Tab. 2,3,4 Specific resistivity of calculated models for the soundings in Lapland

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 th...

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Bibliographic Details
Main Authors: King, Lorenz, Seppälä, Matti
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
1
10
11
12
13
14
15
16
17
18
19
2
20a+b
21
22
23
24
25
26
27
28
29
3
4
5
6
7
8
9
Ailigas
Finnland
Depth
reconstructed
Event label
GEOEL
GeoEl-01
GeoEl-02
GeoEl-03
GeoEl-04
GeoEl-05
GeoEl-06
GeoEl-07
GeoEl-08
GeoEl-09
GeoEl-10
GeoEl-11
GeoEl-12
GeoEl-13
GeoEl-14
GeoEl-15
Fjell
Northern Finland
permafrost
Polarforschung
Lapland
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.756362
https://doi.org/10.1594/PANGAEA.756362
Description
Summary: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.

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