2019 https://afrlscholars.usra.edu HW#8 due Nov 1 Test#2

More information

Outline 9: Origin of the Earth: solids, liquids, and gases

Outline 9: Origin of the Earth: solids, liquids, and gases Outline 9: Origin of the Earth: solids, liquids, and gases The Early Archean Earth Origin of Earth s Matter The earth is made of recycled elements formed in stars that existed prior to our Sun. Supernova

More information

Geology of the terrestrial planets Pearson Education, Inc.

Geology of the terrestrial planets Pearson Education, Inc. Geology of the terrestrial planets 2014 Pearson Education, Inc. Earth s Bulk Properties Earth s Bulk Properties albedo - A = 0.39 A = 0 planet absorbs all sunlight that hits it A =1 planet reflects all

More information

Jovian Planets Jupiter, Saturn, Uranus and Neptune

Jovian Planets Jupiter, Saturn, Uranus and Neptune The Inner Planets The Inner Planets Terrestrial Planets Mercury, Venus, Earth and Mars Rocky Surfaces No rings No or Few Moons Jovian Planets Jupiter, Saturn, Uranus and Neptune Gas Surfaces rings Many

More information

Today. Events. Terrestrial Planet Geology. Fall break next week - no class Tuesday

Today. Events. Terrestrial Planet Geology. Fall break next week - no class Tuesday Today Terrestrial Planet Geology Events Fall break next week - no class Tuesday When did the planets form? We cannot find the age of a planet, but we can find the ages of the rocks that make it up. We

More information

Examining the Terrestrial Planets (Chapter 20)

Examining the Terrestrial Planets (Chapter 20) GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: Examining the Terrestrial Planets (Chapter 20) For this assignment you will require: a calculator, colored pencils, a metric ruler, and your geology

More information

Distance of Mercury to the Sun or the Orbital Radius

Distance of Mercury to the Sun or the Orbital Radius Distance of Mercury to the Sun or the Orbital Radius The minimum distance from the Sun to Mercury is about 45866304 kilometers and the maximum distance is about 70006464 kilometers. Space Station One Day

More information

Lecture Outlines. Chapter 8. Astronomy Today 7th Edition Chaisson/McMillan Pearson Education, Inc.

Lecture Outlines. Chapter 8. Astronomy Today 7th Edition Chaisson/McMillan Pearson Education, Inc. Lecture Outlines Chapter 8 Astronomy Today 7th Edition Chaisson/McMillan Chapter 8 The Moon and Mercury Units of Chapter 8 8.1 Orbital Properties 8.2 Physical Properties 8.3 Surface Features on the Moon

More information

Lesson 2 The Inner Planets

Lesson 2 The Inner Planets Lesson 2 Student Labs and Activities Page Launch Lab 25 Content Vocabulary 26 Lesson Outline 27 MiniLab 29 Content Practice A 30 Content Practice B 31 School to Home 32 Key Concept Builders 33 Enrichment

More information

The Classification of Galaxies

The Classification of Galaxies Admin. 11/9/17 1. Class website http://www.astro.ufl.edu/~jt/teaching/ast1002/ 2. Optional Discussion sections: Tue. ~11.30am (period 5), Bryant 3; Thur. ~12.30pm (end of period 5 and period 6), start

More information

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

Starting from closest to the Sun, name the orbiting planets in order. Chapter 9 Section 1: Our Solar System Solar System: The solar system includes the sun, planets and many smaller structures. A planet and its moon(s) make up smaller systems in the solar system. Scientist

More information

The Moon & Mercury: Dead Worlds

The Moon & Mercury: Dead Worlds The Moon & Mercury: Dead Worlds There are many similarities between the Moon and Mercury, and some major differences we ll concentrate mostly on the Moon. Appearance of the Moon from the Earth We ve already

More information

Outline 9: Origin of the Earth: solids, liquids, and gases. The Early Archean Earth

Outline 9: Origin of the Earth: solids, liquids, and gases. The Early Archean Earth Outline 9: Origin of the Earth: solids, liquids, and gases The Early Archean Earth Origin of Earth s Matter The earth is made of recycled elements formed in stars that existed prior to our Sun. Supernova

More information

Admin. 8/29/17. If you re at North Pole, you ll NEVER see stars that are below your horizon. Key Concepts: Lecture 4

Admin. 8/29/17. If you re at North Pole, you ll NEVER see stars that are below your horizon. Key Concepts: Lecture 4 Admin. 8/29/17 1. Class website http://www.astro.ufl.edu/~jt/teaching/ast1002/ 2. Optional Discussion sections (start Aug. 30th) (see me at end of lecture if you can t make one of these times)! Tuesday

More information

Solar System B UT Regional 2018

Solar System B UT Regional 2018 Solar System B UT Regional 2018 Competitors: School Name: Team Number: This test contains 4 parts, worth 150 points in total. As always, you ll have 50 minutes to complete the test. You may separate the

More information

1 Describe the structure of the moon 2. Describe its surface features 3. Summarize the hypothesis of moon formation

1 Describe the structure of the moon 2. Describe its surface features 3. Summarize the hypothesis of moon formation Loulousis 1 Describe the structure of the moon 2. Describe its surface features 3. Summarize the hypothesis of moon formation moon -a body that revolves around a planet and that has less mass than the

More information

Space and Time Before Einstein. The Problem with Light. Admin. 11/2/17. Key Concepts: Lecture 28: Relativity

Space and Time Before Einstein. The Problem with Light. Admin. 11/2/17. Key Concepts: Lecture 28: Relativity Admin. 11/2/17 1. Class website http://www.astro.ufl.edu/~jt/teaching/ast1002/ 2. Optional Discussion sections: Tue. ~11.30am (period 5), Bryant 3; Thur. ~12.30pm (end of period 5 and period 6), start

More information

[17] Magnetic Fields, and long-term changes in climate (10/26/17)

[17] Magnetic Fields, and long-term changes in climate (10/26/17) 1 [17] Magnetic Fields, and long-term changes in climate (10/26/17) Upcoming Items 1. Read Chapter 11, do the self-study quizzes 2. Midterm #2 on Tuesday, November 7 On classes from Oct 5 through Oct 31

More information

page - Lab 13 - Introduction to the Geology of the Terrestrial Planets

page - Lab 13 - Introduction to the Geology of the Terrestrial Planets page - Lab 13 - Introduction to the Geology of the Terrestrial Planets Introduction There are two main families of planets in our solar system: the inner Terrestrial planets (Earth, Mercury, Venus, and

More information

Lecture 19. Outline. Outline For Rest of Semester. Mercury. Discuss Quiz Mercury Venus

Lecture 19. Outline. Outline For Rest of Semester. Mercury. Discuss Quiz Mercury Venus Lecture 19 iscuss Quiz Mercury Venus Outline Outline For Rest of Semester Oct. 29 th hapter 9 (Earth) Nov 3 rd and 5 th hapter 9 and hapter 10 (Earth and Moon) Nov. 10 th and 12 th hapter 11 (Mars, Venus,

More information

Mercury = Hermes Mythology. Planet Mercury, Element, Mercredi God of Commerce, Messenger God, guide to Hades Winged sandals and staff

Mercury = Hermes Mythology. Planet Mercury, Element, Mercredi God of Commerce, Messenger God, guide to Hades Winged sandals and staff Mercury = Hermes Mythology Planet Mercury, Element, Mercredi God of Commerce, Messenger God, guide to Hades Winged sandals and staff Mercury s Orbit Mercury never seen more than 28 from the sun Revolves/orbits

More information

Orbit of Mars. Exploration of Mars

Orbit of Mars. Exploration of Mars Mars 1 Orbit of Mars Exploration of Mars First visits were by Mariners 4, 6, and 7. A major step forward was achieved in 1971, when Mariner 9 became the first spacecraft to orbit another planet. The Mariner

More information

The Solar System. Tour of the Solar System

The Solar System. Tour of the Solar System The Solar System Tour of the Solar System The Sun more later 8 planets Mercury Venus Earth more later Mars Jupiter Saturn Uranus Neptune Various other objects Asteroids Comets Pluto The Terrestrial Planets

More information

Solar System B UT Regional 2018

Solar System B UT Regional 2018 Solar System B UT Regional 2018 Competitors: School Name: Team Number: This test contains 5 parts, worth 150 points in total. As always, you ll have 50 minutes to complete the test. You may separate the

More information

Motion of the planets

Motion of the planets Our Solar system Motion of the planets Our solar system is made up of the sun and the 9 planets that revolve around the sun Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune & Pluto (maybe?)

More information

The Terrestrial Planets

The Terrestrial Planets The Terrestrial Planets Large Bodies: Earth (1 R E, 1 M E ) Venus (0.95 R E, 0.82 M E ) Small Bodies: Mars (0.53 R E, 0.11 M E ) Mercury (0.38 R E, 0.055 M E ) Moon (0.27 R E, 0.012 M E ) The surfaces

More information

10/31/2010. Opposition and Conjunction. Opposition occurs every 2 years. Best opposition at perihelion. Percival Lowell

10/31/2010. Opposition and Conjunction. Opposition occurs every 2 years. Best opposition at perihelion. Percival Lowell Opposition and Conjunction Opposition occurs every 2 years Best opposition at perihelion Percival Lowell 1 Canals on Mars? Martians? Orson Welle s Broadcast (1938) The War of the Worlds H G Wells (1898)

More information

Astro 1010 Planetary Astronomy Sample Questions for Exam 4

Astro 1010 Planetary Astronomy Sample Questions for Exam 4 Astro 1010 Planetary Astronomy Sample Questions for Exam 4 Chapter 8 1. Which of the following processes is not important in shaping the surface of terrestrial planets? a) Impact cratering b) Tectonism

More information

SOLAR SYSTEM. planet feature cards

SOLAR SYSTEM. planet feature cards SOLAR SYSTEM planet feature cards PLANET space FEATURE grab bag CARDS The Largest Space Volcano Shuttle in Challenger Solar System explodes (Olympus 73 Mons) seconds after launch, causing a nearly three-year

More information

Lecture 19: The Moon & Mercury. The Moon & Mercury. The Moon & Mercury

Lecture 19: The Moon & Mercury. The Moon & Mercury. The Moon & Mercury Lecture 19: The Moon & Mercury The Moon & Mercury The Moon and Mercury are similar in some ways They both have: Heavily cratered Dark colored surfaces No atmosphere No water They also have some interesting

More information

For the next few weeks: Terrestrial Planets, their Moons, and the Sun. Planetary Surfaces and Interiors 2/20/07

For the next few weeks: Terrestrial Planets, their Moons, and the Sun. Planetary Surfaces and Interiors 2/20/07 For the next few weeks: Terrestrial Planets, their Moons, and the Sun Announcements Reading Assignment Section 9-1 (pp 186-189), 9-5 and 9-6 (pp 199-203) 3 rd Homework is now posted on the course website

More information

SOLAR SYSTEM NOTES. Scientists believe its at least 4.6 billion years old!!! 10/26/2017 ENERGY TRANSFERS RADIATION FROM THE SUN

SOLAR SYSTEM NOTES. Scientists believe its at least 4.6 billion years old!!! 10/26/2017 ENERGY TRANSFERS RADIATION FROM THE SUN SOLAR SYSTEM NOTES Our Solar System is composed of: 1. The Sun 2. The Planets 3. Asteroids 4. Comets 5. Meteors 6. Natural & Artificial satellites Remember: How old is our Solar System? Scientists believe

More information

The Cosmic Perspective Planetary Atmospheres: Earth and the Other Terrestrial Worlds

The Cosmic Perspective Planetary Atmospheres: Earth and the Other Terrestrial Worlds Chapter 10 Lecture The Cosmic Perspective Seventh Edition Planetary Atmospheres: Earth and the Other Terrestrial Worlds Planetary Atmospheres: Earth and the Other Terrestrial Worlds 10.1 Atmospheric Basics

More information

Planetary Atmospheres (Chapter 10)

Planetary Atmospheres (Chapter 10) Planetary Atmospheres (Chapter 10) Based on Chapter 10 This material will be useful for understanding Chapters 11 and 13 on Jovian planet systems and Extrasolar planets Chapters 4, 5, and 8 on Momentum,

More information

Ronald Wilhelm & Jennifer Wilhelm, University of Kentucky Ages on Mars. Martian Surface Age Exploration

Ronald Wilhelm & Jennifer Wilhelm, University of Kentucky Ages on Mars. Martian Surface Age Exploration Ronald Wilhelm & Jennifer Wilhelm, University of Kentucky 2008 Ages on Mars Martian Surface Age Exploration You have now learned some very important things about various planets and moons in our Solar

More information

The Planets, Asteroids, Moons, etc.

The Planets, Asteroids, Moons, etc. DATE DUE: Ms. Terry J. Boroughs Geology 305 Name: Section: The Planets, Asteroids, Moons, etc. Instructions: Read each question carefully before selecting the BEST answer or option. Use GEOLOGIC vocabulary

More information

Lecture 11 The Structure and Atmospheres of the Outer Planets October 9, 2017

Lecture 11 The Structure and Atmospheres of the Outer Planets October 9, 2017 Lecture 11 The Structure and Atmospheres of the Outer Planets October 9, 2017 1 2 Jovian Planets 3 Jovian Planets -- Basic Information Jupiter Saturn Uranus Neptune Distance 5.2 AU 9.5 AU 19 AU 30 AU Spin

More information

PLATO - 4. The terrestrial planets, planetology

PLATO - 4. The terrestrial planets, planetology PLATO - 4 The terrestrial planets, planetology 1 Disk Formation Why does the contracting cloud form a disk?! As matter rotates faster and faster, it feels more and more centrifugal force, resisting gravity!

More information

If your plan is for one year, plant rice. If your plan is for 100 years, educate children. Confucius

If your plan is for one year, plant rice. If your plan is for 100 years, educate children. Confucius If your plan is for one year, plant rice. If your plan is for 100 years, educate children. Confucius Test 1 on Wednesday Feb. 20. Sample test and review are On the course web page now. Grades are there

More information

Earth. Physical Properties of Earth kg. Average Density g/cm 2. Surface Gravity 9.8 m/s o C to 50 o C. Surface Temperature

Earth. Physical Properties of Earth kg. Average Density g/cm 2. Surface Gravity 9.8 m/s o C to 50 o C. Surface Temperature Earth Physical Properties of Earth Equatorial Diameter Mass 12,756 km 5.976 10 24 kg Average Density 5.497 g/cm 2 Surface Gravity 9.8 m/s 2 Escape Velocity Surface Temperature 11.2 km/s -50 o C to 50 o

More information