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Brown: NeMO Net |
Science News | ||||
NOAA Ship Ron Brown - ROV Cruise |
R/V Wecoma - CTD Cruise |
Teacher Logbooks | ||||
NOAA Ship Ron Brown - Jeff Goodrich The scientists are gathering mounds of data about the dynamic nature of Axial Volcano and it's hydrothermal vents. However, for a deeper understanding of this complex tectonic system, snapshot science really doesn't cut it. Continual monitoring or monitoring during eruptive events is ideal. This process has already been started. In 1998 a rumbleometer, a device that measures vertical displacement and temperature, detected inflation and deflation of the volcano during the eruption. More...
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R/V Wecoma - Missy Holzer Floating around in the "Big O" on the R/V Wecoma one finds peace, solitude as well the tranquil sounds of the waves crashing against the ship. With being swept away by all this wonderment, comes the longing for a few amenities only found on land, especially after being out at sea for an extended period of time. The acquisition of some amenities have to wait until the ship gets to port, but other amenities (albeit small) can be brought along on the cruise and act as a creature comfort until the ship gets back to port. More... |
Interview
with Dave Butterfield Jeff G: In monitoring the vent chemistry at Axial, are there any surprises so far this year? Dave: In the SE eruption zone things are cooling off. Cloud vent (where we put the NeMO Net RAS) has been steadily decreasing in temperature since we first measured it in 1998. Some of the other vents seem to be more stable. ASHES has been chugging along since we've been coming out here in the late 1980's and hasn't really changed very much. The structures there haven't grown very much and the chemistry hasn't changed a lot either. There haven't been any real surprises. However, we haven't gone back and done the detailed work in the lab yet to see what we've got. Overall, we've seen the disappearance of widespread venting that occurred right after the eruption and it seems to be focusing down to a few areas. It turns out that those areas are the same ones that have historically been diffuse vent areas before the eruption. There's something about those locations that focuses the flow. More... |
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