ASTR 1101-001 Spring 2008

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ASTR 1101-001 Spring 2008 Joel E. Tohline, Alumni Professor 247 Nicholson Hall [Slides from Lecture30]

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ASTR 1101-001 Spring 2008. Joel E. Tohline, Alumni Professor 247 Nicholson Hall [Slides from Lecture30]. Chapter 11: Terrestrial Planets. Mercury Heavily cratered (like the Earth’s moon) Some evidence of lava flows and shrinkage of the planet’s crust Generally considered a “dead” planet - PowerPoint PPT Presentation

Transcript of ASTR 1101-001 Spring 2008

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ASTR 1101-001Spring 2008

Joel E. Tohline, Alumni Professor

247 Nicholson Hall

[Slides from Lecture30]

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Chapter 11: Terrestrial Planets

• Mercury– Heavily cratered (like the Earth’s moon)– Some evidence of lava flows and shrinkage of

the planet’s crust– Generally considered a “dead” planet

• Venus

• Mars

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Chapter 11: Terrestrial Planets

• Mercury– Heavily cratered (like the Earth’s moon)– Some evidence of lava flows and shrinkage of

the planet’s crust– Generally considered a “dead” planet

• Venus

• Mars

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Chapter 11: Terrestrial Planets

• Mercury– Heavily cratered (like the Earth’s moon)– Some evidence of lava flows and shrinkage of

the planet’s crust– Generally considered a “dead” planet

• Venus

• Mars

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Chapter 11: Terrestrial Planets

• Mercury– Heavily cratered (like the Earth’s moon)– Some evidence of lava flows and shrinkage of

the planet’s crust– Generally considered a “dead” planet

• Venus

• Mars

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Chapter 11: Terrestrial Planets

• Venus– Rotating very slowly…and backwards!– Atmosphere: Dense, hot, and corrosive!– Properties of atmosphere due to runaway

“greenhouse” effect

• Venus

• Mars

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Venus:

Image of the surface of Venus obtained by radar imaging.

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Venus: topographic map

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Chapter 11: Terrestrial Planets

• Venus– Rotating very slowly…and backwards!– Atmosphere: Dense, hot, and corrosive!– Properties of atmosphere due to runaway

“greenhouse” effect

• Venus

• Mars

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Chapter 11: Terrestrial Planets

• Venus– Rotating very slowly…and backwards!– Atmosphere: Dense, hot, and corrosive!– Properties of atmosphere due to runaway

“greenhouse” effect

• Venus

• Mars

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Atmospheres of Earth & Venus

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Venus:

Ultraviolet image of Venus highlighting theCloud layer structure.

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Chapter 11: Terrestrial Planets

• Venus– Rotating very slowly…and backwards!– Atmosphere: Dense, hot, and corrosive!– Properties of atmosphere due to runaway

“greenhouse” effect

• Venus

• Mars

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Chapter 11: Terrestrial Planets

• Mars– Surface imaged by spacecraft extremely well– Surface explored by spacecraft that have

successfully soft-landed on surface• Viking Lander (VL1 & VL2)• Mars Pathfinder (MP)• Exploration Rovers (Opportunity & Spirit)

– Evidence for (subsurface) water

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Chapter 11: Terrestrial Planets

• Mars– Surface imaged by spacecraft extremely well– Surface explored by spacecraft that have

successfully soft-landed on surface• Viking Lander (VL1 & VL2)• Mars Pathfinder (MP)• Exploration Rovers (Opportunity & Spirit)

– Evidence for (subsurface) water

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Mars: topographic mapwww.google.com/mars

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Chapter 11: Terrestrial Planets

• Mars– Surface imaged by spacecraft extremely well– Surface explored by spacecraft that have

successfully soft-landed on surface• Viking Lander (VL1 & VL2)• Mars Pathfinder (MP)• Exploration Rovers (Opportunity & Spirit)

– Evidence for (subsurface) water

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Chapter 11: Terrestrial Planets

• Mars– Surface imaged by spacecraft extremely well– Surface explored by spacecraft that have

successfully soft-landed on surface• Viking Lander (VL1 & VL2)• Mars Pathfinder (MP)• Exploration Rovers (Opportunity & Spirit)

– Evidence for (subsurface) water

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Mars: topographic mapwww.google.com/mars

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Chapter 11: Terrestrial Planets

• Mars– Surface imaged by spacecraft extremely well– Surface explored by spacecraft that have

successfully soft-landed on surface• Viking Lander (VL1 & VL2)• Mars Pathfinder (MP)• Exploration Rovers (Opportunity & Spirit)

– Evidence for (subsurface) water

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Mars: topographic mapwww.google.com/mars

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Chapter 11: Terrestrial Planets

• Mars– Surface imaged by spacecraft extremely well– Surface explored by spacecraft that have

successfully soft-landed on surface• Viking Lander (VL1 & VL2)• Mars Pathfinder (MP)• Exploration Rovers (Opportunity & Spirit)

– Evidence for (subsurface) water

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Mars: topographic mapwww.google.com/mars

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Rover ‘Opportunity’: Landing Site

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Rover ‘Opportunity’: Four+ years of travel

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Rover ‘Opportunity’: Four+ years of travel

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Rover ‘Opportunity’: View from edge of Victoria Crater

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Chapter 11: Terrestrial Planets

• Mars– Surface imaged by spacecraft extremely well– Surface explored by spacecraft that have

successfully soft-landed on surface• Viking Lander (VL1 & VL2)• Mars Pathfinder (MP)• Exploration Rovers (Opportunity & Spirit)

– Evidence for (subsurface) water

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