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Lecture 33

The Solar System. The Inner Planets. The Solar System Overview Terrestrial Planets. Lecture 33. Chapter 16.1  16.8. The Big Bang – beginning of the Universe 12-16 billion years ago. Galaxies are flying away from each other No expansion within galaxies. Our Cosmic Origins.

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Lecture 33

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  1. The Solar System. The Inner Planets. The Solar System Overview Terrestrial Planets Lecture 33 Chapter 16.1  16.8

  2. The Big Bang – beginning of the Universe 12-16 billion years ago Galaxies are flying away from each other No expansion within galaxies Our Cosmic Origins • Only hydrogen and helium in the early Universe • All other chemical elements were created inside stars • We are all created from the stars’ stuff • Current composition of the Sun: 70%H, 28%He, 2%others

  3. Speed of light: c = 300,000 kilometers per second Light year – distance which light travels in 1 year From the Sun to Earth - 8 minutes From the Sun to Pluto - 5 ½ hours To the closest star - 4 years Through the Milky Way - 100,000 years To the closest galaxy - 2,500,000 years Images of Time • The farther away the object, the further back we look in time

  4. Sun within our Galaxy

  5. Appearance of the Milky Way

  6. Content: Sun (the only star) 9 planets Nearly 100 moons Asteroids Comets Free-flying gas and ‘dusty’ particles The Solar System

  7. APOD: 2002 April 29 - Dusk of the Planets http://solarviews.com/eng/homepage.htm Solar System

  8. Temperature (at surface) - 6000 degrees Kelvin (K) Size (diameter) - 1,392,500 kilometers (km) Mass – 1.86 1030 kilograms (kg) or 98% of the total mass of the Solar system Energy production rate – 4 million tons of mass (E=mc2) Age – 4.6 billion years Total stable life time - ~10 billion years The Sun

  9. APOD: 2003 May 17 - Dark Sky, Bright Sun APOD: 2003 March 24 - A Digital Sunset Over Europe and Africa APOD: 2002 July 29 - A Setting Sun Trail Our very own star

  10. Inside the Terrestrial Worlds Two families of planets in the Solar system: terrestrial (Earth-like) and Jovian (Jupiter-like) The terrestrial planets are relatively small and almost spherical The Earth has a radius of 6,378 km and an obliquity of 1/298 They are mostly made of rocky materials that can deform and flow Every object exceeding ~500 km in diameter can become spherical under the influence of gravity

  11. Lithospheres of the Terrestrial Planets Planetary surfaces are all warmed by sunlight, but the high temperatures inside the planets today are due to radioactive heating.

  12. Mercury and Moon The 2 smallest terrestrial worlds covered with lots of impact craters. They have volcanic activity in the past (example - lunar maria). Mercury has a 88-day orbit and a 59-day rotation. Temperature is up to 425oC on the day side and down to 150oC on the night side. It has many craters, but also traces of geological activity.

  13. Venus Venus is the third brightest object in the sky after the Sun and the Moon. Venus has very similar parameters to those of the Earth. However, it spins backwards (clockwise if looking from its north pole). Its atmosphere has 96% CO2, surface temperature 400740 K, surface pressure is 90 times the Earth’s one. It has volcanic activity, but probably no tectonic activity. The Soviet spacecraft Venera 9 landed on Venus and send a panoramic view of its surface. The US Magellan spacecraft transmitted radio images.

  14. Mars This is an intermediate-size planet and the most distant of the terrestrial planets from the Sun. It has polar caps made of frozen CO2, many deserts, and volcanoes. There is no liquid water on Mars today, but rather traces of past water flows. The surface is different in the northern (low plains) and southern (highlands). Only 13 missions to Mars out of 23 were successful.

  15. Summary Terrestrial planets are small and rocky Only a handful geological processes shape the terrestrial planets Every terrestrial world was heavily cratered long ago. Most of the craters are erased now. Understanding of planetary geology might help us learn about planets of other star systems

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