Abstract - The volcanic events of West Cameroon are controlled by tectonic lines. Even the historical eruptions of Mount Cameroon (the 1982 eruption is described) show persistant structural influences.Résumé - Le volcanisme de l'Ouest Cameroun est très influencé par un substratum marqué par des directions tectoniques. Ce caractère persiste, malgré certaines apparences, dans les éruptions récentes (celles du dix-neuvième siècle, et celle de 1982 qui est décrite).Morin Serge, Mottet Gérard, Zogning Appolinaire. Deux études sur le volcanisme du Mont Cameroun. (Two studies about Mount Cameroun). In: Bulletin de l'Association de géographes français, 62e année, 1985-2 ( juillet). pp. 135-144
Mt Cameroon is a steep lava-dominated volcano located on the coast of the Gulf of Guinea. This 1400 ...
Rumpi Hills designate a mosaic of hills and valleys (1500 km2) at 80 km north of Mount CaMeroon. The...
This study describes the seismo-tectonic evolution of Cameroon. It is noticed that seismic activity ...
The Mt Cameroon volcano is the highest and most active volcano of the Cameroon Volcanic Line. Little...
Au cours des trente dernières années, les risques et les catastrophes naturels ont été identifiés et...
Abstract. - Many lakes can be studied in volcanic areas : dams lakes, under-ice lakes, maars, crater...
The volcanic activity of Mts Bambouto and Oku (Western Highlands) and of the Ngaoundere Plateau, in ...
The Cameroun Volcanic Line (CVL) is a magmatic alignment, extending on both oceanic and continental ...
Abstract : Limbe, a footslope town on an active volcano in a humid tropical environment. Located in ...
Mount Cameroon is an active volcano located in the Gulf of Guinea, west of Central Africa. After the...
The current evolution of natural milieux in central and west Cameroon Central and west Cameroon has ...
International audienceThe volcanic story of Mount Manengouba is related to four chronological stages...
International audienceTombel graben and Mounts Bambouto are two volcanic fields of the typical syste...
La chaine de Ngovayang fait partie des formations tectoniques majeures de l’unité du Nyong au sud du...
Mt Cameroon is a steep lava-dominated volcano located on the coast of the Gulf of Guinea. This 1400 ...
Rumpi Hills designate a mosaic of hills and valleys (1500 km2) at 80 km north of Mount CaMeroon. The...
This study describes the seismo-tectonic evolution of Cameroon. It is noticed that seismic activity ...
The Mt Cameroon volcano is the highest and most active volcano of the Cameroon Volcanic Line. Little...
Au cours des trente dernières années, les risques et les catastrophes naturels ont été identifiés et...
Abstract. - Many lakes can be studied in volcanic areas : dams lakes, under-ice lakes, maars, crater...
The volcanic activity of Mts Bambouto and Oku (Western Highlands) and of the Ngaoundere Plateau, in ...
The Cameroun Volcanic Line (CVL) is a magmatic alignment, extending on both oceanic and continental ...
Abstract : Limbe, a footslope town on an active volcano in a humid tropical environment. Located in ...
Mount Cameroon is an active volcano located in the Gulf of Guinea, west of Central Africa. After the...
The current evolution of natural milieux in central and west Cameroon Central and west Cameroon has ...
International audienceThe volcanic story of Mount Manengouba is related to four chronological stages...
International audienceTombel graben and Mounts Bambouto are two volcanic fields of the typical syste...
La chaine de Ngovayang fait partie des formations tectoniques majeures de l’unité du Nyong au sud du...
Mt Cameroon is a steep lava-dominated volcano located on the coast of the Gulf of Guinea. This 1400 ...
Rumpi Hills designate a mosaic of hills and valleys (1500 km2) at 80 km north of Mount CaMeroon. The...
This study describes the seismo-tectonic evolution of Cameroon. It is noticed that seismic activity ...