Hillenbrand, Claus-Dieter; Kuhn, Gerhard; Smith, James A; Gohl, Karsten; Graham, Alastair G C; Larter, Robert D; Klages, Johann Philipp; Downey, Rachel; Moreton, Steven Grahame; Forwick, Matthias; Vaughan, David G (2013): Shear strength of sediment core PS75/129-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.773955, In supplement to: Hillenbrand, C-D et al. (2013): Grounding-line retreat of the West Antarctic Ice Sheet from inner Pine Island Bay. Geology, 41(1), 35-38, https://doi.org/10.1130/G33469.1
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Project(s):
Coverage:
Latitude: -74.509000 * Longitude: -134.120830
Date/Time Start: 2010-02-18T22:40:00 * Date/Time End: 2010-02-18T22:40:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 2.55 m
Event(s):
PS75/129-1 * Latitude: -74.509000 * Longitude: -134.120830 * Date/Time: 2010-02-18T22:40:00 * Elevation: -923.0 m * Penetration: 3.5 m * Recovery: 2.58 m * Location: westernmost Getz Trough, inner shelf (meltwater channel) * Campaign: ANT-XXVI/3 (PS75) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 3 core sections: 0-0.58, .58-1.58, 1.58-2.58, 2.58 m
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Shear strength, primary | Shear str | kPa | Hillenbrand, Claus-Dieter | Shear vane, hand-held |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
52 data points
Data
1 Depth sed [m] | 2 Shear str [kPa] |
---|---|
0.01 | 0 |
0.05 | 0 |
0.10 | 1 |
0.15 | 3 |
0.20 | 5 |
0.26 | 7 |
0.31 | 3 |
0.36 | 3 |
0.40 | 3 |
0.45 | 6 |
0.50 | 5 |
0.55 | 2 |
0.60 | 4 |
0.65 | 6 |
0.70 | 7 |
0.75 | 7 |
0.80 | 7 |
0.85 | 7 |
0.90 | 2 |
0.95 | 3 |
1.00 | 4 |
1.05 | 6 |
1.10 | 8 |
1.15 | 9 |
1.20 | 7 |
1.25 | 5 |
1.30 | 4 |
1.35 | 4 |
1.40 | 2 |
1.45 | 4 |
1.50 | 6 |
1.55 | 4 |
1.60 | 10 |
1.65 | 7 |
1.70 | 6 |
1.75 | 7 |
1.80 | 9 |
1.85 | 13 |
1.90 | 11 |
1.95 | 6 |
2.00 | 5 |
2.05 | 6 |
2.10 | 5 |
2.15 | 5 |
2.20 | 4 |
2.25 | 6 |
2.30 | 6 |
2.35 | 5 |
2.40 | 5 |
2.45 | 5 |
2.50 | 5 |
2.55 | 5 |