We are all teachers and students throughout our lives – even as adults we are students and even as children we are teachers. As adults, we are often afforded unusual opportunities to learn as we push ourselves in our interests and abilities. Through these opportunities—both expected and unexpected—our own understanding of what is possible expands as well as our desire
Teacher David Thesenga and the Ice Shelf Flow and Fracture Dynamics Research Team discuss field work on the McMurdo Shear Zone (SZ) live from Antarctica.
The Follow A Researcher (FAR) website from the University of Maine will be releasing weekly videos starting the first week of October closely following the Ice Shelf Flow and Fracture Dynamics Expedition in Antarctica.
PolarTREC alumna Susy Ellison talks about her two expeditions and how they affected her personally and professionally. Researcher Jeff Rasic joins in to talk about what it was like to have a teacher in the field for the Early Human Settlement in Arctic Alaska 2011 expedition.
Through this demonstration and review of the attached research documents and the expedition PolarConnect event archive you will better be able to visualize how warming deep ocean currents undermine the ice sheets of Antarctica.
Objectives
To determine, through a demonstration and review of a scientific abstract, how warm water currents speed up ice sheet loss and sub-ice
As a teacher on the NB Palmer Totten Cruise in the winter of 2014, I successfully traversed the Magnetic South Pole. This is a wandering point on the Earth’s surface where geomagnetic field lines are directed vertically upwards. As an Outdoor Educator I utilize compasses regularly to navigate. The traverse of the Magnetic South Pole inspired this lesson
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
Ground penetrating radar is an important tool for studying glacier dynamics. Glacier scientists use GPR images to analyze attributes of glaciers. The following research activity will familiarize students with the basics of the different types of glaciers and their dynamics along with ground penetrating radar and its use in glacier studies.
This is part two of a small series following Parishville-Hopkinton Central School science teacher Glenn W. Clark’s involvement last winter in the National Science Foundation’s 2013-2014 Antarctic Research Consortium research trip to Eastern Antarctica. Since his return to the north country last spring, he has been educating the public about the excursion in a three piece presentation on science, expedition