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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


B


 


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).