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Last year I first got involved with my research on a trip to Assateague Island, MD where a team of geologists from George Mason were collecting sediment core samples of relict (ancient) inlets. Unsure that this weekend of fieldwork would turn into a yearlong project, I have gained a tremendous amount of priceless experience working both in the lab and out in the field. I have become familiar with many geological tools and multiple coring techniques that few undergrads have the opportunity of and have been given a head start into the research process that I hope to one day continue in graduate school.
For my study, I have had the chance to analyze a shore parallel transect of sediment cores from the former Sinepuxent Inlet of Assateague Island, Maryland. The core technique I used for this research project is known as a pulse auger. Essentially, this tool works like a plunger that is able to pull sediment samples up from different depths at certain intervals until the core tube cannot go down any further or a depth of 8 meters is reached. Everyday in the lab I sieve through hundreds of sand grains to sort them by size and weigh them. By doing this for each sample depth I am able to reconstruct visually through statistics any trends within the core. Trends within sediment cores tell a story and from participating in this research I am contributing to a better record of Assateague Island’s geologic history.