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.
Students will develop research questions that will help them develop an ecosystem profile (species/conditions etc.) of a local pond. Their results will be compared with data from the McMurdo Dry Valley Lakes in Antarctica. Discussions about climate and energy dynamics will be conducted as conclusions are drawn. A map and key for the local pond (species/locations/conditions) will be
During this lesson, students will learn basic glacial features and how to interpret Topographic maps and satellite images in order to create a model replica of a glacier valley. The Dry Valleys of Antarctica have classic glacial features, both in the barren valleys and in the remaining glaciers in the area. The glaciers are a major contributor to