| Shakira 
                    Brown-Petit traveled to and worked at a remote Antarctic field 
                    camp called Offshore New Harbor as an educator with Dr. Stephen 
                    Pekar's Offshore 
                    New Harbor Expedition. The Offshore New Harbor team conducted 
                    seismic and gravity surveys as part of an effort to study 
                    Antarctica's distant past. The goal of the Offshore New Harbor 
                    (ONH) Project is to study sediments deposited in Antarctica 
                    during the  
                    Greenhouse World. The team lived and worked on the sea 
                    ice in tents for approximately 35 to 40 days. It is from this 
                    extremely remote location that Shakira Brown-Petit did webcasts 
                    and video conferencing to teach students about what the team 
                    is learning from their work as part of the ARISE program (ANDRILL 
                    Research Immersion for Science Educators). More information 
                    on Antarctica's past transition from "Greenhouse World" 
                    to "Icehouse World" can be found  
                    here. The 
                    Offshore New Harbor project is a program of  
                    ANDRILL (ANtarctic geological DRILLing). As described 
                    on their website, ANDRILL is "a multinational collaboration 
                    comprised of more than 200 scientists, students, and educators 
                    from five nations (Germany, Italy, New Zealand, the United 
                    Kingdom and the United States) to recover stratigraphic records 
                    from the Antarctic margin using Cape Roberts Project (CRP) 
                    technology. The chief objective is to drill back in time to 
                    recover a history of paleoenvironmental changes that will 
                    guide our understanding of how fast, how large, and how frequent 
                    were glacial and interglacial changes in the Antarctica region." |