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| Leg2 | Cruise
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RUSCALA
Rock and sediment sampling on the Piip submarine volcano
Anatoliy Astakhov,
Boris Li, and Maxim Ivanov
V.Il’ichev Pacific Oceanological Institute,
Vladivostok,
Russia
The sampling of volcanic and subvolcanic rocks was carried
out using the “Okean” rectangular dredge. Sediment sampling was carried out by
use of a hydrostatic core HSS-2. Results of our geological sampling over and
adjacent to the Piips Volcano are depicted in Table 1.
Table 1. List of stations (Leg 1, RUSALCA-2004)
|
Date |
Stat. No |
Instru-
ment |
Latitude, N |
Longitude, E |
Water depth, m |
Short description
|
|
31.07.2004 |
A03 |
grab |
55°
25,5 |
167°
16,6 |
798 |
Pieces of dacite |
|
31.07.2004 |
A03 |
grab |
55°
25,5 |
167°
16,7 |
798 |
Fragment (50x40x30 cm) of
andesite |
|
31.07.2004 |
A04 |
grab |
55°
24,8 |
167°
16,5 |
390 |
Pieces of dacite |
|
31.07.2004 |
A05a |
dredge |
55°
24,6 |
167°
15,85 |
554 |
Pieces of dacite with
manganese crust |
|
|
|
|
55°
24,873* |
167° 16,094* |
380* |
|
|
31.07.2004 |
A05b |
grab |
55°
25,04 |
167°
16,2 |
395 |
Fragment
(40x40x30 cm) of black andesite |
|
|
|
|
55°
25,03* |
167°
16,5* |
|
|
|
31.07.2004 |
A05c |
dredge |
55°
24,8 |
167°
16,2 |
600 |
Fragment and pieces of
dacite |
|
|
|
|
55°
25,0* |
167°
16,5* |
400* |
|
|
31.07.2004 |
A07 |
dredge |
55°
22,44 |
167°
15,4 |
697 |
Pieces of pumice with manganese crust, carbonate-siliceous
concretion. |
|
|
|
|
55°
22,9* |
167°
16,2* |
550* |
|
|
01.08.2004 |
A08 |
core |
55°
20,652 |
167°
18,09 |
1890 |
Muds and diatom oozes, 2.45
m. |
|
01.08.2004 |
A09 |
dredge |
55°
22,8 |
167°
15,51 |
470 |
Pieces
of pumice, dropstones, manganese crust |
|
|
|
|
55°
21,1* |
167°
16,1* |
660* |
|
|
01.08.2004 |
A10 |
core |
55°
23,878 |
167°
13,382 |
1400 |
Pieces of pumice, dropstones,
sand |
|
01.08.2004 |
A11 |
dredge |
55°
22,64 |
167°
15,56 |
568 |
Fragments of pumice, dropstones,
sand |
|
|
|
|
55°
22,99* |
167°
16,14* |
500* |
|
|
01.08.2004 |
A12 |
core |
55°
23,984 |
167°
13,56 |
1251 |
Detritus of gray pumice |
|
01.08.2004 |
A13 |
core |
55°
27,43 |
167°
18,70 |
2096 |
Detritus of andesite |
*
coordinates and depth at the finish of the dredging operation.
The
samples of magmatic rocks collected during the RUSALCA expedition are similar
to previously collected samples from the submarine Piip volcano. The large
fragments of fresh andesites (Fig. 1A) and dacites were dredged on the North
Peak of the volcano. In some cases thin crusts of manganese oxides covered the
samples. A large quantity of samples
was dredged from the south peak of the Piip Volcano. They were primarily dacite
pumice (Fig.
1B). Most of these samples were covered by
manganese crust. In some cases
hydrothermally altered authigenic clays accumulated in pumice pores and were
spread along the surface. Two samples of carbonate-siliceous concretions and
sulfide-cemented crust were also dredged from the south peak of the Piip
Volcano (Fig. 1C).
|
A
|
|
C |
||||||
|
Figure
1. Sample of dredged rocks: A – fresh
andesite fragment, station A02; B – altered pumice with manganese crust,
station A07; C – sulfide cemented crust with ice rafted pebble, station A09. |
||||||||
Sediments were sampled by cores and a bottom grab
only at station A08 from a depth of 1,890 m. The samples were a mixture of
diatom ooze and sand (0-22 cm) and clayey silt interspersed with volcanic ash
layers (109-113 and 173-175
cm).