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By Michael M. Burrell

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Diagram of setting Sun, as viewed from north of the Earth. Fig. 2-4. 4. Diagram of setting Sun, and the Moon overhead for observer on the Earth. Which declinations can be observed from the North Pole? the South Pole? the equator? Which right ascensions can be seen from the above locations each day? From the North Pole, declinations 0–908 north can be seen. From the South Pole, declinations 0–908 south can be seen. From the equator, all declinations can be seen. Since the Earth rotates completely around its axis in one day, all right ascensions can be seen from every location on the Earth every day.

This region is called the weird terrain. The density of Mercury is greater than the density of the Moon (Mercury ¼ 5,420 kg=m3 , Moon ¼ 3,340 kg=m3 ), so it must have more heavy elements than the Moon. One explanation is that during a collision with a large planetesimal, part of the mantle was blown away. Very little of Mercury’s primordial atmosphere remains. The current atmosphere is very thin (less than 106 particles/cm3 ), and mainly formed from solar wind particles trapped by Mercury’s magnetic field, and from recently released atoms from the surface.

Ans. 22. When the Moon and the Earth become locked in completely synchronous rotation (‘‘tidally locked’’), how many orbits will the Moon make in one Earth day? Ans. 23. When the Moon and the Earth become locked in synchronous rotation, will lunar observers see the Earth pass through phases? will Earth observers see the Moon pass through phases? Ans. 24. E. What is the advantage of an analog camera over a digital camera? Ans. 31. No In what year (approximately) will Vega again become the ‘‘North Star’’?

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