Structure of Mercury And no atmosphere, so no wind or erosion. Surface reflects geologic history well. (from Mariner 10 and theoretical arguments) 1.Crust.

Slides:



Advertisements
Similar presentations
Chapter 7 Earth and the Terrestrial Worlds
Advertisements

© 2005 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors in teaching their.
ASTR100 (Spring 2008) Introduction to Astronomy Earth as a Planet Prof. D.C. Richardson Sections
Lecture Outlines Astronomy Today 8th Edition Chaisson/McMillan © 2014 Pearson Education, Inc. Chapter 10.
Mars Astronomy 311 Professor Lee Carkner Lecture 14.
Mars Astronomy 311 Professor Lee Carkner Lecture 14.
The Terrestrial Planets Astronomy 311 Professor Lee Carkner Lecture 9.
The Moon = 3.3 g/cm 3 (Earth 5.5 g/cm 3 ) = 1/6 that of Earth Mass Radius Density Gravity = 7.4 x g = M Earth  = 1738 km = 0.27 R Earth.
Announcements Ch. 5 homework will finally post tonight Test 2 score have posted. If you did not have your ID, please see me after class Scores on Mastering.
Venus Astronomy 311 Professor Lee Carkner Lecture 11.
Mercury = 5.4 g/cm 3 (Earth 5.5 g/cm 3 ) = 0.38 that of Earth Mass Radius Density Gravity = 3.3 x g = M Earth  = 2439 km = 0.38 R Earth Semimajor.
April 11, 2006Astronomy Chapter 9 Earth-Like Planets: Venus and Mars Venus and Mars resemble Earth more than any other planets. Is it possible that.
The Terrestrial Planets Astronomy 311 Professor Lee Carkner Lecture 9.
Interiors of Terrestrial Planets. Mercury MEAN RADIUS: km MASS: (Earth=1) DENSITY: 5.43 (g/cm^3) GRAVITY: (Earth=1) ORBIT PERIOD:
Mars. Some similarities between Mars & Earth Mars’ Bulk Properties Mars has days & seasons like Earth.
The Terrestrial Planets Astronomy 311 Professor Lee Carkner Lecture 9.
Astronomy Picture of the Day. Mercury Mass = M Earth Radius = 0.38 R Earth  Surface Temp: K Average distance from Sun =.39 AU Moonlike:
The Moon = 3.3 g/cm 3 (Earth 5.5 g/cm 3 ) = 1/6 that of Earth Mass Radius Density Gravity = 7.4 x g = M Earth  = 1738 km = 0.27 R Earth.
Astronomy Picture of the Day. Mercury Mass = M Earth Radius = 0.38 R Earth  Surface Temp: K Moonlike: Surface craters, no atmosphere.
15 February 2005AST 2010: Chapter 9 1 Venus & Mars.
The Terrestrial Planets, Part III Mars. MARS The God of War.
The Solar System.
Chapter 6 The Terrestrial Planets. Units of Chapter 6 Orbital and Physical Properties Rotation Rates Atmospheres The Surface of Mercury The Surface of.
© 2011 Pearson Education, Inc. Venus and Mars. © 2011 Pearson Education, Inc. Venus.
Chapter 7 Earth and The Terrestrial Worlds Principles of Comparative Planetology Comparative Planetology is the study of the solar system through examining.
Astronomy 1. Weekly Quiz  In place of a quiz this week, you must be able to identify each inner planet and give several facts for each.  So pay attention!!!!
The Inner Planets. Mercury Small Weak gravitational force No atmosphere Many craters.
Unit 2 Lesson 4 The Terrestrial Planets Copyright © Houghton Mifflin Harcourt Publishing Company.
Mars Mars is a dry dead world. There are no Martian transits.
Announcements Online calendar has been updated – check it out Ch. 5 homework has finally posted Test 2 score have posted. If you did not have your ID,
1 Inner or Terrestrial Planets All the inner planets formed at the same time. Their composition is also very similar. They lack the huge atmospheres of.
1. fluidized ejecta - liquid material expelled from meteor crater. Probably caused by permafrost melting when meteor hits.
The Inner Planets 20.3.
Mars - The Red Planet Image Courtesy of NASA/JPL-Caltech.
The Inner Planets Chapter Terrestrial Planets Mercury, Venus, Earth, Mars Mostly solid rock with metallic cores Impact craters.
Image Courtesy of NASA/JPL-Caltech.  Known to Babylonians 3,600 years ago as “Star that Wandered”  The Greeks referred to it as “Ares” the god of War.
MARS. Where is Mars? 4 th planet in our solar system. Last of the rocky planets. Our solar system is in the Orion arm of the Milky Way Galaxy. Our sun.
Chapter 10 Mars. Mars’s orbit is fairly eccentric which affects amount of sunlight reaching it 10.1 Orbital Properties.
Earth and the Other Terrestrial Worlds
INNER PLANETS Terrestrial Planets are the Four planets closest to the sun. These planets have rocky terrain, and have higher temperatures due to receiving.
The Inner planets Section 28.2.
Astronomy: A Beginner’s Guide to the Universe Seventh Edition © 2013 Pearson Education, Inc. Chapter 6 Lecture The Terrestrial Planets.
Life on Mars Stephen Eikenberry 12 October 2010 AST
MARS.
Mars. When and where can you see it? Can be seen all night long. Sometimes undergoes apparent retrograde motion.
Mars Images How We Know What We Know Current Spacecraft Mars Odyssey (’01-present) Mars Express (’03-present) Mars Exploration Rovers (’04-present) Mars.
Sept 29, 2003Astronomy 100 Fall 2003 Last Homework before Exam (HW#4) is due Friday at 11:50am. Nighttime observing has 8 more nights. Check the webpage.
Unit 11 Mars. Physical Properties Radius: 3400 km Moons: Deimos, Phobos Mass: 6.4 × kg Density: 3900 kg/m 3 Length of Day: 24.6 hours.
Chapter 7c Mars: Freeze-dried Image from:
© 2010 Pearson Education, Inc. Erosion of Craters Details of some craters suggest they were once filled with water.
The Terrestrial Planets Mercury, Venus, Earth, Mars.
The Inner Planets.
{ The Inner Planets Chapter 14 Section 3.
Mars Mars is a dry dead world. There are no Martian transits.
Curiosity Curiosity pictures Rover view Old Rover View form older rover.
Mars.
Mars - The Red Planet Image Courtesy of NASA/JPL-Caltech.
Unit 2 Lesson 4 The Terrestrial Planets
Mars eccentricity = Mass = 0.11 MEarth
Section 2: The Inner Planets
© 2017 Pearson Education, Inc.
Planets in the Solar System
Mars.
Orbital and Physical Properties
Venus Mass = 0.82 MEarth Radius = 0.95 REarth Density = 5.2 g/cm3
Section 2: The Inner Planets
Mars - The Red Planet Image Courtesy of NASA/JPL-Caltech.
Mercury – Craters.
Craters on Mars Many craters Closer to asteroid belt No water erosion
Stephen Eikenberry 21 Feb 2019 AST 2037
Presentation transcript:

Structure of Mercury And no atmosphere, so no wind or erosion. Surface reflects geologic history well. (from Mariner 10 and theoretical arguments) 1.Crust km thick 2. Mantle 600 km thick 3. Core, 1800 km in radius

Venus Mass = 0.82 M Earth Radius = 0.95 R Earth  Density = 5.2 g/cm 3 Average distance from Sun = 0.72 AU Orbital period = 225 days Rotation period = 243 days (longer than orbital period, and retrograde!)

Venus' Atmosphere - Pressure at surface is 90 x that of Earth's => much more gas in atmosphere. No oceans. - Consequence - meteoroids burn up easily. No impact craters less than ~3 km. What ’ s the composition of the atmosphere? - Hot at surface K! Almost hot enough to melt rock - Why so hot? Huge amount of CO 2 leads to strong greenhouse effect % CO 2 - Yellowish color from sulfuric acid clouds and haze.

Early on, T may have been much lower (but still warmer than Earth). Oceans existed? But if warm enough, T would start to rise because of... Runaway Greenhouse Effect 1) Water and CO 2 evaporate from oceans into atmosphere. 2) Greenhouse effect more efficient. 3) Temperature rises. 4) More evaporation (back to #1). => complete evaporation of oceans. Thick atmosphere.

The Habitable Zone or “The Goldilocks Problem” In the zone …

Missions to Venus Soviet Venera ( ) Mariner 2, 5 and 10 (1962, 1967 and 1974) Pioneer Venus (1978) Magellan (1989) Venera 13 photo of surface. Rocks are basalt and granite. Color is due to atmosphere. Color corrected for atmosphere.

"Radar Echo" technique measures altitude space probe time for signal to return tells you the altitude of surface feature. Planet Surface

Radar data (Pioneer Venus mission) reveal altitude variations on surface. Flatter than Earth, no evidence for plate boundaries => no large scale plate tectonics. 1 km But plenty of evidence of stresses and fractures on smaller scales => much small-scale shifting of crust

Unlike Moon, larger impact craters distributed randomly over surface => all parts of surface have about same age. Paucity of large impact craters => surface is young, million years? Impact Craters

Volcanism Shield volcano elevation map from Magellan radar data. About 100 km across. Volcanism may be ongoing, based on sulfur dioxide variations in atmosphere. But very little resurfacing in past million years. Venus surface flyover

Volcanism Venus surface flight simulation using data from Magellan.

Clicker Question: Why is Venus the hottest planet in the Solar System? A: It is the closest planet to the Sun. B: There is a lot of radioactive material in the crust. C: There is a large concentration of carbon dioxide in the atmosphere. D: The Russians left the lights on in the Venera 5 landing vehicle. E. Paris Hilton lives there.

Mars Mass = 0.11 M Earth Radius = 0.53 R Earth Density = 3.9 g/cm 3 Average distance from Sun = 1.52 AU eccentricity = Range in distance from Sun = AU Rotation Period = 24.6 hours Orbital Period = 687 days

The Martian Atmosphere - 95% CO 2 - Surface Pressure that of Earth's atmosphere (thin air!) - Surface Temperature 250 K. - Dust storms sometimes envelop most of Mars, can last months. A “Reverse Runaway Greenhouse Effect”? During volcanic phase (first two billion years), thicker atmosphere, warmer surface, possibly oceans. Gradually most CO 2 dissolved into surface water and combined with rocks, then atmospheric and surface water froze (creating ice caps and probable permafrost layer).

Mars' Moons Phobos and Deimos Phobos: 28 x 20 km Deimos: 16 x 10 km Properties similar to asteroids. They are probably asteroids captured into orbit by Mars' gravity.

Clicker Question: From Mars, Deimos has an angular diameter of 140 arcseconds. Would colonists on Mars ever see Deimos produce a total solar eclipse? A: Yes, every day on Mars B: Yes, every new moon C: Yes, but rarely D: Never

The Martian Surface Valles Marineris Olympus Mons Tharsis Bulge Southern Hemisphere ~5 km higher elevation than Northern, and more heavily cratered. South is like lunar highlands, surface ~4 billion years old, North like maria, ~3 billion years old. Valles Marineris km long, up to 7 km deep. Ancient crack in crust. Reasons not clear. Tharsis Bulge - highest (10 km) and youngest (2-3 billion years) region. Olympus Mons - shield volcano, highest in Solar System, 3x Everest in height. 100 km across. (Mars Global Surveyor radar data)

View From the Surface Viking 1 site (1976)Sojourner robot from Pathfinder (1997) Dry, desert-like. Red => high iron content. Mars didn't differentiate as completely as Earth. Sky has butterscotch hue due to dust.

Opportunity panorama: inside Victoria Crater Deepest crater explored by far (230 feet) => apparently it was the top of an underground water table.

Evidence for Past Surface Water "runoff channels" or dry rivers "outflow channels" teardrop "islands" in outflow channels standing water erosion in craters? South North

Red arrows: rounded boulders indicating water erosion? White arrows: "conglomerate" rock, like in Earth's riverbeds? Blue arrows: sharp-edged boulders, volcanic rock? Pathfinder site was an outflow channel

Did Mars once have a huge ocean? Long stretches along border are very even in elevation, like a coastline Ocean fed by outflow channels from higher elevation southern hemisphere?

Evidence for "Permafrost" layer beneath surface "Splosh" craters suggesting liquefied ejecta.

Evidence for Water on Mars Now Phoenix Lander (2008) Deployable arm subsurface ice

Phoenix mission – icy soil at the poles! Phoenix analyzing scooped up dirt – was Mars ever favorable for microbial life? Organic compounds?

Mars' History Smaller than Earth, Mars cooled faster. Atmosphere and surface water in first 1.5 billion years. Life? Most volcanic activity ended two billion years ago. Differentiation less complete than on Earth. No evidence for plate tectonics. Atmosphere mostly froze out into subsurface ice, polar ice caps and surface rocks.

Clicker Question: The largest mountain in our solar system is: A: Caloris Basin range on Mercury B: Gula Mons on Venus C: Mt. Everest on Earth D: Olympus Mons on Mars

Clicker Question: Where is the water that once flowed on the surface of Mars? A: In the atmosphere B: In the polar caps only C: In a layer of permafrost below the surface and in the polar caps D: It was diverted to Los Angeles

Martian ‘Snick’ meteorite ALH84001 shows odd shaped features that are reminiscent of bacteria. General consensus is no life.

Valles Marinaris flyover movie

The Face on Mars Viking orbiter photos showed this:

Newer, high resolution photo – Mars Global Surveyor 1998

Isn’t this more disturbing???

Spirit and Opportunity Rovers Scenes from “Roving Mars” (start at 15:10, skip to 20:27, skip to 26:16)