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 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
Follow the link in this article to hear an audio recording about PolarTREC teacher Glenn Clark's preparation for a trek to the Totten Glacier System in Antarctica this winter.
This one hour webinar is conducted by PolarTREC alumni Missy Holzer. She highlighted her work with the High Arctic Change expedition 2008 and bringing inquiry-based science into her classroom. This webinar is part of the C-ISE online professional development course.
This website is produced by the geological mapping programme GEOKART of the Norwegian Polar Institute. We want to provide information for geologists working or interested in the Norwegian polar areas, with emphasis on Svalbard (Spitsbergen).
We want to inform about: NPI's geological programmes, activities, services and products, logistic requirements and working conditions in polar areas, ongoing activities, and basic scientific
This geologic time calculator allows the user to manipulate the relativism of time to other markers. It builds from the classic analogy for illustrating the relative durations of parts of the geologic time scale is the yardstick.