Ch. 28 Sec. 2 The Moon
Reaching for the Moon Soviet Union launched Sputnik I in 1957 –First step into understanding our space 1961, Soviet astronaut Yuri A. Gagarin became first human in space U.S. Project Mercury launched first American, Alan B. Shepard, in space: 1961 1969, Apollo Program landed Armstrong and Aldrin on the moon: Apollo 11
Lunar Properties Our moon, one of the largest known moons Only moon for the inner planets Only moon that is solid and rocky, others are ice Moon is 27 % of Earth’s radius
Lunar Surface Lunar surface is quite dark –The albedo is only.07% reflective –Albedo is the amount of sunlight reflected –B/c of no atmosphere: 127 o C in sunlight -173 o C in darkness
Lunar Surface No erosion except that of other impacts Highlands –Light in color –Mountainous: heavily covered with craters –Impact craters: Ejecta and Rays
Lunar Surface Mare or Maria –Dark smooth plains –Rilles: valley like structures
History of Moon Moon is aged from bil. Yrs. Old Moon heavily bombarded in first 800 mil yrs –Resulted in breaking & heating of rocks –Formed loose ground layer known as regolith
Moon tectonics Infer from seismometer data that moon has layers B/c of known volcano activity & magnetic field, little to no tectonic act. On moon
Moon formation Theories Capture Theory –Beginning of solar system, an object ventured to close to earth –Got caught in the gravity field –Problem: earth and moon of similar elements If came from somewhere else, would be different elements
Moon formation Theories Simultaneous Formation Theory –Earth and moon formed in general area and the same time –Moon did not have to be slowed down –Problem Different accounts of Iron on moon than Earth
Moon formation Theories Impact Theory –Gigantic collision on earth that ejected into air –Materials merged together to form the moon –Iron deficient crust and all water would have evaporated on collision
Impact Theory