Moss, Andy (2010): Lithology of sediment core BK0702R, Bradford Kaims, United Kingdom [dataset]. European Pollen Database (EPD), PANGAEA, https://doi.org/10.1594/PANGAEA.741187
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Bartley, David D (1966): Pollen analysis of some lake deposits near Bamgurgh in Northumberland. New Phytologist, 65(2), 141-156, http://www.jstor.org/stable/2430353
Coverage:
Latitude: 55.588889 * Longitude: -1.761111
Date/Time Start: 1964-06-30T00:00:00 * Date/Time End: 1964-06-30T00:00:00
Minimum DEPTH, sediment/rock: 0.1000 m * Maximum DEPTH, sediment/rock: 5.7600 m
Event(s):
BK0702R (BKII) * Latitude: 55.588889 * Longitude: -1.761111 * Date/Time: 1964-06-30T00:00:00 * Elevation: 46.0 m * Location: Bradford Kaims, United Kingdom * Comment: No laminations. Local vegetation: Sphagnum peatbasin. Physiography: esker with unsorted and unwashed materia. Surrounding vegetation: field.
Comment:
This dataset was archived on 2010-05-11 from the EPD database.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Depth, top/min | Depth top | m | Moss, Andy | of the lithological unit | |
3 | Depth, bottom/max | Depth bot | m | Moss, Andy | of the lithological unit | |
4 | Lithology/composition/facies | Lithology | Moss, Andy |
License:
Creative Commons Attribution-NonCommercial 3.0 Unported (CC-BY-NC-3.0)
Size:
27 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Lithology |
---|---|---|---|
0.1000 | 0.0000 | 0.2000 | Worked soil and clay |
0.7050 | 0.2000 | 1.2100 | Peat |
1.3050 | 1.2100 | 1.4000 | Coarse detritus |
2.0750 | 1.4000 | 2.7500 | Nekron (gel) mud |
3.1700 | 2.7500 | 3.5900 | Coarse detritus |
3.8450 | 3.5900 | 4.1000 | Calcareous detritus |
4.1400 | 4.1000 | 4.1800 | Coarse detritus |
4.6900 | 4.1800 | 5.2000 | Lake clay |
5.7600 | 5.2000 | 6.3200 | Lake marl with much clay |