Examining the Terrestrial Planets (Chapter 20)

Size: px
Start display at page:

Download "Examining the Terrestrial Planets (Chapter 20)"

Transcription

1 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 305 textbook as a reference. Objectives for chapter 20: After you have completed this exercise, you should be able to: 1. List and describe the geologic processes that have shaped the landforms of the terrestrial planets; 2. Give an example of a feature on Earth or the Moon produced by each of the geologic processes that have shaped the landforms of the terrestrial planets; 3. List the primary geologic processes that have shaped the landforms of each of the terrestrial planets; 4. Describe the procedure for determining the relative ages of a planet s surface features. The following questions refer to Chapter 20, (PAGES IN YOUR MANUAL, 7 th Ed.) or (Pages in your manual, 8 th edition) (Read the questions from your manual and place your answers in the following spaces provided.) 1. Identify the geologic processes that modified the landscapes of the Earth and the Moon depicted in the following figures and/or photographs. The processes involve include the following: Volcanism, Tectonism (evidence of plate tectonics), Gradation (leveling of the surface due to erosion and deposition), and Impact Cratering. Figures and/or photographs Fig A & B Identify the geologic processes that modified these surfaces and/or landscapes (use Volcanism, Tectonism, Gradation, or Impact cratering Fig Fig & 20.4 Fig Fig A Smooth, dark areas of central figure in Fig Indicate the agent of gradation and/or specific process (if known) that is responsible for the feature the following figures: Figures and/or photographs Identify the agent of gradation and/or specific process (if known) that is responsible for the feature Inside the crater of Fig A Fig Fig Impact craters and volcanoes can both have craters. One has its crater rim along the ground s surface, whereas the other has its crater up atop a cone. The crater rim for an impact site is typically located: The crater rim for a volcano is typically located: Instructor: Ms. Terry J. Boroughs 1

2 4. Meteor Crater, Figure 20.5, has a diameter of approximately 1,200 meters. It is estimated that the object that produced it was about 25 meters across. How may times greater is the size of the crater than the object that produced it? Such a small object can produce such a large crater due to (high velocity, high momentum, high mass, or a combination of all of these.) (Pick the best answer.) 5. Despite being one of the best-preserved and youngest impact craters on Earth, Meteor Crater, Figure 20.5, shows signs or erosion. Do you see signs of weathering and erosion in the form of dry stream channels cutting through the rim of the crater, or debris from rock falls and/or rock slides at the base of the crater walls, or do you see a combination of both? 6. Which Lunar feature (figure 20.6 a, b, c, or d) most resembles Meteor Crater? 8. How are the surfaces of Mercury and the Moon similar? (What do they have in common?) 9. Figure 20.7A shows a close-up view of a portion of Mercury s surface. It is similar to certain features found on the Moon. Which figure of the Moon (Figure 20.6 A, B, C, or D) shows a feature similar to figure 20.7A? (Pick the best answer.) 10. Figure 20.7B shows a close-up view of a portion of Mercury s surface. It is similar to certain features found on the Moon. Which figure of the Moon (Figure 20.6 A, B, C, or D) shows a feature similar to figure 20.7B? (Pick the best answer.) 11. Of the four processes that alter a planet s surface, which one the most effective on Mercury? (In other words, which process is readily visible or common on the surface of Mercury?) 12. Why does Mercury show little evidence of erosion due to running water, wind, or ice? 13. Choosing from the processes that act on a planet s surface, (volcanism, tectonism, gradation, impact cratering) write the name of the process that is most likely responsible for the features in the following figures on Mercury. Be specific, for example, Gradation wind vs. Gradation ice. Figure 20.7 A: Figure 20.7 D (flat areas in lower left corner): Instructor: Ms. Terry J. Boroughs 2

3 14. Using these images of Mercury, figure 20.7C notice the trace of a cliff-like structure that has offset more than 1.6 kilometers (1 mile). Which of the four major geologic processes (volcanism, impact cratering, gradation, or tectonism) created this structure? (Pick the best answer.) 15. Using the full-disk image of Venus and the smaller images in Figure 20.8, do you see any of the following processes (volcanism, impact cratering, gradation, or tectonism) evident on the surface of Venus? Tectonism in the form of fracturing or faulting (yes or no): Volcanism (yes or no): Impact cratering (yes or no): Gradation (yes or no): If yes, what type(s)? 16. Choosing from the processes that act on a planet s surface, (volcanism, tectonism, gradation, impact cratering) write the name of the process that is most likely responsible for the following features (volcanism, impact cratering, gradation, or tectonism) evident on the surface of Venus? Figure 20.8 A: Figure 20.8 B: Figure 20.8 C: Figure 20.8 D: 17. In radar images, smooth surfaces appear darker, and rough, multi-faceted surfaces appear bright. These differences are not due to compositional differences like seen on the Moon, but instead due to the effects of weathering, erosion, etc. Do you think that the smooth surfaces are (Older or younger?) Pick one. Do you think that the rough surfaces are (Older or younger?) Pick one. 18. The gradational agent responsible for the feature in Figure 20.8 D is: 19. A. Is the central feature in Figure 20.8 C younger or older than the surrounding landscape? B. What type of structure is this feature? A. B. 20. The bright areas on the central global view of Venus (figure 20.8) show highly fractured ridges and canyons of the Aphrodite highlands. What geologic process produced these features: (volcanism, tectonic activity, gradation, or impact cratering)? (Pick the best answer.) Instructor: Ms. Terry J. Boroughs 3

4 21. Approximately 1000 impact craters have been identified on the surface of Venus. Do think this is (more or less) than the number on the surface of Mercury? 22. Identify the geologic processes that modified the landscapes of Mars depicted in the following figures and/or photographs. The processes involve include the following: Volcanism, Tectonism (evidence of plate tectonics), Gradation (leveling of the surface due to erosion and deposition), and Impact Cratering. Figures and/or photographs Fig A Fig B Fig C Fig E Identify the geologic processes that modified these surfaces and/or landscapes (use Volcanism, Tectonism, Gradation, or Impact cratering 23. Using the full-disk and the smaller images of Mars in or figure 20.9, do you see any of the following processes (volcanism, impact cratering, gradation, or tectonism) evident on the surface of Mars? Tectonism in the form of fracturing or faulting (yes or no): Volcanism (yes or no): Gradation (yes or no): Impact cratering (yes or no): If yes, what type(s)? 24. How does the Martian surface compare to the surfaces of Mercury and the Moon in regards to crater density (the number of craters in a given area)? Does Mars have more or fewer craters than Mercury? 25. Choosing from the gradational processes that act on the surface of Mars, write the name of the process that is most likely responsible for the features in the following figures. Be specific, for example, Gradation wind vs. Gradation ice. Figure 20.9 A: Figure 20.9 E: 26. The long linear feature near the center of the full-disk image of Mars is Valles Marineris, a large canyon system. Do you think Valles Marineris is (larger or smaller) than the Grand Canyon located in the U.S. (Pick the best answer.) 27. Do you think that Valles Marineris may have formed from tectonic activity? Do you think this tectonic activity is currently active? Instructor: Ms. Terry J. Boroughs 4

5 28. Because the subsurface of some regions on Mars contains abundant ice, impacts often generate ejecta with a mud-like consistency. Do you think the impact crater shown in figure 20.9 B exhibits this type of ejecta pattern? (yes or no) 29. Using Figure 20.9 C, Olympus Mons is one of four huge volcanoes in a region called Tharsis. Compare the surface of Olympus Mons to the surface of Mercury and the lighter regions of the Moon. Is the surface of Olympus Mons geologically (young, old, or about the same age) as the surfaces of Mercury and the lighter regions of the Moon? (Pick the best answer.) 30. Using Figure 20.6 Describe the origin and/or characteristics of the Lunar Maria and Lunar Highlands. Highlands: Maria: 31. Rocks brought back from the lunar Maria during the Apollo landings are about billion years old. Therefore, are the lunar highlands (older or younger) than billion years. (Pick the best answer.) 32. List these lunar features in order, from youngest to oldest: maria, highlands, rayed craters. Youngest: Middle: Oldest: 33. Are the rayed craters older or younger than the area around them? (Pick the best answer.) 34. Based upon the density of craters, the surface of Mars appears to be (older, younger, about the same age) as the Moon s highlands and (older, younger, about the same age) as the surface of Mercury. Write your answers here, don t circle them. 35. Considering its history, describe how the surface of Mercury is likely to change during the next billion years. 36. On a global scale, which planet looks more like Venus: Mercury or Mars? 37. Place the four terrestrial planets and our moon into sequence from the youngest, most modified surface to the oldest, less modified surface. Youngest: :Oldest Instructor: Ms. Terry J. Boroughs 5

6 38. Of the four terrestrial planets which is the: Most active: Least Active: 39. Using figure Compare the southern half of the photograph to the northern half. Which surface is younger? Northern ½ or Southern ½ is younger? How did you know? 40. Using figure 20.12, How do you know that the craters in the Southern ½ are of various ages? Extra Credit Questions from page or 339 (Summary / Report Page for chapter 20): 1. What are the four major geologic processes that have shaped the surfaces of the terrestrial planets and the Moon? Give examples of landforms produced by these processes. Process: Example landform: Process: Process: Process: Example landform: Example landform: Example landform: 2. The surface of the Moon most resembles the surface of (Mercury, Venus, or Earth) whereas the surface of Venus is similar to that of (Earth or Mars)? 3. Which planet s surface has been mapped exclusively by Radar? Why is radar mapping used? 4. List the most significant geologic processes that shape or has shaped the surface of each of the terrestrial planets and the Moon. Most significant process on Mercury: Most significant process on Venus: Most significant process on Earth: Most significant process on Moon: Most significant process on Mars: Instructor: Ms. Terry J. Boroughs 6

7 5. Of the major gradational agents, (running water, gravity, wind, or ice) is the only one that alters the surface of all the terrestrial planets? (I.e. all terrestrial planets exhibit this gradational agent. (Pick the best answer.) 6. Using images from Mars figure (B), do you think that these elongate and irregular features were produced by gradation and if so, specify the type of gradational process involved. 7. Briefly describe how the relative ages of various planetary surfaces can be determined. (I.E. what type of features or surface characteristics would indicate older surfaces vs. younger surfaces? Examining the Terrestrial Planets Lab Supplement 1. Tectonism / Tectonic activity A. Involves the movement of crustal rock by fracturing, faulting, or folding B. Can exhibit the following: Linear or gently curving factures and/or faults Fault scarps Folded terrain Mountain belts, mountain ranges Linear ridges 2. Volcanism A. Volcanism is the eruption of molten rock material (magma) and its associated gases, ash, etc. onto a planet s surface. B. Can exhibit the following: Steep, conical hills with summit craters or large caldera Calderas form as a result of summit collapse and may exhibit fractures in a concentric ring shape. Lava flows which can produce a lobe-shaped deposit with an undulating surface. Lava flows that fill craters and leave behind a smooth surface 3. Impact Cratering A. Impact craters are the consequence of rapidly moving meteorites and/or asteroids that strike the surface of a planet. B. Can exhibit the following: Central peaks or pinnacles in the center of the crater Ejecta blankets Ejecta rays Ringed crater rims Overturned crater rims Overlapping crater rims Crater chains, etc. Instructor: Ms. Terry J. Boroughs 7

8 4. Gradation A. The process that levels a surface to a common elevation by erosion and deposition is controlled by the surface environment. Gravity, temperature, and the presence of an atmosphere all play key roles. B. The major agents of gradation include the following: Running water Eroded stream channels Delta deposits Alluvial fans Lake sediments Ocean sediments, beaches, etc Gravity Wind Ice Materials become eroded and fall, flow, etc. due to the influence of gravity and include: Talus slopes (material collecting at the base of a steep surface, such as a cliff face or the walls of an impact crater Landslides, mudflows, avalanches, etc. often triggered by excess water Crater rims will become eroded and debris will start to fill the crater with eroded material, often burying the central peak, which can also become eroded All of the terrestrial planets have mass and therefore gravity!!! Wind requires and active atmosphere Typically only the fine-grained particles will be carried by the wind May produce wavy sand dunes May produce streaks of sediment when the wind carries some of the ejecta material in one direction, following an impact by a meteorite Requires the presence of water and other atmospheric compounds Ice is often very reflective and may appear white in pictures Ice and glaciers are very effective for scouring a surface flat and evening out the landscape. Often found closer to the polar regions of the Earth. Instructor: Ms. Terry J. Boroughs 8

ESCI 110: Planetary Surfaces Page 3-1. Exercise 3. Surfaces of the Planets and Moons

ESCI 110: Planetary Surfaces Page 3-1. Exercise 3. Surfaces of the Planets and Moons ESCI 110: Planetary Surfaces Page 3-1 Introduction Exercise 3 Surfaces of the Planets and Moons Our knowledge of the solar system has exploded with the space exploration programs of the last 40 years.

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

COSMORPHOLOGY - May 2009

COSMORPHOLOGY - May 2009 Name COSMORPHOLOGY - May 2009 Geologic landforms Purpose: By studying aerial photographs you will learn to identify different kinds of geologic features based on their different morphologies and learn

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

Geologic Landforms Seen on Aerial Photos Instructor Notes

Geologic Landforms Seen on Aerial Photos Instructor Notes 1.5 hours Exercise Two Geologic Landforms Instructor Notes Suggested Correlation of Topics Geomorphology, gradation, impact cratering, tectonism, volcanism, photography Purpose The objective of this exercise

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 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

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

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

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

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

Photogeologic Mapping of Mars

Photogeologic Mapping of Mars Exercise Two and Fifteen are suggested as introductory exercises. 2.0 hours Exercise Seventeen Photogeologic Mapping of Mars Instructor Notes Suggested Correlation of Topics Deductive reasoning, geologic

More information

Moon 101. By: Seacrest School Moon Crew Blake Werab David Prue

Moon 101. By: Seacrest School Moon Crew Blake Werab David Prue Moon 101 By: Seacrest School Moon Crew Blake Werab David Prue The 101 images The smooth Mare surfaces common on the nearside of the Moon Mare Surfaces from Late heavy Bombardment We find that the 3 images

More information

Extraterrestrial Volcanism

Extraterrestrial Volcanism Extraterrestrial Volcanism What does it take to create volcanic activity? How do different planetary conditions influence volcanism? Venus Volcanism in our solar system. Io Europa Mercury Venus Earth/Moon

More information

Highs and Lows Floods and Flows

Highs and Lows Floods and Flows Highs and Lows Floods and Flows Planetary Mapping Facilitator Guide Becky Nelson Education Specialist The Lunar and Planetary Institute Highs and Lows, Floods and Flows Planetary Mapping Overview In this

More information

Name Date. Partners. Comparative Planetology by Mary Lou West after Paul Johnson and Ron Canterna

Name Date. Partners. Comparative Planetology by Mary Lou West after Paul Johnson and Ron Canterna Name Date Partners Comparative Planetology by Mary Lou West after Paul Johnson and Ron Canterna Purpose : to become familiar with the major features of the planets of the solar system, especially the Earth,

More information

Mapping the Surface of Mars Prelab. 1. Explain in your own words what you think a "geologic history" for a planet or moon is?

Mapping the Surface of Mars Prelab. 1. Explain in your own words what you think a geologic history for a planet or moon is? Prelab 1. Explain in your own words what you think a "geologic history" for a planet or moon is? 2. Describe some of the major features seen on the Martian surface by various spacecraft missions over the

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

b. What evidence could you see on, above, or around the rim of a planet, dwarf planet, or moon that would indicate the presence of an atmosphere?

b. What evidence could you see on, above, or around the rim of a planet, dwarf planet, or moon that would indicate the presence of an atmosphere? ASTR& 101 Name: Extra Credit Exercise in Planetary Geology: The Geology of Pluto The New Horizons satellite, launched by NASA in 2006, completed its flyby of Pluto in July of 2014, passing the dwarf of

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

Q. Some rays cross maria. What does this imply about the relative age of the rays and the maria?

Q. Some rays cross maria. What does this imply about the relative age of the rays and the maria? Page 184 7.1 The Surface of the Moon Surface Features To the naked eye, the Moon is a world of grays. Some patches are darker than others, creating a vague impression of what some see as a face ( the man

More information

Planetary Geology. Geology Colloquium. Tucker County Research Assistants

Planetary Geology. Geology Colloquium. Tucker County Research Assistants Planetary Geology Geology Colloquium Dr. Peter Sak, Dickinson College Interseismic Coupling, Quaternary Uplift Rates, and Fore Arc Deformation along the Costa Rican Segment of the Middle American Trench

More information

Type of Exercise: In-Class Activity or Laboratory Exercise.

Type of Exercise: In-Class Activity or Laboratory Exercise. Using Lava Flows & Volcanic Structures on Mars to Introduce the Concept of Relative Dating in Introductory Courses Audeliz Matias Skidmore College, Saratoga Springs, NY 12866 amatias@skidmore.edu Type

More information

core mantle crust the center of the Earth the middle layer of the Earth made up of molten (melted) rock

core mantle crust the center of the Earth the middle layer of the Earth made up of molten (melted) rock core the center of the Earth mantle the middle layer of the Earth made up of molten (melted) rock crust the surface layer of the Earth that includes the continents and oceans 1 continental drift the theory

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

Where do they come from?

Where do they come from? Exploring Meteorite Mysteries Lesson 7 Crater Hunters Objectives Students will: observe impact craters on Earth and other solar system bodies. discuss geologic forces that have removed most of the evidence

More information

Lunar Geology of Apollo 11 Landing Site. Chenango Forks High School Sharon Hartzell Sarah Maximowicz Benjamin Daniels Sarah Andrus Jackson Haskell

Lunar Geology of Apollo 11 Landing Site. Chenango Forks High School Sharon Hartzell Sarah Maximowicz Benjamin Daniels Sarah Andrus Jackson Haskell Lunar Geology of Apollo 11 Landing Site Chenango Forks High School Sharon Hartzell Sarah Maximowicz Benjamin Daniels Sarah Andrus Jackson Haskell Lunar Maria Lunar Maria Lunar Maria Low albedo Volcanic

More information

Introduction. Background

Introduction. Background Introduction In introducing our research on mars we have asked the question: Is there a correlation between the width of an impact crater and the depth of that crater? This will lead to answering the question:

More information

Read Across America. Listen as I read for facts about Volcanoes. In the Shadow of the Volcano

Read Across America. Listen as I read for facts about Volcanoes. In the Shadow of the Volcano Read Across America Listen as I read for facts about Volcanoes. In the Shadow of the Volcano Constructive & Destructive Processes Earth s surface is always changing. Blowing wind and flowing water causes

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: 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

EXPLORING THE GEOLOGY OF SEVERAL WORLDS FROM SPACE

EXPLORING THE GEOLOGY OF SEVERAL WORLDS FROM SPACE NAME DATE PARTNER(S) EXPLORING THE GEOLOGY OF SEVERAL WORLDS FROM SPACE We have investigated to understand how scientists can map the sea floor and land surfaces of the Earth. Now let=s extend our vision

More information

Rilles Lunar Rilles are long, narrow, depressions formed by lava flows, resembling channels.

Rilles Lunar Rilles are long, narrow, depressions formed by lava flows, resembling channels. Rilles Lunar Rilles are long, narrow, depressions formed by lava flows, resembling channels. Rugged Terra Rugged terra are mountainous regions of the moon. Wrinkle Ridges Wrinkle Ridges are created through

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

Constructive & Destructive Forces

Constructive & Destructive Forces Constructive & Destructive Forces Intro: Constructive Forces Processes that create landforms. Destructive Forces Processes that destroy landforms. Intro: Constructive Forces Volcanoes Deposition Landslides

More information

TAKE HOME EXAM 8R - Geology

TAKE HOME EXAM 8R - Geology Name Period Date TAKE HOME EXAM 8R - Geology PART 1 - Multiple Choice 1. A volcanic cone made up of alternating layers of lava and rock particles is a cone. a. cinder b. lava c. shield d. composite 2.

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

UNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA

UNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA UNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA A map that shows Earth s Topographic Map surface topography, which is Earth s shape and features Contour

More information

1.2: Observing the Surfaces of Mars and Earth

1.2: Observing the Surfaces of Mars and Earth GEOLOGY ON MARS Unit 1 - Chapter 1-2 Comparing Rocky Planets 1.2: Observing the Surfaces of Mars and Earth Log on to Amplify Geology on Mars Chapter 1.2 In a moment, you will watch a video made by other

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

COSMORPHOLOGY - May 2012

COSMORPHOLOGY - May 2012 Name COSMORPHOLOGY - May 2012 Geologic mapping Goals: To recognize the similarities and differences in the processes affecting the outer planet satellites, and in the resulting landforms. To demonstrate

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

Unit 7.2 W.E.D. & Topography Test

Unit 7.2 W.E.D. & Topography Test Name: Score: Unit 7.2 W.E.D. & Topography Test 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19. 20. 21. 22. 23. 24. 25. 1. The formation of mountains is due mainly to while the destruction

More information

Interiors of Worlds and Heat loss

Interiors of Worlds and Heat loss Interiors of Worlds and Heat loss Differentiation -materials separate into layers by gravity How do we learn about planetary interiors? Measure moment of inertia & average density Observe seismic events

More information

Highs and Lows, Floods and Flows PLANETARY MAPPING

Highs and Lows, Floods and Flows PLANETARY MAPPING Highs and Lows, Floods and Flows PLANETARY MAPPING OVERVIEW Teams of students become familiar with the topography of Mars, its geologic features, and patterns of features using a color-coded topographic

More information

CHANNELS ON MARS. KWL Prior Knowledge/Engagement Activity

CHANNELS ON MARS. KWL Prior Knowledge/Engagement Activity CHANNELS ON MARS KWL Prior Knowledge/Engagement Activity In your small group, brainstorm ideas about what you think you know about channels and what questions you have about channels on Mars. You will

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

A geologic process An erosional force A chronological tool An influence on biology

A geologic process An erosional force A chronological tool An influence on biology Impact Cratering: Physics and Chronology A geologic process An erosional force A chronological tool An influence on biology Impact features are common All solar system bodies with solid surfaces show evidence

More information

Changes to Land 5.7B. landforms: features on the surface of Earth such as mountains, hills, dunes, oceans and rivers

Changes to Land 5.7B. landforms: features on the surface of Earth such as mountains, hills, dunes, oceans and rivers All the landforms on Earth have changed over time and continue to change. Many of the changes were caused by wind, moving water, and moving ice. Mountains have grown and shrunk. Rivers have cut away land

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

Think about the landforms where you live. How do you think they have changed over time? How do you think they will change in the future?

Think about the landforms where you live. How do you think they have changed over time? How do you think they will change in the future? reflect All the landforms on Earth have changed over time and continue to change. Many of the changes were caused by wind, moving water, and moving ice. Mountains have grown and shrunk. Rivers have cut

More information

1. Which type of climate has the greatest amount of rock weathering caused by frost action? A) a wet climate in which temperatures remain below

1. Which type of climate has the greatest amount of rock weathering caused by frost action? A) a wet climate in which temperatures remain below 1. Which type of climate has the greatest amount of rock weathering caused by frost action? A) a wet climate in which temperatures remain below freezing B) a wet climate in which temperatures alternate

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

Rocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock

Rocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock Rocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock can start out as one type and change into another.

More information

GEOLOGY 12 CHAPTER 22 WORKSHEET COMPARATIVE PLANETOLOGY INTRODUCTION (VIDEO) Name

GEOLOGY 12 CHAPTER 22 WORKSHEET COMPARATIVE PLANETOLOGY INTRODUCTION (VIDEO) Name GEOLOGY 12 CHAPTER 22 WORKSHEET COMPARATIVE PLANETOLOGY Name References: Video: Overview of the Solar System (Standard Deviants 30 minutes) Text: pages 165-167 and 475-501 CDROM (Library): Exploring the

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

deep within the planet. They are also shaped by conditions on the planet s surface. In

deep within the planet. They are also shaped by conditions on the planet s surface. In Chapter 4 Landforms, Water, and Natural Resources Earth is home to many different types of landforms. These landforms are shaped by forces deep within the planet. They are also shaped by conditions on

More information

Lunar Crater Activity - Teacher Pages

Lunar Crater Activity - Teacher Pages Adapted from: http://www.nasa.gov/pdf/180572main_etm.impact.craters.pdf I took the activity and simplified it so that there was just one independent variable: the drop height, and one dependent variable:

More information

SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES

SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES UNIVERSE CYCLE OVERVIEW OF SECOND GRADE UNIVERSE WEEK 1. PRE: Discovering stars. LAB: Analyzing the geometric pattern of constellations. POST: Exploring

More information

UNIVERSITY OF MARYLAND ASTRONOMY DEPARTMENT. Mars Cratering. Crater count isochrons of Arsia and Pavonis Mons

UNIVERSITY OF MARYLAND ASTRONOMY DEPARTMENT. Mars Cratering. Crater count isochrons of Arsia and Pavonis Mons UNIVERSITY OF MARYLAND ASTRONOMY DEPARTMENT Mars Cratering Crater count isochrons of Arsia and Pavonis Mons Paul Hearding and Ben McIlwain 5/21/2007 Imagery of Arsia and Pavonis Mons taken by Mars Global

More information

CRATER COMPARISONS Investigating Impact Craters on Earth and Other Planetary Worlds

CRATER COMPARISONS Investigating Impact Craters on Earth and Other Planetary Worlds CRATER COMPARISONS Investigating Impact Craters on Earth and Other Planetary Worlds PART 1: OBSERVATIONS AND PRELIMINARY QUESTIONS The images below are of impact craters from different planetary worlds

More information

Class Announcements. Solar System. Objectives for today. Will you read Chap 32 before Wed. class? Chap 32 Beyond the Earth

Class Announcements. Solar System. Objectives for today. Will you read Chap 32 before Wed. class? Chap 32 Beyond the Earth Class Announcements Please fill out an evaluation for this class. If you release your name I ll I give you quiz credit. Will you read Chap 32 before Wed. class? a) Yes b) No Chap 32 Beyond the Earth Objectives

More information

Exploring Geography. Chapter 1. Chapter 1, Section

Exploring Geography. Chapter 1. Chapter 1, Section Chapter 1, Section World Geography Chapter 1 Exploring Geography Copyright 2003 by Pearson Education, Inc., publishing as Prentice Hall, Upper Saddle River, NJ. All rights reserved. Chapter 1, Section

More information

Locating the Planets (Chapter 19) and the Moon and Sun (Chapter 21)

Locating the Planets (Chapter 19) and the Moon and Sun (Chapter 21) GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: Locating the Planets (Chapter 19) and the Moon and Sun (Chapter 21) For this assignment, you will require: a calculator, colored pencils, a metric

More information

Jupiter. Jupiter is the third-brightest object in the night sky (after the Moon and Venus). Exploration by Spacecrafts

Jupiter. Jupiter is the third-brightest object in the night sky (after the Moon and Venus). Exploration by Spacecrafts Jupiter Orbit, Rotation Physical Properties Atmosphere, surface Interior Magnetosphere Moons (Voyager 1) Jupiter is the third-brightest object in the night sky (after the Moon and Venus). Exploration by

More information

Locating the Planets (Chapter 20) and the Moon and Sun (Chapter 22)

Locating the Planets (Chapter 20) and the Moon and Sun (Chapter 22) GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: Locating the Planets (Chapter 20) and the Moon and Sun (Chapter 22) For this assignment, you will require: a calculator, colored pencils, a metric

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

RAYMOND SIEVER Harvard University

RAYMOND SIEVER Harvard University E A R T H FOURTH EDITION FRANK PRESS National Academy of Sciences RAYMOND SIEVER Harvard University W. H. Freeman and Company New York Preface xiii Acknowledgments xviii PART I PROLOGUE CHAPTER 1 HISTORY

More information

MARINER VENUS / MERCURY 1973 STATUS BULLETIN

MARINER VENUS / MERCURY 1973 STATUS BULLETIN MARINER VENUS / MERCURY 1973 STATUS BULLETIN MARINER 10 PICTURES OF MERCURY; SECOND ENCOUNTER PLANNED Fig. 1. (a) Photomosaic of Mercury made from nine computer-enhanced pictures taken at 234,000 km, 6

More information

Chapter 2: Physical Geography

Chapter 2: Physical Geography Chapter 2: Physical Geography Pg. 39-68 Learning Goals for Chp2: q q q q q Explain how the Earth moves in space and why seasons change. Outline the factors that influence climate and recognize different

More information

Day 3 Weathering and Erosion.notebook. October 02, Section 7.2. Erosion and Deposition. Objectives

Day 3 Weathering and Erosion.notebook. October 02, Section 7.2. Erosion and Deposition. Objectives Objectives Describe the relationship of gravity to all agents of erosion. Contrast the features left from different types of erosion. Analyze the impact of living and nonliving things on the processes

More information

The Solar System. Earth as a Planet

The Solar System. Earth as a Planet The Solar System Earth as a Planet Earth s Interior Core: Highest density; nickel and iron Mantle: Moderate density; silicon, oxygen, etc. Crust: Lowest density; granite, basalt, etc. Differentiation Gravity

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

Chapter 9. ASTRONOMY 202 Spring 2007: Solar System Exploration. Class 27: Planetary Geology [3/26/07] Announcements.

Chapter 9. ASTRONOMY 202 Spring 2007: Solar System Exploration. Class 27: Planetary Geology [3/26/07] Announcements. ASTRONOMY 202 Spring 2007: Solar System Exploration Instructor: Dr. David Alexander Web-site: www.ruf.rice.edu/~dalex/astr202_s07 Class 27: Planetary Geology [3/26/07] Announcements Planetary Geology Planetary

More information

MAPPING THE SURFACE OF MARS

MAPPING THE SURFACE OF MARS MAPPING THE SURFACE OF MARS What will you learn in this lab? How can we determine the geologic history of a planet or satellite without travelling to the planetary body? In this lab you will create a simple

More information

Landscape evolution. An Anthropic landscape is the landscape modified by humans for their activities and life

Landscape evolution. An Anthropic landscape is the landscape modified by humans for their activities and life Landforms Landscape evolution A Natural landscape is the original landscape that exists before it is acted upon by human culture. An Anthropic landscape is the landscape modified by humans for their activities

More information

Question #1: What are some ways that you think the climate may have changed in the area where you live over the past million years?

Question #1: What are some ways that you think the climate may have changed in the area where you live over the past million years? Reading 5.2 Environmental Change Think about the area where you live. You may see changes in the landscape in that area over a year. Some of those changes are weather related. Others are due to how the

More information

Impact Cratering. David A. Hardy MARS EDUCATION PROGRAM

Impact Cratering. David A. Hardy MARS EDUCATION PROGRAM Impact Cratering David A. Hardy MARS EDUCATION PROGRAM Impact cratering overview: What we will learn about impact craters today: Causes of impacts - meteorites! Impact craters in our solar system Formation

More information

Science EOG Review: Landforms

Science EOG Review: Landforms Mathematician Science EOG Review: Landforms Vocabulary Definition Term canyon deep, large, V- shaped valley formed by a river over millions of years of erosion; sometimes called gorges (example: Linville

More information

Planetary Geology Earth 9th Edition Chapter 24 Mass wasting: summary in haiku form Overview of the solar system The solar system

Planetary Geology Earth 9th Edition Chapter 24 Mass wasting: summary in haiku form Overview of the solar system The solar system 1 2 3 4 5 6 7 8 9 Planetary Geology Earth 9 th Edition Chapter 24 Mass wasting: summary in haiku form Can it be geo-? When there's only one planet qualified as "Earth?" Solar system includes Sun Eight

More information

Unit 3 Study Guide -- Greenberg science, 6C

Unit 3 Study Guide -- Greenberg science, 6C Unit 3 Study Guide -- Greenberg science, 6C Name Pd. Date / / 2018 + +5 extra credit points on the test if submitted complete and correct ON THE TEST DATE. + A copy can be found on my website mgreenberg.weebly.com

More information

Constructive and Destructive Forces. Processes That Act Upon Earth s Surface Features

Constructive and Destructive Forces. Processes That Act Upon Earth s Surface Features Constructive and Destructive Forces Processes That Act Upon Earth s Surface Features What are Constructive and Destructive Forces? Constructive Force A constructive force is a process that raises or builds

More information

Venus. Appearance. Earth s Sister? Venus is very bright.

Venus. Appearance. Earth s Sister? Venus is very bright. Venus Earth s Sister? Appearance Venus is very bright. It goes through phases, although full cannot be seen. Angular size varies from 10 to 64 arcsec. Venus is at its greatest brilliance when it is a crescent,

More information

Weathering, Erosion, and Deposition Guided Notes

Weathering, Erosion, and Deposition Guided Notes 1. Weathering, Erosion, and Deposition 2. Outline Section 1: Weathering Section 2: Erosion Section 3: Deposition Section 4: Case Study Weathering, Erosion, and Deposition Guided Notes 3. Section 1: Weathering

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

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

Teachersʼ Guide. Creating Craters. Down to Earth KS3

Teachersʼ Guide. Creating Craters. Down to Earth KS3 Teachersʼ Guide Creating Craters Creating Craters! Creating Craters - Teachersʼ Guide - 2 Overview This lesson allows pupils to create impact craters in layered dry materials. Pupils can perform controlled

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

Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE

Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE The Structure of the Earth To understand the forces that create Canada's physical landscape we must understand the structure

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

A Geological Tour of Tumbledown Mountain, Maine

A Geological Tour of Tumbledown Mountain, Maine Maine Geologic Facts and Localities April, 1998 A Geological Tour of Tumbledown Mountain, Maine 44 45 3.21 N, 70 32 50.24 W Text by Robert G. Marvinney, Department of Agriculture, Conservation & Forestry

More information

Earth s Dynamic Surface

Earth s Dynamic Surface Earth s Dynamic Surface Key Concepts What is the difference between physical and chemical weathering? How do water, ice, and wind change Earth s surface? Changing Earth s Surface What do you think? Read

More information

The Marine Environment

The Marine Environment The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write or. 1.

More information

Assignment 4. Due TBD

Assignment 4. Due TBD Assignment 4 Due TBD Show all work and turn in answers on separate pages, not on these pages. Circle your final answers for clarity. Be sure to show/explain all of your reasoning and that your work is

More information

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

23.1 The Solar System. Orbits of the Planets. Planetary Data The Solar System. Scale of the Planets The Solar System 23.1 The Solar System Orbits of the Planets The Planets: An Overview The terrestrial planets are planets that are small and rocky Mercury, Venus, Earth, and Mars. The Jovian planets are the huge gas giants

More information

EROSIONAL FEATURES. reflect

EROSIONAL FEATURES. reflect reflect Have you ever looked at the land around you and wondered what processes shaped what you see? Perhaps you see mountains, valleys, rivers, or canyons. Do you know how long these geologic features

More information

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

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

Teacher Background. Impact! Down to Earth KS 3&4

Teacher Background. Impact! Down to Earth KS 3&4 Teacher Background Impact! Impact! - Teacher Background- 2 Meteorites What Are They, and Where Do They Come From? Meteorites are rocks from space that have passed through the atmosphere and landed on the

More information

crater density: number of craters per unit area on a surface

crater density: number of craters per unit area on a surface Reading for this week: Chap. 9, Sect. 9.4-9.5, Chap. 10, Sect. 10.1-10.5 Homework 6: due in recitation Friday/Monday (Oct. 13, 16) Midterm grade estimates posted on Blackboard this week Astro 120 Fall

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