PROGRESS
To date, I have described five lithofacies present in the Salona and Coburn formations. Two
lithofacies are interpreted as storm deposits and make up the limestone component of the
thinly-bedded couplets. Some trends were observed in the raw data; however, because of the
“noisy” nature of the data, a plot of the five-point moving average of bed thickness was
created to define the cycles better.