King, Lorenz; Seppälä, Matti (2011): Tab. 2,3,4 Specific resistivity of calculated models for the soundings in Lapland [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.756362, Supplement to: King, L; Seppälä, M (1987): Permafrost thickness and distribution in Finnish Lapland - results of geoelectrical soundings. Polarforschung, 57(3), 127-147, hdl:10013/epic.29588.d001
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
Geoelectrical soundings were carried out in 29 different places in order to find permafrost and to measure its thickness. In most places above timber Iine a permafrost thickness of 10-50 m was recorded. Permafrost was found at sites with thin snow cover during winter. Here, deflation phenomena on the summits of fjells indicate the occurence of permafrost, Vegetation type might be a good indicator of permafrost, too. It seems obvious that permafrost exists extensively on fjell summits of northern Finland.
Coverage:
Median Latitude: 69.399879 * Median Longitude: 24.759769 * South-bound Latitude: 68.434400 * West-bound Longitude: 20.733900 * North-bound Latitude: 69.833300 * East-bound Longitude: 27.444400
Date/Time Start: 1985-07-27T00:00:00 * Date/Time End: 1985-08-11T00:00:00
Minimum Elevation: 205.0 m * Maximum Elevation: 890.0 m
Event(s):
GeoEl-01 (1) * Latitude: 68.434400 * Longitude: 27.444400 * Date/Time: 1985-07-27T00:00:00 * Elevation: 435.0 m * Location: Kaunispää, Finnland * Method/Device: Geoelectric (GEOEL) * Comment: Flat area with dry heath
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Layer description | Layer | King, Lorenz | curve type | ||
| 3 | Resistivity, electrical | Resist electr | Ohm m | King, Lorenz | rho 0 | |
| 4 | Resistivity, electrical | Resist electr | Ohm m | King, Lorenz | rho m | |
| 5 | Resistivity, electrical | Resist electr | Ohm m | King, Lorenz | rho 1 | |
| 6 | Resistivity, electrical | Resist electr | Ohm m | King, Lorenz | rho 2 | |
| 7 | Resistivity, electrical | Resist electr | Ohm m | King, Lorenz | rho 3 | |
| 8 | Depth, reconstructed | Reconstr depth | m | King, Lorenz | d0 | |
| 9 | Depth, reconstructed | Reconstr depth | m | King, Lorenz | d m | |
| 10 | Depth, reconstructed | Reconstr depth | m | King, Lorenz | d 1 | |
| 11 | Depth, reconstructed | Reconstr depth | m | King, Lorenz | d 2 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
195 data points
Data
| 1 Event | 2 Layer (curve type) | 3 Resist electr [Ohm m] (rho 0) | 4 Resist electr [Ohm m] (rho m) | 5 Resist electr [Ohm m] (rho 1) | 6 Resist electr [Ohm m] (rho 2) | 7 Resist electr [Ohm m] (rho 3) | 8 Reconstr depth [m] (d0) | 9 Reconstr depth [m] (d m) | 10 Reconstr depth [m] (d 1) | 11 Reconstr depth [m] (d 2) |
|---|---|---|---|---|---|---|---|---|---|---|
| GeoEl-02 | double-descending tpye, 3 layers | 20000 | 4000 | 7500 | 1000 | 2 | 3 | 45 | ||
| GeoEl-03 | double-descending tpye, 3 layers | 60000 | 4000 | 10000 | 1000 | 1 | 2 | 18 | ||
| GeoEl-04 | double-descending tpye, 3 layers | 60000 | 4000 | 10000 | 1200 | 1 | 1 | 11 | ||
| GeoEl-05 | double-descending tpye, 3 layers | 22000 | 1200 | 2800 | 1000 | 2 | 3 | 24 | ||
| GeoEl-06 | double-descending tpye, 3 layers | 36000 | 2500 | 6000 | 1000 | 1 | 2 | 18 | ||
| GeoEl-07 | double-descending tpye, 3 layers | 20000 | 1200 | 3000 | 1000 | 1 | 2 | 22 | ||
| GeoEl-08 | double-descending tpye, 4 layers | 60000 | 4000 | 10000 | 1200 | 1 | 1 | 13 | ||
| GeoEl-09 | double-descending tpye, 3 layers | 40000 | 2800 | 6500 | 1000 | 2 | 3 | 18 | ||
| GeoEl-10 | double-descending tpye, 3 layers | 36000 | 5000 | 12000 | 4000 | 2 | 5 | 14 | ||
| GeoEl-11 | double-descending tpye, 4 layers | 17000 | 2000 | 6000 | 3500 | 2 | 4 | 15 | ||
| GeoEl-12 | minimum type, 3 layers | 5500 | 1000 | 3000 | 2 | 6 | ||||
| GeoEl-13 | double-descending tpye, 3 layers | 50000 | 4000 | 10000 | 1000 | 1 | 1 | 7 | ||
| GeoEl-14 | descending, 2 layers | 20000 | 2000 | 1300 | 2 | 4 | ||||
| GeoEl-15 | double-descending tpye, 3 layers | 46000 | 16000 | 6000 | 1 | 14 | ||||
| GeoEl-16 | maximum type, 5 layers | 24000 | 100000 | 6000 | 1 | 5 | ||||
| GeoEl-17 | - | 5500 | ||||||||
| GeoEl-18 | maximum type, 3 layers | 100000 | >150000 | <2000 | 1 | >6 | ||||
| GeoEl-19 | double-descending tpye, 3 layers | 12000 | 6000 | 400 | >1 | 10 | ||||
| GeoEl-20 | maximum type, 3 layers | 900 | 30000 | 100 | 1 | 7 | ||||
| GeoEl-01 | minimum type, maximum type, 4 layers | 10000 | 10000 | 3000 | <6 | 70 | ||||
| GeoEl-21 | maximum type, 3 layers | <10000 | 60000 | 2500 | 1 | 2 | ||||
| GeoEl-22 | maximum type, 3 layers | <10000 | 60000 | 3000 | 1 | 1 | ||||
| GeoEl-23 | maximum type, 3 layers | 20000 | 65000 | 4000 | 2 | >50 | ||||
| GeoEl-24 | maximum type, 3 layers | 10000 | 22000 | 4000 | 11 | 50 | ||||
| GeoEl-25 | maximum type, 3 layers | 15000 | 33000 | 4000 | 11 | >60 | ||||
| GeoEl-26 | maximum type, 3 layers | 5000 | 8500 | 3500 | 2 | 8 | ||||
| GeoEl-27 | maximum type, 4 layers | 5000 | 10000 | 6000 | 1 | 2 | 13 | |||
| GeoEl-28 | maximum type, 3-4 layers | 12000 | 55000 | 4000 | 0 | 2 | 40 | |||
| GeoEl-29 | maximum type, 3-5 layers | 10000 | 50000 | 4000 | 1 | 5 | 50 |