An update from Emma, a geology and mathematics major:
I woke up on our last day in Jamaica at 7 am to finish my final paper. I was in the sediment group, and we analyzed the sand on the beach to determine its angle of repose, porosity and density, with the ultimate goal of determining the probability of slope failure in and around Kingston Harbour.
One of my jobs was to conduct a statistical analysis on all of the data we collected. I calculated the mean, standard deviation and coefficient of variation for the angle of repose for sediments of varying water content.
At 8 am everyone ate breakfast, then packed up to return to Kingston for our final night. On the drive back, we stopped in Yallahs for some traditional Jamaican Jerk and continued on to Judgement Cliff. The cliff was created in 1692 by a landslide caused by the same earthquake that destroyed Port Royal. It is an enormous landslide.
When we arrived in Kingston we dropped off our seismic and surveying equipment at the University of the West Indies campus, toured the Earthquake Unit where Lyndon works and then went to Usain Bolt’s restaurant, “Tracks & Records,” for dinner.
After dinner we all listened to Brett and Gwen’s presentation. They were part of the surveying team and had integrated our angle of repose results with their surveying analysis to assess slope stability at Port Royal. In their presentation they came to the preliminary conclusion that only a magnitude ~5 earthquake near Kingston is necessary to cause slope failure in Port Royal. Further analysis is necessary, but their conclusion – based both on experimental and theoretical data – closely matches historical observations.
I have had an amazing time in Jamaica and learned so much. I am on the 730 flight back to Dallas, so I will be in bed early!