Ó Cofaigh, Colm; Dowdeswell, Julian A; Grobe, Hannes (1996): Ice rafted debris (> 2 mm gravel) distribution in sediment core PS1939-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.50387, In supplement to: Ó Cofaigh, C et al. (2001): Holocene glacimarine sedimentation, inner Scoresby Sund, East Greenland: the influence of fast-flowing ice-sheet outlet glaciers. Marine Geology, 175(1-4), 103-129, https://doi.org/10.1016/S0025-3227(01)00117-7
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Project(s):
Coverage:
Latitude: 71.538300 * Longitude: -26.996700
Date/Time Start: 1990-09-21T00:00:00 * Date/Time End: 1990-09-21T00:00:00
Minimum DEPTH, sediment/rock: 0.01000 m * Maximum DEPTH, sediment/rock: 0.76000 m
Event(s):
PS1939-2 (PS17/274) * Latitude: 71.538300 * Longitude: -26.996700 * Date/Time: 1990-09-21T00:00:00 * Elevation: -1245.0 m * Penetration: 6.5 m * Recovery: 0.76 m * Location: Scoresby Sund * Campaign: ARK-VII/3b (PS17) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 1 section: 0-76; bei 6,5m bananisiert
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Ice rafted debris, number of gravel | IRD | #/10 cm3 | Grobe, Hannes | IRD-Counting (Grobe, 1987) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
76 data points
Data
1 Depth sed [m] | 2 IRD [#/10 cm3] |
---|---|
0.01000 | 1 |
0.02000 | 2 |
0.03000 | 1 |
0.04000 | 1 |
0.05000 | 3 |
0.06000 | 2 |
0.07000 | 2 |
0.08000 | 4 |
0.09000 | 4 |
0.10000 | 3 |
0.11000 | 1 |
0.12000 | 2 |
0.13000 | 6 |
0.14000 | 4 |
0.15000 | 5 |
0.16000 | 2 |
0.17000 | 6 |
0.18000 | 4 |
0.19000 | 2 |
0.20000 | 3 |
0.21000 | 4 |
0.22000 | 4 |
0.23000 | 5 |
0.24000 | 4 |
0.25000 | 8 |
0.26000 | 4 |
0.27000 | 3 |
0.28000 | 5 |
0.29000 | 4 |
0.30000 | 4 |
0.31000 | 2 |
0.32000 | 6 |
0.33000 | 4 |
0.34000 | 3 |
0.35000 | 2 |
0.36000 | 3 |
0.37000 | 4 |
0.38000 | 0 |
0.39000 | 4 |
0.40000 | 7 |
0.41000 | 4 |
0.42000 | 3 |
0.43000 | 3 |
0.44000 | 3 |
0.45000 | 5 |
0.46000 | 6 |
0.47000 | 4 |
0.48000 | 6 |
0.49000 | 3 |
0.50000 | 3 |
0.51000 | 6 |
0.52000 | 8 |
0.53000 | 6 |
0.54000 | 12 |
0.55000 | 4 |
0.56000 | 4 |
0.57000 | 7 |
0.58000 | 6 |
0.59000 | 4 |
0.60000 | 3 |
0.61000 | 2 |
0.62000 | 2 |
0.63000 | 0 |
0.64000 | 1 |
0.65000 | 1 |
0.66000 | 3 |
0.67000 | 4 |
0.68000 | 6 |
0.69000 | 2 |
0.70000 | 3 |
0.71000 | 3 |
0.72000 | 4 |
0.73000 | 6 |
0.74000 | 4 |
0.75000 | 4 |
0.76000 | 5 |