Saarse, Leili (2010): Lithology of sediment core KALSA, Kalsa Mire, Estonia [dataset]. European Pollen Database (EPD), PANGAEA, https://doi.org/10.1594/PANGAEA.741411
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Related to:
Kimmel, Kai; Pirrus, Reet; Raukas, Anto (1999): Holocene deposits. In: A Miidel and A Raukas (Editors) Lake Peipsi. Geology, Sulemees Publishers, Tallinn, 42-52
Coverage:
Latitude: 58.166667 * Longitude: 27.450000
Minimum DEPTH, sediment/rock: 0.6500 m * Maximum DEPTH, sediment/rock: 2.9250 m
Event(s):
KALSA * Latitude: 58.166667 * Longitude: 27.450000 * Elevation Start: 38.0 m * Elevation End: 0.0 m * Location: Kalsa Mire, Estonia * Method/Device: Russian corer (RUSC) * Comment: Local vegetation: Sphagnum. Core diameter: 10 cm. Area: 170 ha. Mire, peat cutting at the edges. Physiography: undulating moraine topography. Surrounding vegetation: Pinus, Betula, Picea forest. in SW 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 | Saarse, Leili | of the lithological unit | |
3 | Depth, bottom/max | Depth bot | m | Saarse, Leili | of the lithological unit | |
4 | Lithology/composition/facies | Lithology | Saarse, Leili | |||
5 | Boundary layer, lower | Bound low | Saarse, Leili |
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 | 5 Bound low |
---|---|---|---|---|
0.6500 | 0.0000 | 1.3000 | Eriophorum-Sphagnum peat | Diffuse |
1.5250 | 1.3000 | 1.7500 | Eriophorum-Sphagnum-woody peat | Diffuse |
1.8000 | 1.7500 | 1.8500 | Eriophorum-Sphagnum peat | Diffuse |
1.9250 | 1.8500 | 2.0000 | Eriophorum-Sphagnum-woody peat | Diffuse |
2.3500 | 2.0000 | 2.7000 | Eriophorum-woody peat, 264-268:charcoal | Diffuse |
2.7750 | 2.7000 | 2.8500 | woody peat | Sharp |
2.9250 | 2.8500 | 3.0000 | silt |