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Earth typical (and not!) terrestrial planet Agenda:  Core  Geology  Atmosphere.

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Presentation on theme: "Earth typical (and not!) terrestrial planet Agenda:  Core  Geology  Atmosphere."— Presentation transcript:

1 Earth typical (and not!) terrestrial planet Agenda:  Core  Geology  Atmosphere

2 How much of the mass of the solar system is contained within the Sun? A. 63% B. 25% C. 75% D. 99% E. Cannot conclude

3 Home, sweet home

4 Terrestrial planets Differentiated core/crust  Geological activity? Atmosphere Few moons

5 Differentiation metals Silicates, oxides Granite, Basalt, quartz

6 Geologic activity is driven by internal heat

7 More Hawaiian islands are being built right now!

8 The crust is made of plates These plates move around! Wikipedia

9 Plates can pull apart

10 Pulling apart

11 Plates can jam under one another

12 Pushing together – caused 2004 tsunami

13 2004 Tsunami

14 Plates can slide parallel

15 San Andreas fault Moving parallel

16 Earth’s crust is 10-20 miles thick. Have we drilled through it? A. Yes B. No C. Cannot conclude

17 The atmosphere

18 Absorbs ultraviolet Absorbs x-rays Height (Km)

19 Greenhouse effect Atmosphere as blanket

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22 CO 2 concentrations and temperature

23 Evidence for global warming Retreat of glaciers (worldwide) Severe drought (worldwide) Increased surface temperature Melting of polar ice caps  (rising of sea levels) Consensus in peer-reviewed journal articles

24 Retreating glaciers

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26 Katrina

27 Work of Katrina

28 Polar ice caps are melting polar ice cap movie 1979-2005

29 Polar ice caps are melting 1979-2005 (NASA)

30 It’s not the Sun’s fault...at least not mainly.

31 Summary Earth is differentiated Geologically active Atmosphere plays many roles Global warming is occurring

32 Team activity #15 Mapping the solar system from Earth


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