the size of a crater and its characteristics. To make the craters, I used several balls and both threw them up in the air and also shot them into the sand at a local beach with a slingshot. The balls varied in density, mass, and velocity. Density was the only variable that had a distinct correlation with the size of the impact craters, with the densest balls consistently making the largest crater relative to their size. Mass had no consistent effect with crater sizes varying greatly. Velocity did have an effect with the slowest ball (a ping pong ball) making the smallest crater. This ball was also the least dense so future work will be necessary to vary the velocity in the more dense balls as well. The impact craters produced a lip higher than the surrounding sand, similar to craters observed on the moon. Last updated: March 4, 2010 | |||||||||||||
Copyright ©2007 Woods Hole Oceanographic Institution, All Rights Reserved, Privacy Policy. |