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Index to Marine and Lacustrine Geological Samples (IMLGS)

Repository: Lamont-Doherty Earth Observatory
Contact the Curator
Ship: Robert D. Conrad
Cruise: RC14 (RC1407)
Sample: 171
Device: core, piston
Latitude: 51.373
Longitude: -140.057
Water Depth(m): 3738
Date: 19710915
IGSN: DSR000M88
Core length (cm): 790
Diameter (cm): 6
Storage: room temperature, moisture sealed
1 :    0 to 18 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Geologic Age: unknown
2 :    18 to 268 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Geologic Age: unknown
3 :    268 to 274 cm in core
Primary composition: calcareous, foraminifera
Primary texture: mud or ooze
Geologic Age: unknown
4 :    274 to 505 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Geologic Age: unknown
5 :    505 to 507 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Secondary composition: calcareous, foraminifera
Secondary texture: mud or ooze
Geologic Age: unknown
6 :    507 to 622 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Secondary composition: calcareous, foraminifera
Secondary texture: mud or ooze
Geologic Age: unknown
7 :    622 to 623 cm in core
Primary composition: calcareous, foraminifera
Primary texture: mud or ooze
Geologic Age: unknown
8 :    623 to 640 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Geologic Age: unknown
9 :    640 to 649 cm in core
Primary composition: calcareous, foraminifera
Primary texture: mud or ooze
Geologic Age: unknown
10 :    649 to 766 cm in core
Primary composition: terrigenous
Primary texture: mud or ooze
Geologic Age: unknown
11 :    766 to 790 cm in core
Primary composition: terrigenous
Primary texture: sand
Secondary composition: volcanics
Secondary texture: glass shards
Geologic Age: unknown
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When you refer to individual samples/data in the IMLGS, please cite each source repository whose data you use.

More Information and how to cite the IMLGS: doi:10.7289/V5H41PB8.


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