S EARTH ORIGIN P * % of Earth’s History 78.0% 43.0% 9.3% 8.0% 3.8% 0.1% S If we compare the history of the earth to a trip from College Station to Bush Intercontinental (100 miles), the earliest human ancestors would show up 117 yards from the entrance - barely the length of a football field. S Order of Planets from the Sun Sizes are Relative Distances are not Accurate S Order of Planets from the Sun Sizes are Relative Distances are not Accurate S Milky Way Galaxy S QuickT ime™ and a P hoto CD Decompressor needed to use this pict ure Decay Products of U235 P Half-life = the time it takes for half of the parent to decay into the daughter QuickT ime™ and a S P hoto CD Decompressor needed to use this pict ure Long half-life Slow Processes Short half-life Fast Processes P Earth’s Atmosphere Changes S Life on Earth • Earliest known evidence of life was about 3.6 billion years ago • Early life may have started in the intertidal zone or at black smokers Intertidal Algae S Deep-sea Black Smoker P Life on Earth • Evidence suggest the composition of seawater has changed little over the last 600 million years • Mass extinctions have occured over time. Why? S Moon Craters S Impact Craters in Canada S Most impact craters would be in the oceans P P Life on Earth • Impacts from extraterrestrial bodies – the latest big one was at the K/T boundary about 66 million years ago – it corresponds with the extinction of the dinosaurs – in 1991 bull’s eye pattern of gravity variations was detected off northern Yucatan (Chicxulub) – the circle was 180 km in diameter P Life on Earth • other more recent events include: – Winslow, Arizona about 50,000 years ago leaving a crater 4,000’ wide and 750’ deep - caused by an object 135’ in diameter traveling at 12 miles a second with an explosive force of 15 megatons – Tunguska, Siberia - 1908 - no crater, extensive damage, 10 megatons, site not visited for 20 years S Meteorite Crater near Winslow, Arizona