Transcript Day 17
Announcements •The last 1st Quarter Observing Night is tomorrow night. Starts at 7:30pm so set-up begins at 6:45pm. Meet here at that time. We will set-up in the Atrium with a few Dobs outside if it is clear. •Don’t forget the second project. Presentations are two weeks from today. •Exam 3 is Tuesday May 3 at 4:00pm. Will cover Chapters 8 & 9. Sample questions are posted. Understanding the rings of Saturn Galileo had observed Saturn in 1610 and noted strange appendages With a better telescope, Huygens figures it out In 1659 Christian Huygens figure out that the strange appendages of Saturn were rings Giovanni Cassini discovers gaps in the rings in 1675 A smaller gap in the A ring is named in honor of Johann Encke for his studies of the rings in the early 1800’s In 1850, with one of the new refractors, William Bond discovered the C- ring of Saturn His son, George Bond, though he saw changes in the rings and proposed they were a fluid James Clerk Maxwell finally solved the riddle: they are independent particles in orbit He published his theory in a paper titled On the Stability of The Motion of Saturn’s Rings in 1859 The Search for Planet X Percival Lowell did calculations on the orbits of Uranus and Neptune and deduced there must be a 9th planet “out there” Lowell hired a young Clyde Tombaugh to look for Planet X Tombaugh used a blink comparator to search his images for moving objects After several years, Tombaugh discovered Pluto The birth of the solar system Laplace had proposed what became known as the nebular hypothesis in 1796. The theory had problems. The biggest problem was the angular momentum problem Thomas Chamberlin proposed that a passing star had pulled material off the Sun to create the planets Hannes Alfven in the 1960’s proposed a magnetic fields solution to the angular momentum problem Theories on the formation of the Moon Prior to the Apollo days one of the theories for our Moon was the Capture theory Major problem: this requires a third body to take away some angular momentum or the Moon just drifts by The co-accretion model was another theory This would make the moon’s composition identical to Earth’s. Rocks brought back by the Apollo missions showed subtle differences from Earth rocks thus killing this theory. The spin-off theory was the third theory A rapidly rotating molten Earth flings off a blob which forms the moon Again, composition should be identical to Earth. After Apollo a new theory emerged The Giant Impact model forms a moon with almost (but not quite) the same composition The Giant Impact also explains our axial tilt It means the Moon was once much closer to Earth