Guardado en:
| Autores principales: | , |
|---|---|
| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
2011
|
| Materias: | |
| Acceso en línea: | https://doi.org/10.1594/PANGAEA.756362 |
| Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
| _version_ | 1867169979566129152 |
|---|---|
| author | King, Lorenz Seppälä, Matti |
| author_facet | King, Lorenz Seppälä, Matti |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_756362 |
| institution | PANGAEA |
| language | en |
| publishDate | 2011 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Tab. 2,3,4 Specific resistivity of calculated models for the soundings in Lapland King, Lorenz Seppälä, Matti 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; GeoEl-16; GeoEl-17; GeoEl-18; GeoEl-19; GeoEl-20; GeoEl-21; GeoEl-22; GeoEl-23; GeoEl-24; GeoEl-25; GeoEl-26; GeoEl-27; GeoEl-28; GeoEl-29; Geoelectric; Hietatievat, Finnland; Kaunispää, Finnland; Layer description; Peldojoki, Finnland; Perra, Finnland; Pikku-Malla, Finnland; Resistivity, electrical; Saana, Finnland; Skallovarri, Finnland 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. |
| title | Tab. 2,3,4 Specific resistivity of calculated models for the soundings in Lapland |
| topic | 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; GeoEl-16; GeoEl-17; GeoEl-18; GeoEl-19; GeoEl-20; GeoEl-21; GeoEl-22; GeoEl-23; GeoEl-24; GeoEl-25; GeoEl-26; GeoEl-27; GeoEl-28; GeoEl-29; Geoelectric; Hietatievat, Finnland; Kaunispää, Finnland; Layer description; Peldojoki, Finnland; Perra, Finnland; Pikku-Malla, Finnland; Resistivity, electrical; Saana, Finnland; Skallovarri, Finnland |
| url | https://doi.org/10.1594/PANGAEA.756362 |