- Alvin 3358 - Dive Summary
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- 19 February 1998
- Observers: Cindy Van Dover, Karl Grönvold (transcript)
- Pilot: Blee Williams
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- Dive Summary
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- The dive began about 200 m west of the Oasis low-T Vent Site
in heavily sedimented sheet flow - sample 1. Heading 110 this
gave way to a very uneven (AA-like) broken up sheet flow, most
likely with similar heavy sediment cover. There was then a relatively
clear contact between this and a younger lobate flow with much
lighter sediment cover - sample 2. This is a lobate flow with
occasional pillows and extends to Oasis.
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- We arrived at the southwest margin of OASIS which begins
as a bed of orange anemones (several cm diameter and height),
giving way to orange anemones and barnacle (Neolepas zevinae)
bushes with an understory of small (~1 cm height, diameter) grey
anemones, and then to patches of mussels or clams within the
anemone/barnacle bed. We sampled a total of 6 mussel patches
within OASIS, working S to N along the margin of a drop-off.
At the first 3 OASIS Sites, we took both pot and scoop samples;
scoop samples only at OASIS Sites 4-6. Temperatures among mussels
ranged from 4-6C. The entire N-S extent of OASIS is ~100 m and
the eastern boundary is at the drop-off (collapse?); there is
a gap in mussel patches within the middle of the field. Anemones
do occupy the lobate field E of the drop-off, and there are patches
of long-dead mussel and clam shells, as well as an inactive sulfide
chimney (13 m) covered with serpulid tubes. Debris (anchors,
cables, markers) from an old Japanese/Shinkai experiment was
observed throughout the OASIS field.The lobate lava with occasional
pillows and pillow groups continued north of Oasis and all the
way to Stanley. During the passage however a change was observed
which was mainly manifested in more glassy loabates. With no
clear difference in lava morphology - no firm contact was registered
but we may both have traversed possible contact again and even
travelled along it.We reached Stanley (Mkr #21; named during
the Lilley/von Damm cruise) toward the end of the dive and explored
the area, looking for mussel beds with no success. The local
area supports some anemones and at one time supported a few mussels,
clams, and serpulid worms. The site hosts an active sulfide chimney.
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- Sample Locations:
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- Navigation Plot (GMT)
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