El campo volcánico catalán
Catalan volcanic field, in Iberian Peninsula Northeast, has been made during Neogene and Quaternary. It is made up Empordà, la Selva and la Garrotxa Zones, the best volcanic morphology is in the last one because is the most recent. In this paper we explain the volcanic rocks general characteristics,...
| Autores: | , |
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| Tipo de documento: | artigo |
| Estado: | Versão publicada |
| Data de publicação: | 1999 |
| País: | España |
| Recursos: | Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya) |
| Repositório: | Recercat. Dipósit de la Recerca de Catalunya |
| OAI Identifier: | oai:recercat.cat:10256/4276 |
| Acesso em linha: | http://www.raco.cat/index.php/ECT/article/view/88637/0 http://hdl.handle.net/10256/4276 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Volcans -- Catalunya -- Garrotxa Roques volcàniques -- Catalunya -- Garrotxa Rocks, Igneous -- Catalonia -- Garrotxa Volcanoes -- Catalonia -- Garrotxa |
| Resumo: | Catalan volcanic field, in Iberian Peninsula Northeast, has been made during Neogene and Quaternary. It is made up Empordà, la Selva and la Garrotxa Zones, the best volcanic morphology is in the last one because is the most recent. In this paper we explain the volcanic rocks general characteristics, what eruption activity generate it and the final volcanic edifice morphology. Finally, we propose some crops to visit |
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