The submarine geology of Foveaux Strait / by David J. Cullen.

By: Cullen, D. J.
Contributor(s): New Zealand Oceanographic Institute | New Zealand. Department of Scientific and Industrial Research.
Material type: materialTypeLabelBookSeries: New Zealand Oceanographic Institute memoir: no. 33; DSIR bulletin: 184Publisher: Wellington, N.Z. : DSIR, 1967Description: 67, [1] pages : illustrations (1 folded chart) ; 30 cm.Subject(s): SUBMARINE GEOLOGY | SEDIMENTS | SEDIMENTATION | PETROLOGY | SUBMARINE CANYONS | OCEAN FLOOR | SEDIMENT SAMPLING | DEPOSITION | BOTTOM TOPOGRAPHY | FOVEAUX STRAIT | NEW ZEALANDOnline resources: NIWA document server In: DSIR bulletin In: New Zealand Oceanographic Institute memoirSummary: Foveaux Strait has a smooth featureless sea floor. The sediments in the strait confirm the former existence of a terrestrial environment, and in the submarine gravels palimpsest fluviatile dispersal patterns are distinguishable by petrographic and statistical analyses of the constituent pebbles.
Tags from this library: No tags from this library for this title. Log in to add tags.
Holdings
Item type Current library Collection Call number Copy number Status Date due Barcode
JOURNAL JOURNAL WELLINGTON OFF-SITE STACK NO. 184 1967 1 Available J011054
JOURNAL JOURNAL WELLINGTON OFF-SITE NWAC-02801 STACK NO. 33 1967 1 Available J021247

27 references; 16 figures; 3 tables.

Foveaux Strait has a smooth featureless sea floor. The sediments in the strait confirm the former existence of a terrestrial environment, and in the submarine gravels palimpsest fluviatile dispersal patterns are distinguishable by petrographic and statistical analyses of the constituent pebbles.

There are no comments on this title.

to post a comment.

Powered by Koha