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.
Abstract
Science, Technology, Engineering, and Math (STEM) disciplines have become key focus areas in the education community of the United States. Newly adopted across the nation, Next Generation Science Standards require that educators embrace innovative approaches to teaching. Transforming classrooms to actively engage students through a combination of knowledge and practice develops conceptual understanding and application skills. The partnerships between
This lesson/project/lab has students predict via multiple drawings and time lapse photography predictive Flubber flow before the placement of barriers and other obstacles in front of the Flubber. Contour lines in two directions are drawn on both the paper prediction and the Flubber for comparison purposes.
Following predictive drawing completion glacier flow (Flubber flow), with obstacles in place