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

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RESEARCH ASSOCIATES<br />

Daniel Curewitz<br />

Introductory<br />

Oceanography (EAR<br />

117), Volcanoes and<br />

<strong>Earth</strong>quakes (EAR<br />

200), and <strong>Earth</strong>’s<br />

Climate (EAR111)<br />

have rounded<br />

out my teaching<br />

schedule quite<br />

nicely. In addition<br />

to developing and<br />

modifying lectures<br />

Plaid shirt - icon <strong>of</strong> a geologist! for the courses, I<br />

am working on new ways to give students hands-on<br />

exposure and practical experience with the concepts<br />

and ideas that underlie the teaching material, mostly<br />

through the development <strong>of</strong> recitations and in-class<br />

activities. One aspect <strong>of</strong> teaching these courses<br />

that has been particularly rewarding is the focus on<br />

visual learning and the interpretation, deconstruction<br />

and creation <strong>of</strong> diagrams, charts or other means<br />

<strong>of</strong> absorbing and communicating <strong>Earth</strong> <strong>Sciences</strong><br />

concepts.<br />

I continue to delve into long- and shortterm<br />

mechanical connections between faulting and<br />

hydrothermal activity through detailed investigation<br />

<strong>of</strong> more than 40 years worth <strong>of</strong> maps and data from<br />

the mid-ocean ridge hydrothermal systems exposed<br />

in the rift zones along the Mid-Atlantic Ridge, where<br />

it emerges and forms the Eurasian-North American<br />

plate boundary in Iceland. Transporting the insights<br />

gained from investigation <strong>of</strong> on-land, heavily mapped<br />

and monitored areas into the deep frontiers <strong>of</strong><br />

hydrothermal research along the submarine sections<br />

<strong>of</strong> the mid-ocean ridge system is the next phase <strong>of</strong><br />

the work, and it is just over the horizon and will<br />

continue through the next year <strong>of</strong> investigation.<br />

Ultimately, the work is intended to incorporate ideas<br />

and results from previous research into structural<br />

control <strong>of</strong> hydrothermal activity, the geological impact<br />

and expression <strong>of</strong> dike intrusion at divergent plate<br />

boundaries, and fault population analysis <strong>of</strong> active rift<br />

systems.<br />

Jennifer Hargrave<br />

I’ve completed my first year at SU as part <strong>of</strong><br />

the Lacustrine Rift Basins research group led by Dr.<br />

Chris Scholz, which included a second trip to the<br />

southeastern shores <strong>of</strong> Lake Turkana, Kenya. For<br />

this trip, I spent two months around the village <strong>of</strong><br />

Loiyangalani in search <strong>of</strong> lacustrine carbonates. Our<br />

living conditions improved from last year, from palm<br />

huts in a campsite to the Oasis Lodge which was<br />

complete with a warm spring-fed pool. We were<br />

able to interact more with the villagers, and several<br />

were employed to help us with our research. A group<br />

<strong>of</strong> us also visited a local secondary school to share<br />

with them our interest in Lake Turkana. A few <strong>of</strong> the<br />

students were particularly interested in geology and<br />

had rocks to share with us.<br />

The trip was a very successful one, as we<br />

doubled our study area and collected and mapped<br />

numerous outcroppings <strong>of</strong> stromatolites, as well as<br />

ash layers which we will use to date and correlate our<br />

sections. In addition to the onshore fieldwork, I also<br />

assisted in the collection <strong>of</strong> <strong>of</strong>fshore cores, acquisition<br />

<strong>of</strong> multichannel seismic data, and dredging.<br />

Jen is discussing the rocks that are commonly<br />

found around Lake Turkana at a local secondary<br />

school in Loiyangalani. Photo by M. Hicks<br />

We presented our preliminary findings at the<br />

annual AAPG meeting in New Orleans in April and<br />

generated a lot <strong>of</strong> interest among our sponsors last<br />

November. We are currently analyzing our newly<br />

collected data to produce a depositional model <strong>of</strong> the<br />

lake system.<br />

Joseph Kula<br />

It has been a challenging and exciting<br />

year working here at <strong>Syracuse</strong> University, and<br />

in conjunction with the New York Center for<br />

Astrobiology. Degassing experiments on crystalline<br />

jarosite have been started to constrain the diffusion<br />

kinetics <strong>of</strong> radiogenic 40 Ar through the mineral. A<br />

primary goal <strong>of</strong> these experiments is to determine the<br />

argon closure temperature for jarosite and to evaluate<br />

any potential diffusive loss from the mineral over

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