As technology advances, the way in which geologists study the Earth also advances. Some of these new technologies also make it possible to bring aspects of the field into the classroom. This opens up opportunities for broader audiences to explore a wider range of geologic structures and localities. Structure from motion (SfM) is one of these technologies that is
As science and technology continue to advance, the ways in which scientists and engineers study the surface of the Earth and how it will change in the future, changes along with it. The field of climate change science is continuing to benefit as advances in technology lead to a greater understanding of
The Science of the PolarTREC “Sliding Glaciers” Expedition
PolarTREC (Teachers and Researchers Exploring and Collaborating) is a program in which educators from the United States, both formal and informal (i.e. educators in museums, science centers, etc.) spend 3-6 weeks participating in hands-on field research experiences in the polar regions. The goal of PolarTREC is to invigorate polar science education and
PolarTREC teacher and Rutgers University Geology Museum Director, Dr. Lauren Neitzke Adamo featured in a news release in Rutgers Today and EOAS Website.
Article about Dr. Lauren Neitzke Adamo, co-director of the Rutgers University Geology Museum, and her upcoming expedition through PolarTREC, in the Swiss Alps to study the impact on glacier melting.
This lesson was created by Rebecca Harris after being a part of the Arctic Glacial Lakes PolarTREC Expedition. She was inspired by how important suspended sediment, something so often overlooked by non scientists, was for developing paleoclimate models as well as ecosystems. Students will observe a watershed or a model of a watershed to make predictions about what might
This lesson plan was created by after being a part of the Arctic Glacial Lakes PolarTREC Expedition. I was inspired by the massive amount of data collected over the course of the research project and the complexity of hydrology in glaciated and non-glaciated basins in the Brooks Range of Alaska. Students will work together to make hypotheses about patterns