This lesson was created by 2017 PolarTREC teacher Steve Kirsche who took part in the Dynamic Observations of the Microstructural Evolution of Firn expedition. The lesson is intended to introduce students to the concepts of isostasy and postglacial rebound through a demonstration and related instruction. Students will then see how postglacial rebound is an important factor when assessing the
Analogs are used in science investigations to better understand systems we can’t access ourselves. In this lesson, students explore the Dry Valleys of Antarctica to better understand microbial communities on early Earth and what might have been possible on ancient Mars. Students will examine photographs, written descriptions, and artistic renderings of early Earth, the Dry Valley lakes, and
President Obama recently named 102 researchers as recipients of the Presidential Early Career Awards for Scientists and Engineers, the highest honor bestowed by the United States Government on science and engineering professionals in the early stages of their independent research careers. Researcher Samantha Hansen, who worked for two field seasons in Antarctic with PolarTREC teacher Brian DuBay will be one
This video clip from from Alabama TV 13 News profiles PolarTREC researcher Dr. Samantha Hansen's work studying the history of landforms in Antarctica. Dr. Hansen will be one of a hundred scientists to be awarded the Presidential Early Career Awards for Scientists and Engineers.
1) Why is it important to collect large quantities of research data?
2) How can photographing a subject be similar to scientific observation?
3) How can one plot photographic data on a map?
Introduction:
This lesson was written for a Photography I course, to be taught in a lab with access to either a darkroom or computers/printers. The
This student lesson focuses on plate tectonics and large-scale system interactions, utilizing PolarTREC teacher Brian DuBay's Transantarctic Mountains expedition videos.
Objectives: The student will investigate, make observations, and analyze geologic processes of plate tectonics.
Key concepts include:
a) how geologic processes are evidenced in Antarctic mountains;
b) tectonic processes (compressional, tensional, and transversal forces).
Adapted by Michelle Brand Buhanan for
Founded in 1984 with support from the National Science Foundation, IRIS is a consortium of over 100 US universities dedicated to the operation of science facilities for the acquisition, management, and distribution of seismological data. This weblink is directed to their education and public outreach resources.
This website is an overview on the Transantarctic Mountains with information on geography, geology, mechanisms for formation, issues, and additional references.
The Roof at the Bottom of the World: Discovering the Transantarctic Mountains comprehensively documents the 1,500-mile length of the Transantarctic Mountains. It is the first atlas of the most remote mountain range on Earth. The presentation is historical, following a narrative of the voyages and traverses of those parties that were first to behold new lands.
The Transantarctic Mountains are an extreme example of rift flank uplift, extending over 3500 km across Antarctica and reaching elevations up to 4500 m (see map of the region). The mountain range was formed in the extensional environment associated with the breakup of Gondwanaland. Geological and geophysical work has shown that the Transantarctic Mountains developed along a long-lived lithospheric boundary