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alumni reception - Syracuse Universe Department of Earth Sciences ...

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Evolution in Grenada, Spain and a workshop on<br />

thermal modeling in Aussois, France. Despite that,<br />

and the ever expanding job as Director <strong>of</strong> Graduate<br />

Studies, we managed to publish papers on the Basin<br />

and Range Province (Tectonics, GSA Special Paper),<br />

the Pyrenees (<strong>Earth</strong> and Planetary Science Letters),<br />

the Transantarctic Mountains (Tectonics) and the<br />

Adirondacks (GSA Bulletin) with other papers<br />

(Pyrenees, Alaska) in various stages <strong>of</strong> revision. The<br />

summer <strong>of</strong> 2010 will end with a group <strong>of</strong> us attending<br />

the 12 th International Thermochronology Conference<br />

with activity, including new non-toxic, water-based<br />

mineral separation techniques.<br />

Perhaps the biggest news from Hoke’s corner<br />

is that I landed my first major NSF grant from<br />

Campsite close to the Sesitna Glacier.<br />

in Scotland where I am one <strong>of</strong> the keynote speakers.<br />

PhD students Josh Taylor and Stephanie Perry are<br />

in the final stages <strong>of</strong> writing up their extensive<br />

thermochronology-tectonic PhD’s with both accepting<br />

positions at Exxon.<br />

Gregory Hoke<br />

I just finished my first full academic year at<br />

<strong>Syracuse</strong>, complete with two graduate students to<br />

guide though their respective M.S. projects in tectonic<br />

geomorphology. Needless to say, it was an eventful<br />

year. Both <strong>of</strong> my students are working at elevations<br />

≥ 3000 m (9,900 ft) in the Andes near Mendoza,<br />

Argentina. In order to take advantage <strong>of</strong> the warm<br />

summer conditions at these altitudes, we all spent New<br />

Year’s Eve in the air on our way to Argentina for 3<br />

weeks <strong>of</strong> very productive fieldwork.<br />

While in Argentina, I also began a pilot project<br />

with a collaborator at the University <strong>of</strong> Washington,<br />

instrumenting soil pits over a range <strong>of</strong> elevations and<br />

collecting samples to measure the temperature <strong>of</strong> soil<br />

carbonate formation, using a relatively new technique<br />

called “clumped isotope thermometry.” Back at<br />

<strong>Syracuse</strong>, the tectonic and geomorphology lab is busy<br />

Advisor, field guide and cook!<br />

the Tectonics Program. The project titled, “Basin<br />

evolution and elevation history <strong>of</strong> the SE margin<br />

<strong>of</strong> the Tibetan Plateau: constraints on the timing<br />

and mechanisms <strong>of</strong> surface uplift”, is a three-year,<br />

$365,000 (SU part) endeavor with collaborators from<br />

the University <strong>of</strong> Rochester, University <strong>of</strong> Michigan<br />

and the Institute <strong>of</strong> Tibetan Plateau Research in<br />

China. Last fall I was invited to participate in a oneday<br />

symposium on mountains at Cornell University,<br />

chaired a topical session at the annual GSA meeting in<br />

Portland Oregon, and gave an invited talk on my work<br />

in the Altiplano at AGU. I am a co-author <strong>of</strong> a paper<br />

in press in the journal Tectonics and am currently<br />

contributing to several manuscripts. This fall I will<br />

attend the IAS congress in Mendoza, Argentina where<br />

an Argentine undergraduate I helped supervise will<br />

present her work.<br />

Linda Ivany<br />

I took a semester-long sabbatical this past<br />

spring after ten years and four consecutive semesters<br />

teaching the <strong>Department</strong>’s largest survey course, EAR<br />

105, <strong>Earth</strong> Science. During the sabbatical, I made<br />

significant progress on manuscripts with students<br />

and colleagues. A paper with former student Andrew<br />

Haveles (M.S. 2009) is in press at Palaios. Derived<br />

from Andrew’s thesis, the paper uses high-resolution<br />

stable isotope analysis on fossil mollusks from the US<br />

Gulf Coastal Plain to reveal how changes in growth<br />

rate led to larger body sizes in a famous Eocene<br />

unit called the Gosport Sand. A paper stemming

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