GSA 2012 meeting, Day 3

During day 3 of the GSA meeting I attended several talks, including part of a session on the geologic maps of Vesta being produced as a result of NASA’s Dawn spacecraft mission. Vesta’s surface has been divided into 15 quadrangles and apparently a different team is assigned to map each one. I have to admit it was entertaining to hear them argue over who had the coolest quadrangle to study. There were lots of possibilities, since like so many bodies in our Solar System Vesta is much more complex than anyone imagined. For example, Debra Buczkowski et al. described a high-density area called Vestalia Terra which they suggest may be one of the geologically oldest areas on Vesta, while Jennifer Scully et al. examined elongated troughs (“fossae”) that may be structural shear features.

In the poster session, Matthew Vrazo et al. reported a rich deposit with numerous specimens of the “sea scorpion” Eurypterus (top) from the Silurian of Pennsylvania. Many of these appear to have been molted carapaces.

In what may be the most timely poster ever (keep in mind that abstracts were submitted several months ago), Alan Benimoff et al. modeled the effects of storm surges in the New York-New Jersey-Connecticut area. Quoting directly from their abstract: “Our simulation suggests that even relatively minor tropical storms, striking the area with the right track and tidal combination, can produce substantial flood-related damage and destruction to shipping channels, industrial and sewage plants, subways, bridges, and high rise buildings.”

In a rather disturbing study, Anjian Wang and Shanqin Ni found elevated levels of copper,  lead, zinc, molybdenum, arsenic, and cadmium in the hair of children living downstream from mining areas on the Lean River in China. In most cases the average levels were not considered unsafe, but the concentrations were highly variable.

Rachel Racicot used CT scans to examine the ear region of several extant and extinct porpoises, finding some differences within the group in the semicircular canals and vestibules. It’s not clear if these differences reflect phylogenetic or behavioral differences.

There was a whole aisle of posters today on “The Math You Need, When You Need It”, including some by Jen Wenner and Eric Baer, Jacquelyn Hams, Gretchen Miller, Elizabeth Gordon, Kyle Fredrick, and Meredith Denton-Hedrick. It really is a good program.

Brett’s Physical Geology class at Patrick Henry Community College was supposed to meet this afternoon, but of course she’s here in Charlotte. So for class Brett did a video conference with her students from the poster session. Several other geologists volunteered a few minutes of their time to explain what they do and their impressions of the conference, and to answer questions.

 

There was lots more today, but it’s late, and there are election returns still coming in. We’re planning to stay for most of tomorrow’s sessions as well, and return home tomorrow evening.

 

About these ads
This entry was posted in Conferences and tagged . Bookmark the permalink.

One Response to GSA 2012 meeting, Day 3

  1. George says:

    Butch as a toxicologist the heavy metal ore mines are a major polluter to ground water and drinking supplies. They also add a contamination burden to the air. Certain mines donot pollute since they dig out a sedimentary rock such as limestone and the heavy metal burdon is low. With sandy hitting besides sewage spewing out that has viruses and bacteria the underground tanks some of which have been abandoned for years start to leak and add heavy metals, solvents, PCBs, pesticides etc into creeks streams lakes sewage systems and the overflow gets out to the bays and ocean.

Leave a Reply

Fill in your details below or click an icon to log in:

WordPress.com Logo

You are commenting using your WordPress.com account. Log Out / Change )

Twitter picture

You are commenting using your Twitter account. Log Out / Change )

Facebook photo

You are commenting using your Facebook account. Log Out / Change )

Google+ photo

You are commenting using your Google+ account. Log Out / Change )

Connecting to %s