the terrestrial planets, part i mercury and venus

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The Terrestrial Planets, Part I Mercury and Venus

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Page 1: The Terrestrial Planets, Part I Mercury and Venus

The Terrestrial Planets, Part I

Mercury and Venus

Page 2: The Terrestrial Planets, Part I Mercury and Venus

MERCURYThe Winged Messenger

Page 3: The Terrestrial Planets, Part I Mercury and Venus

Physical Data

Diameter: 4,864 km (0.382 Dearth)

Mass: 3.33x1026 g (0.0558 Mearth) Density: 5.50 g/cm3

Rotation Period: 58.65 days Tilt of Axis: 0o

Surface Temperature: 700 K (day side) . 100 K (dark side)

Page 4: The Terrestrial Planets, Part I Mercury and Venus

Physical Data

Orbital Semi-Major Axis: 0.387 AU

Perihelion Distance: 0.308 AU

Aphelion Distance: 0.467 AU Orbital Period : 87.97 days (0.241 years) Orbital Inclination: 7.00o

Orbital Eccentricity: 0.206 Surface Gravity: 0.38 Earth gravity

Page 5: The Terrestrial Planets, Part I Mercury and Venus

Physical Data

Maximum Elongation: 28o (aphelion)

18o (perihelion) . 23o (average)

Satellites: None Magnetic Field: 1% strength of Earth’s

Page 6: The Terrestrial Planets, Part I Mercury and Venus

Mercury Apparitions At western elongation, Mercury is visible in

the morning before dawn (“morning star”). At eastern elongation, Mercury is visible in

the evening after sunset (“evening star”). Mercury appears to change in size, and has

phases like the Moon.

Page 7: The Terrestrial Planets, Part I Mercury and Venus

Mercury’s 3:2 Resonance

Once thought to be synchronous

Mercury rotates 3 times for every two orbits

One Mercury “day” lasts two Mercurian years!

Page 8: The Terrestrial Planets, Part I Mercury and Venus

Mercury’s Interior

Mercury is the most iron-rich planet in the solar system.

Of all the planets, Mercury has the largest core relative to its overall volume (42%, 16% for Earth)

Page 9: The Terrestrial Planets, Part I Mercury and Venus

Mercury’s Magnetic Field

1% Earth’s Magnetic Field

SUN

Page 10: The Terrestrial Planets, Part I Mercury and Venus

Mercury’s Surface

Mercury appears very Moon-like

m

Page 11: The Terrestrial Planets, Part I Mercury and Venus

Mercury’s Surface

Craters

Page 12: The Terrestrial Planets, Part I Mercury and Venus

Mercury’s Surface

Lobate Scarps

Page 13: The Terrestrial Planets, Part I Mercury and Venus

Mercury’s Surface

Caloris Basin - 1300 km diameter crater

Page 14: The Terrestrial Planets, Part I Mercury and Venus

Mercury’s Surface

“Weird” (or Jumbled) Terrain

Polar caps?

Page 15: The Terrestrial Planets, Part I Mercury and Venus

Other Topics:

Precession of perihelion

Radar measurements of Mercury’s rotation

Page 16: The Terrestrial Planets, Part I Mercury and Venus

VENUSThe Goddess of Love

Page 17: The Terrestrial Planets, Part I Mercury and Venus

Physical Data

Diameter: 12,104 km (0.951 Dearth)

Mass: 4.87x1027 g (0.815 Mearth) Density: 5.30 g/cm3

Rotation Period: 243 days Tilt of Axis: 177.4o (retrograde) Suface Temperature: 750 K

Page 18: The Terrestrial Planets, Part I Mercury and Venus

Physical Data

Orbital semi-major axis: 0.723 AU Orbital period: 224.70 days (0.615 years) Orbital inclination: 3.39o

Orbital Eccentricity: 0.007 Maximun Elongation: 48o

Surface Gravity: 0.90 Earth gravity

Page 19: The Terrestrial Planets, Part I Mercury and Venus

Physical Data

Satellites: None Magnetic Field: No

Surface Pressure: 90 times Earth’s!

Page 20: The Terrestrial Planets, Part I Mercury and Venus

Venus Apparitions At western elongation, Venus is visible in

the morning before dawn (“morning star”). At eastern elongation, Venus is visible in

the evening after sunset (“evening star”). Venus appears to change in size, and has

phases like the Moon

Page 21: The Terrestrial Planets, Part I Mercury and Venus

Clouds of Venus

Clouds whiz aroud Venus at 300 km/hr.

At this speed, a cloud can circle Venus in only four days.

Clouds are composed of mostly sulfuric acid and water.

Page 22: The Terrestrial Planets, Part I Mercury and Venus

The Atmosphere of Venus

96.5% Carbon Dioxide 3% Nitrogen Traces of Other Gases:

0.019% Sulfur Dioxide

0.01% Water Vapor

0.007% Argon

Hydrochloric acid, Hydroflouric acid Atmospheric Pressure 90x Earth’s

Page 23: The Terrestrial Planets, Part I Mercury and Venus

Venus’ Atmosphere

Clouds contain sulfuric acid and water

Cloud tops appear yellow from sulfur dust

Temperature reaches a maximum at the surface of about 750 K (900o F)

15 km

45 km

60 km

75 km

Top of Clouds

30 km

Upper Cloud Deck

Droplets of Sulfuric Acid & Water

Lower Cloud Deck

Sulfuric Acid& Water and Sulfur Crystals

Haze Layer

Clouds T hin Out

Clear, Hot Atmosphere

0 km

Temperature

105 km

200 K 400 K 600 K 800 K0 K

Altitude

Page 24: The Terrestrial Planets, Part I Mercury and Venus

Why is Venus So Hot?

Page 25: The Terrestrial Planets, Part I Mercury and Venus

Venus’ Interior

Core - 12% total volume of planet

Molten core?

Thin crust, with continent sized features.

CORE( iron-nickel )

MANTLE( olivine )

CRUST( silicates)

6052 km

3616 km

Venus

Page 26: The Terrestrial Planets, Part I Mercury and Venus

Soviet Venera Missions

First Surface Photographs, 1970

Photo from Venera 13

Page 27: The Terrestrial Planets, Part I Mercury and Venus

The Magellan Mission

m

Page 28: The Terrestrial Planets, Part I Mercury and Venus

Magellan Surface Imagery

Suface Features:

Impact Craters

Lava Flows

Volcanic Calderas

Volcanoes Peculiar to Venus:

Coronae, Pancake . Domes, Ticks, Graph Paper Regions

m

Page 29: The Terrestrial Planets, Part I Mercury and Venus

Venus’ Surface

Graph Paper Regions

Page 30: The Terrestrial Planets, Part I Mercury and Venus

Venus’ Surface

“The Tick”

Page 31: The Terrestrial Planets, Part I Mercury and Venus

Venus’ Surface

Coronae

Page 32: The Terrestrial Planets, Part I Mercury and Venus

Venus’ Surface

Pancake Domes