Observation of manganese nodules recovered by the USCGS Oceanographer in 1968 over the Blanco Fracture zone, Pacific Ocean

Fuente: PANGAEA
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Autore principale: Melson, William G
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1969
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_version_ 1867171851704205312
author Melson, William G
author_facet Melson, William G
collection Datos científicos de ciencias marinas y ambientales
contents Preliminary results of a 14-day cruise of the USC&GS ship Oceanographer to the area near the junction of Juan de Fuca Ridge and the Blanco Fracture Zone are reported. About 10 full days of bathymetry (using a narrow beam transducer), magnetic, and gravity were completed. Fifteen dredges were attempted, 13 were successful. A striking bathymetric symmetry up to 15 miles on each side of the axis was found on five crossings of the Juan de Fuca Ridge. This symmetry extends at least 17 and possibly 30 nautical miles along the Ridge axis. Relief features, ranging from 100 to 20 fathoms, were found to correlate with similar features across the axis. This bathymetric symmetry is more striking than the magnetic symmetry and is an independent line of evidence in support of sea-floor spreading. A small, median perched graben along portions of the Juan de Fuca Ridge axis is floored by a very recent basaltic flows which have unusual surface structures.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_882378
institution PANGAEA
language en
publishDate 1969
publisher PANGAEA
record_format pangaea
spellingShingle Observation of manganese nodules recovered by the USCGS Oceanographer in 1968 over the Blanco Fracture zone, Pacific Ocean
Melson, William G
Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; OC68; Oceanographer; OCNGR68; OCNGR68-D10; OCNGR68-D12; OCNGR68-D14; OCNGR68-D15; OCNGR68-D9; Pacific Ocean; Position; Quantity of deposit; Size; Substrate type; Visual description
Preliminary results of a 14-day cruise of the USC&GS ship Oceanographer to the area near the junction of Juan de Fuca Ridge and the Blanco Fracture Zone are reported. About 10 full days of bathymetry (using a narrow beam transducer), magnetic, and gravity were completed. Fifteen dredges were attempted, 13 were successful. A striking bathymetric symmetry up to 15 miles on each side of the axis was found on five crossings of the Juan de Fuca Ridge. This symmetry extends at least 17 and possibly 30 nautical miles along the Ridge axis. Relief features, ranging from 100 to 20 fathoms, were found to correlate with similar features across the axis. This bathymetric symmetry is more striking than the magnetic symmetry and is an independent line of evidence in support of sea-floor spreading. A small, median perched graben along portions of the Juan de Fuca Ridge axis is floored by a very recent basaltic flows which have unusual surface structures.
title Observation of manganese nodules recovered by the USCGS Oceanographer in 1968 over the Blanco Fracture zone, Pacific Ocean
topic Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; OC68; Oceanographer; OCNGR68; OCNGR68-D10; OCNGR68-D12; OCNGR68-D14; OCNGR68-D15; OCNGR68-D9; Pacific Ocean; Position; Quantity of deposit; Size; Substrate type; Visual description
url https://doi.org/10.1594/PANGAEA.882378