Smith, James A; Hillenbrand, Claus-Dieter; Kuhn, Gerhard; Larter, Robert D; Graham, Alastair G C; Ehrmann, Werner; Moreton, Steven Grahame; Forwick, Matthias (2010): Shear strength of sediment core JR141_VC427 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.754840, In supplement to: Smith, JA et al. (2011): Deglacial history of the West Antarctic Ice Sheet in the western Amundsen Sea Embayment. Quaternary Science Reviews, 30(5-6), 488-505, https://doi.org/10.1016/j.quascirev.2010.11.020
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Coverage:
Latitude: -73.668900 * Longitude: -114.978000
Date/Time Start: 2006-02-02T04:25:00 * Date/Time End: 2006-02-02T04:25:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 5.60 m
Event(s):
JR141_VC427 (VC427) * Latitude: -73.668900 * Longitude: -114.978000 * Date/Time: 2006-02-02T04:25:00 * Recovery: 4.95 m * Location: Amundsen Sea * Campaign: JR20060109 (JR141 JR150) * Basis: James Clark Ross * Method/Device: Vibro corer (VC)
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 | Smith, James A | Shear vane, hand-held |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
59 data points
Data
| 1 Depth sed [m] | 2 Shear str [kPa] |
|---|---|
| 0.02 | 0 |
| 0.05 | 1 |
| 0.10 | 0 |
| 0.20 | 0 |
| 0.30 | 2 |
| 0.40 | 1 |
| 0.50 | 2 |
| 0.60 | 1 |
| 0.70 | 1 |
| 0.80 | 1 |
| 0.90 | 2 |
| 1.00 | 4 |
| 1.10 | 4 |
| 1.20 | 4 |
| 1.30 | 4 |
| 1.40 | 4 |
| 1.50 | 3 |
| 1.60 | 3 |
| 1.70 | 1 |
| 1.80 | 1 |
| 1.92 | 1 |
| 2.00 | 1 |
| 2.10 | 1 |
| 2.20 | 1 |
| 2.30 | 0 |
| 2.40 | 2 |
| 2.50 | 2 |
| 2.60 | 2 |
| 2.70 | 1 |
| 2.80 | 1 |
| 2.90 | 1 |
| 3.00 | 0 |
| 3.10 | 2 |
| 3.20 | 2 |
| 3.30 | 3 |
| 3.40 | 2 |
| 3.50 | 2 |
| 3.60 | 3 |
| 3.69 | 0 |
| 3.80 | 2 |
| 3.90 | 2 |
| 4.00 | 1 |
| 4.10 | 2 |
| 4.20 | 3 |
| 4.30 | 2 |
| 4.40 | 3 |
| 4.50 | 2 |
| 4.60 | 2 |
| 4.70 | 2 |
| 4.80 | 4 |
| 4.90 | 5 |
| 4.95 | 3 |
| 5.00 | 4 |
| 5.10 | 2 |
| 5.20 | 2 |
| 5.30 | 5 |
| 5.40 | 6 |
| 5.50 | 6 |
| 5.60 | 5 |