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In my geology classes at ����TV we are always learning about how the world is actively changing around us, so from the get-go I was determined to seek out field trip and research opportunities. It was surprisingly easy to get involved and I quickly began doing research with Professor Darren Larsen. Here I was able to build on what I had learned in his previous classes: “GEO 245: Earth’s Climate Past and Future” and “GEO 315: Sedimentary Geology.”

This all led up to a ten-day research trip to Iceland early in June, 2018, where Professor Larsen, fellow student Samuel Sachs ’21 and I studied the active soil erosion occurring in the central highlands. Our ultimate goal was to discover the driving force behind the rapid desertification of Iceland and pinpoint the exact time period when this phenomenon began. By the end of the trip we had begun mapping the extent of the soil erosion to demonstrate how anthropogenic activities, such as the introduction of grazing livestock, are the catalyst for this phenomenon.

Since we were only there for a short amount of time, we got right to work, driving straight to the field site from the airport. We were there around the time of the summer solstice so it was light 24 hours a day and we were able to work around the clock, which was both exhausting and exhilarating. Over the first week of the trip, we dug 7 full soil sections, each containing the last 12,000 years of time. We found a lake that we later learned has never dried up and sampled roughly 6m of mud that also covered the last 12,000 years of time.

In order to begin answering our research questions, we needed to have a historical understanding of the highlands. Being able to get involved with research so easily on campus and how well it paired with our classes throughout the previous semester gave us the background we needed for the trip. We learned that since the last glacial period in Iceland, around 12,000 years ago when ice covered the entire central part of the island, the geological record relating to this project was found in 2 places, the soils and lake sediments (a geological record is the history of the last 12,000 years of geologic activity occurring in Iceland).

As we were researching the effects of livestock grazing on soil erosion, we knew the vegetation was being eaten away, the soil was being eroded and then transported around the highlands due to wind erosion. These eroded sediments, including tephra grains from volcanic ash, were then being transported around the highlands until they accumulated in newer soils and lakes. Thus, on the field mission, we spent a lot of time deep in the soils targeting soil sections with areas of large reworked tephra grains.

In addition to completing our scientific goals for the trip, we were able to see some of Iceland’s breathtaking waterfalls and vistas that were near our field location. We were in the country for 12 days in total, and surprisingly interacted with very few locals as we camped each night in the highlands, where there are very few inhabitants. It turned out that during the World Cup almost 15 percent of the entire population had gone to Russia to watch the Icelandic team compete!