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
Local news interviews PolarTREC teacher Nell Herrmann about her expedition to Palmer Station, Antarctica. The take a visit to her classroom as well. Video and written article are included.
PolarTREC teacher Juan Botella is interview by a local news station about his work on the NB Palmer. Juan discusses ocean circulation and changes affecting marine organisms. Video and article included.
The Dry Valleys region in Antarctica is known as the coldest, windiest, driest place on Earth. Beacon Valley is famous for its katabatic winds which can routinely knock fit adults and PolarTREC teachers to the ground. This lesson was created by PolarTREC teacher Jacquelyn Hams who experienced the cold and the full force of the winds in 2008