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A 1 kilometer asteroid probably strikes the Earth every few million years, while a global killer on the order of 5-10 kilometers strikes the Earth every few hundred million years. A 100 meter asteroid may strike the Earth every thousand years (Cooke, 2004). In fact, in 1908, a 60 meter asteroid exploded in the upper atmosphere over a remote area in Eastern Siberia (Tunguska) and flattened trees for thousands of square miles. A high-velocity impact of a 2 kilometer asteroid with the Earth could kill a billion people. A ten kilometer asteroid impacting the Earth could extinguish us as a species (Foster, 2005). The odds of the Earth suffering a catastrophic collision with an asteroid over the next century is roughly estimated at 1 in 1500 to 1 in 5000 (Schultz, 2001). The probability of being killed by an impact event is very small on the order of 1 in 10,000 to 1/100,000. Driving and overeating are far bigger risks to the average individual.

Impacts by smaller objects are much more common than those of large objects. Smaller objects could produce destructive tsunamis, directly strike a large city, or explode over a large populated area killing millions of people. Fortunately, the Earth’s atmosphere provides an increasingly protective role as objects become smaller. Most meteoroids fragment into small relatively harmless pieces as they travel through the atmosphere at high speeds. Even a very solid mainly metallic asteroid fragment probably needs to be 100 meters in diameter for it to survive passage through the atmosphere intact (Cooke, 2004).

Satellites operating for the United States Department of Defense have been monitoring the Earth for nuclear weapons and missile launches for several decades. Their sensors in visible and infrared light can detect flashes of light from meteoroid atmospheric impacts. Five kiloton equivalent (Hiroshima atomic bomb size) impact events occur in the Earth’s atmosphere every year, but we are saved from harm by the Earth’s atmospheric blanket.
 

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