Geomorfología de los volcanes basálticos monogénicos de la Isla de Tenerife, Canarias
- González Cárdenas, Elena (coord.)
- Escobar Lahoz, Estela (coord.)
- Becerra Ramírez, Rafael (coord.)
- Gosálvez Rey, Rafael Ubaldo (coord.)
- Dóniz Páez, Javier (coord.)
- Martínez de Pisón Stampa, Eduardo (pr.)
Publisher: Centro de Estudios Calatravos
ISBN: 978-84-614-1025-5
Year of publication: 2010
Pages: 181-203
Type: Book chapter
Abstract
Cinder cones are the most common phenomenon caused by subaerial volcanic, (Wood, 1980 a) Even then, the interest they have aroused in the scientific community is vastly lower than that derived from other structures and eruptive processes. Undoubtedly this is related to its lowest mark in the landscape and the low risk posed by a rash of these characteristics (Dóniz, 2004 a).