terrestrial planets. planetary size and heat loss large planets retain internal heat longer small...

79
Terrestrial Planets

Upload: anne-webster

Post on 04-Jan-2016

220 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Terrestrial Planets

Page 2: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 3: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 4: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Planetary size and heat loss

Large planets retain internal heat longer

Small planets cool off quickly

Page 5: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 6: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Geologic processes

1) Impact cratering

2) Volcanism

3) Tectonics

4) Erosion

Page 7: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

The Moon has lots of impact craters, while the Earth has very few. Why do you think there is a difference?

Page 8: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Surface age

The more impact craters on a surface, the older that surface is.

The age of a surface refers to when that surface solidified.

Page 9: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Which area on the Moon is older, the light region to the left or the dark region in the center of the picture?

Page 10: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 11: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Why do you think a more heavily cratered planetary surface is older than a smooth one?

Page 12: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Why?

All the terrestrial planets probably receive about the same number and size distribution of impacts. All the other geologic processes (volcanism, tectonics, and erosion) tend to erase impact craters on the surface.

Page 13: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Rank the terrestrial planets (include the Moon) in terms of the age of their surfaces from youngest to oldest to try and predict which planets will have the most craters.

Page 14: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

1. Earth2. Venus3. Mars4. Mercury5. Moon

Smaller planets retain less heat and therefore have less geologic activity.

Page 15: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 16: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 17: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 18: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 19: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 20: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 21: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 22: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Almost all impact creators are round. Why do you think there are not many elliptically shaped craters?

Page 23: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Almost all impact craters are round

In general, impactors will hit with a velocity greater than the escape velocity. The high speed collision results in the almost complete vaporization of the impactor. This explosion of super-heated, vaporized rock is what creates the crater.

Page 24: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 25: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 26: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Moltke Crater (7 km)

Page 27: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Bessel crater (16 km)

Page 28: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Euler Crater (25 km)

Page 29: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

King Crater (77 km)

Page 30: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Copernicus Crater (95 km)

Page 31: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Schrodinger (320 km)

Page 32: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Mare Orientale (930 km)

Page 33: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Mare Imbrium (1100 km)

Page 34: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Meteor Crater (1.2 km)

Page 35: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Arizona from the Shuttle

Page 36: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Wolf Creek (0.85 km)

Page 37: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

New Quebec Crater (3.4 km)

Page 38: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Clearwater Lakes (26 km)

Page 39: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Chichxulub Crater (250 km)

Page 40: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Manicouagan Crater (100 km)

Page 41: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Why is the Manicouagan crater inverted, with a lower rim and higher center?

Hint: It is at high northern latitude and is rather old.

Page 42: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Radar images of Venus

Bright areas in radar images indicate rough terrain, while dark areas are smooth. Typically, rough terrain is younger than smooth terrain.

Page 43: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Why are rough areas younger?

Page 44: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Adivar Venus (29 km)

Page 45: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Meitner basin Venus (150 km)

Page 46: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 47: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

What does the fact that there are so few eroded craters tell you about Venus?

Page 48: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Plate Tectonics

Page 49: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 50: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 51: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

No plate tectonics on Venus

Venus may not have an asthenosphere, due to the lack of water in Venus’s mantle.

Alternatively, the crust of Venus may be too plastic to form large-scale faults.

Page 52: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 53: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 54: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 55: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 56: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Colaris basin Mercury (1340 km)

Page 57: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 58: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Hellas basin Mars (2000 km)

Page 59: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 60: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 61: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Notice anything unusual about this crater on Mars? What can you conclude about the surface of Mars where this crater formed?

Page 62: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Why are craters important

• Numbers of craters provide relative ages

• Transition size between simple and complex craters as well as ejecta blanket size and distribution provide clues to the strength of the surface.

Page 63: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Liquid Water

All life on Earth depends on liquid water.

Earth is the only body in the solar system with liquid water on its surface.

Page 64: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Atmospheres

All the terrestrial planets and the Moon have some atmosphere.

The Moon and Mercury have very thin atmospheres while Venus has the thickest.

Page 65: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Venus at inferior conjunction

Page 66: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 67: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 68: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 69: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Effects of atmospheres

Atmospheric pressure keeps liquids from boiling

Protects the surface from solar wind and cosmic rays and, depending on composition, ultraviolet and x-ray radiation

Moderates surface temperatures

Page 70: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 71: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

How do you think an atmosphere can moderate a planet’s surface temperature?

Page 72: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 73: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

As the Sun shines on the planets surface, it heats the soil and rocks. Without an atmosphere that heat is radiated away mostly in the low-energy infrared region of the spectrum.

If the planet has an atmosphere, the heat can be transferred to the gas molecules and stored, acting as a blanket.

Page 74: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Rank the terrestrial planets (including the Moon) in terms of their daily temperature swings from most extreme to the least extreme?

Page 75: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Surface temperatures

Mercury – day: 425 C night: -175 CMoon – day: 125 C night: -175 C Mars – day: -3 C night: -96 CEarth – day: 15 C night: 3 CVenus – day: 470 C night: 470 C

Page 76: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Discussion

Although Venus is closer to the Sun than Earth, its cloud cover reflects nearly 60% of the light that falls on it. The surface therefore receives less energy from the Sun that the Earth’s surface does.

So why is Venus so much hotter than Earth?

Page 77: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

The greenhouse effect

Carbon dioxide (as well as water vapor and methane) absorb infrared radiation. Sunlight can pass to the surface of Venus and heat it. But the infrared radiation it emits can not escape back into space.

Page 78: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly
Page 79: Terrestrial Planets. Planetary size and heat loss Large planets retain internal heat longer Small planets cool off quickly

Exam next Tuesday

Covers chapters 1-4 in the text + Seasons (p265) and all lecture notes including this week

4 essay questions in which you will be asked to explain concepts

Allowed one sheet of notes with writing on one side only