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Cruise Report (PDF, 4.8Mb) - NOAA, Ocean Explorer

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J416 Sample Log<br />

sample<br />

name type Location date hr min vv lat vv long<br />

J416-sed-01 geo near landing<br />

J416-sed-02 geo near landing<br />

J416-rock-03 geo<br />

traveling up<br />

N slope<br />

47<br />

vv<br />

rec<br />

5/9<br />

2009 04 37 -15.389232 -174.253560 3113 129 2 1815<br />

5/9<br />

2009 04 42 -15.389234 -174.253574 3121 129 2 1815<br />

5/9<br />

2009 05 19 -15.390445 -174.252966 3203 125 3 1743<br />

hd<br />

g alt jasZ J416 Sample Comments (NELSC and Maka) PI<br />

~12 cm long pushcore. The entire core is dominantly<br />

glass, but planktic foraminifers and rare diatoms are<br />

present in each subsection as well. The character of<br />

the coarse glass changes through the core with only<br />

rare limu o Pele in the basal portions, increasing upsection.<br />

Pele’s hairs are very rare in the entire core,<br />

although more abundant in the fine fractions. The<br />

pyroclasts near the bottom are mostly scoria to finely<br />

vesicular fragments that approach pumice. There are<br />

no obvious flow fragments or other lithic fragments in<br />

the core, although some scoria fragments are altered<br />

to a white amorphous silica(?). Additional fragments,<br />

particularly near the bottom, are coated with brown<br />

hydrothermal precipitates, but most glass is fresh<br />

throughout the core. The glasses are all light brown<br />

in color. Each subsection has about twice as much<br />

material in the >500 micron fraction as in the 63-500<br />

micron fraction. Zero age? yes/no<br />

Small scoop sample that consists almost entirely of<br />

glass fragments of pyroclastic origin. The largest<br />

fragments are cm-sized, but about half the sample is<br />

0.063-0.5 mm in size. A significant amount passed<br />

through the 63 micron sieve. Limu o Pele fragments<br />

are fairly rare and Pele’s hairs absent. Some of the<br />

fragments are stained reddish brown, but most are<br />

fresh. Plnktic foraminifers are common, comprising a<br />

percent or so of the bulk sample. The finer fraction<br />

contains abundant lava ribbons. Zero age? yes/no<br />

Piece of a plate?. Small fragment of older material<br />

with iron oxide staining on other surfaces. 1 cm thick<br />

glass rind. Looks fairly vesicular. Sampled while<br />

climbing up the north side of the ridge toward the<br />

ridge crest. Not suspected to be zero age.<br />

geo<br />

group<br />

geo<br />

group<br />

geo<br />

group

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