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Malfait, Bruce Terry (1974): Annotated record of the detailed examination of a Mn deposits from the Carnegie Ridge in the Pacific Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.876539, Supplement to: Malfait, BT (1975): The Carnegie Ridge near 86⁰ W. : structure, sedimentation and near bottom observations. Ph. D. Dissertation), Oregon State University, USA, 142 pp, hdl:1957/28552

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Abstract:
The Carnegie Ridge is a linear, aseismic, submarine ridge lying between the Galapagos Islands and the coast of South America. Surface ship, near bottom, and grain size studies from the saddle have been used to delineate the present geological environment and history of the ridge. Structurally the Carnegie Ridge is rather simple in profile, being bounded by east-west trending scarps which give the ridge a block-faulted appearance. Acoustic basement over the ridge appears smooth on reflection profiles and is composed of chert. The sedimentary sequence above the chert horizon contains a lower chalk unit overlain by calcareous ooze. Where erosion has exposed the chalk a karst-like micro-topography is present which is characterized by steep walled channels and cliffs and consolidated bed forms undergoing erosion and dissolution. The ridge crest has been stripped of almost its entire sediment cover. Thick sequences of sediment are found only in areas protected from north or south flowing bottom currents. Evidence of erosion is provided by extensive channeling on both the north and south flanks of the ridge. Near bottom observations in one channel on the north flank revealed a large field of sand dunes indicating northward, downslope sediment transport. These dunes are found on manganese-encrusted chalk which floors the channel.
Source:
Grant, John Bruce; Moore, Carla J; Alameddin, George; Chen, Kuiying; Barton, Mark (1992): The NOAA and MMS Marine Minerals Geochemical Database. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V52Z13FT
Further details:
Warnken, Robin R; Virden, William T; Moore, Carla J (1992): The NOAA and MMS Marine Minerals Bibliography. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V53X84KN
Coverage:
Median Latitude: -1.197238 * Median Longitude: -85.511857 * South-bound Latitude: -1.400000 * West-bound Longitude: -85.703333 * North-bound Latitude: -0.727000 * East-bound Longitude: -85.298000
Date/Time Start: 1971-10-01T00:00:00 * Date/Time End: 1971-10-11T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 6.700 m
Event(s):
Y71-03-20 (MG1)  * Latitude: -1.335000 * Longitude: -85.323000 * Date/Time: 1971-10-08T00:00:00 * Elevation: -2310.0 m * Campaign: Y71-03 * Basis: Yaquina * Method/Device: Piston corer (PC)
Y71-03-21C  * Latitude: -1.316667 * Longitude: -85.613333 * Date/Time: 1971-10-01T00:00:00 * Elevation: -2417.0 m * Location: Carnegie Ridge, Pacific Ocean * Campaign: Y71-03 * Basis: Yaquina * Method/Device: Photo/Video (PV)
Y71-03-26PC  * Latitude: -0.877000 * Longitude: -85.298000 * Date/Time: 1971-10-10T00:00:00 * Elevation: -2521.0 m * Recovery: 2.57 m * Location: Carnegie Ridge, Pacific Ocean * Campaign: Y71-03 * Basis: Yaquina * Method/Device: Piston corer (PC)
Comment:
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
IdentificationID
DEPTH, sediment/rockDepth sedmGeocode
Depth, top/minDepth topm
Depth, bottom/maxDepth botm
PositionPositionVisual description
Deposit typeDeposit type
Quantity of depositQuantity
SizeSize
10 Substrate typeSubstrate
11 CommentComment
12 DescriptionDescription
13 File nameFile name
14 Uniform resource locator/link to imageURL image
Size:
112 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

ID

Depth sed [m]

Depth top [m]

Depth bot [m]

Position

Deposit type

Quantity

Size
10 
Substrate
11 
Comment
12 
Description
13 
File name
14 
URL image
Y71-03-20 Y71-03-20-10.3000.000.60BuriedMn nodule1Yellowish gray sand and clayIndurated Fe-Mn nodule
Y71-03-20Y71-03-20-26.7006.407.00BuriedMn nodule1Yellowish gray clay with black masses of metallic grainsIndurated Fe-Mn nodule
Y71-03-20Y71-03-20-31.1951.191.20BuriedMn crust1Consolidated sedimentMottled yellow silty clayMn accretion mass
Y71-03-20Y71-03-20-41.8501.851.85BuriedMn crust1Consolidated sedimentMottled white nannofossil chalk oozeMn accretion mass
Y71-03-20Y71-03-20-53.8653.694.04BuriedMn crustSeveralConsolidated sedimentMottled pale yellow slightly silty clayMn accretions
Y71-03-20Y71-03-20-64.2804.244.32BuriedMn crustSeveralConsolidated sedimentDark brown and black partially indurated siltMn accretions
Y71-03-26PC Y71-03-26PC-10.0000.000.00SurfaceMn noduleSmallLight yellowish brown claySmall manganese nodule lodged in the nose of the gravity core
Y71-03-32 Y71-03-32-10.0000.000.00SurfaceMn noduleSeveralLight yellowish brown sand with numerous forams,Basalt pebbles and manganese nodules
Y71-03-21C Y71-03-21C-10.0000.000.00SurfaceMn coatingSeveralRock; chalkForaminifera sandFractured plates of lithified sediments with nodular surface covered what appears to be manganeseFig21A_Malfait_1975.jpgFig21A_Malfait_1975.jpg
Y71-03-30C Y71-03-30C-10.0000.000.00SurfaceMn coatingSeveralRock; chalkForaminifera sandRubble pavement of lithified chalk covered with manganeseFig30B_Malfait_1975.jpgFig30B_Malfait_1975.jpg
Y71-03-32C Y71-03-32C-10.0000.000.00SurfaceMn coatingSeveralThinRock; chalkClayey sandStereoscopic pair showing outcrop of chalk apparently coated by thin layer of manganeseFig32_Malfait_1975.jpgFig32_Malfait_1975.jpg
Y71-03-34C Y71-03-34C-10.0000.000.00SurfaceMn noduleManyForaminifera sandPavement of manganese nodules between elongated masses of lithified sedimentFig34_Malfait_1975.jpgFig34_Malfait_1975.jpg