Dittmers, Klaus Hauke; Niessen, Frank; Stein, Ruediger (2005): Geometry and morphology of the paleo-Ob River channels (Typ II) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.338934, In supplement to: Dittmers, KH et al. (2008): Late Weichselian Fluvial Evolution on the Southern Kara Sea Shelf, North Siberia. Global and Planetary Change, 60(3-4), 327-350, https://doi.org/10.1016/j.gloplacha.2006.12.006
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Dittmers, Klaus Hauke (2006): Late Weichselian to Holocene sedimentation in the inner Kara Sea: Qualification and Quantification of Processes. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 523, 185 pp, https://doi.org/10.2312/BzPM_0523_2006
Project(s):
Siberian River Run-Off (SIRRO)
Coverage:
Median Latitude: 75.344167 * Median Longitude: 74.327917 * South-bound Latitude: 73.240000 * West-bound Longitude: 66.420000 * North-bound Latitude: 76.930000 * East-bound Longitude: 76.920000
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | LATITUDE | Latitude | Geocode | |||
| 2 | LONGITUDE | Longitude | Geocode | |||
| 3 | Depth, bathymetric | Bathy depth | m | Stein, Ruediger | ParaSound (Atlas Hydrographic) | |
| 4 | Depression | Depres | m | Stein, Ruediger | ParaSound (Atlas Hydrographic) | |
| 5 | Sediment thickness | Sed thick | m | Stein, Ruediger | ParaSound (Atlas Hydrographic) | |
| 6 | Bankful width | Bankf width | m | Stein, Ruediger | ParaSound (Atlas Hydrographic) | |
| 7 | Bankful depth | Bankf depth | m | Stein, Ruediger | ParaSound (Atlas Hydrographic) | |
| 8 | Bankful width/depth ratio | Bankf w/d | Stein, Ruediger | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
144 data points
Data
| 1 Latitude | 2 Longitude | 3 Bathy depth [m] | 4 Depres [m] | 5 Sed thick [m] | 6 Bankf width [m] | 7 Bankf depth [m] | 8 Bankf w/d |
|---|---|---|---|---|---|---|---|
| 73.24 | 66.42 | 50 | 3.7 | 8.3 | 1240 | 12 | 100 |
| 74.00 | 73.11 | 29 | 10.0 | 10.0 | 600 | 20 | 30 |
| 74.00 | 73.27 | 28 | 10.0 | 10.0 | 1500 | 20 | 80 |
| 74.76 | 74.85 | 25 | 5.0 | 10.0 | 3960 | 15 | 260 |
| 74.90 | 75.85 | 36 | 7.0 | 6.0 | 2810 | 13 | 220 |
| 75.00 | 74.48 | 39 | 4.0 | 12.0 | 4080 | 16 | 260 |
| 75.17 | 75.70 | 34 | 6.0 | 6.0 | 3770 | 12 | 310 |
| 75.17 | 75.70 | 34 | 6.0 | 6.0 | 3770 | 12 | 310 |
| 75.28 | 73.77 | 40 | 8.0 | 18.0 | 7200 | 26 | 280 |
| 75.46 | 73.12 | 42 | 12.0 | 12.0 | 4950 | 24 | 210 |
| 75.50 | 72.99 | 80 | 15.0 | 10.0 | 3120 | 25 | 120 |
| 75.53 | 74.07 | 42 | 8.0 | 6.0 | 300 | 14 | 20 |
| 75.53 | 74.10 | 42 | 17.0 | 6.0 | 600 | 23 | 30 |
| 75.54 | 74.16 | 40 | 10.0 | 5.0 | 900 | 15 | 60 |
| 75.54 | 74.21 | 39 | 10.0 | 5.0 | 600 | 15 | 40 |
| 75.54 | 74.26 | 42 | 17.0 | 5.0 | 600 | 22 | 30 |
| 75.67 | 73.64 | 53 | 43.0 | 8.0 | 5040 | 51 | 100 |
| 75.70 | 74.54 | 50 | 7.0 | 7.0 | 600 | 14 | 40 |
| 75.71 | 75.13 | 52 | 2.0 | 13.0 | 3370 | 15 | 220 |
| 75.72 | 75.95 | 50 | 5.0 | 8.0 | 250 | 13 | 20 |
| 75.72 | 76.07 | 48 | 7.0 | 7.0 | 300 | 14 | 20 |
| 76.30 | 76.92 | 60 | 15.0 | 8.0 | 950 | 23 | 40 |
| 76.35 | 76.79 | 80 | 4.0 | 15.0 | 600 | 19 | 30 |
| 76.93 | 74.77 | 40 | 45.0 | 10.0 | 13500 | 55 | 250 |