rdfs:comment
| - La ceinture volcanique de Garibaldi (en anglais : Garibaldi Volcanic Belt) ou chaîne volcanique de Garibaldi est une ceinture volcanique de Colombie-Britannique, au Canada. Constituée par un ensemble de volcans, elle se situe dans le nord des chaînes côtières du Pacifique, dans l'arc volcanique des Cascades.
* Portail du volcanisme
* Portail de la Colombie-Britannique (fr)
- The Garibaldi Volcanic Belt is a northwest–southeast trending volcanic chain in the Pacific Ranges of the Coast Mountains that extends from Watts Point in the south to the Ha-Iltzuk Icefield in the north. This chain of volcanoes is located in southwestern British Columbia, Canada. It forms the northernmost segment of the Cascade Volcanic Arc, which includes Mount St. Helens and Mount Baker. Most volcanoes of the Garibaldi chain are dormant stratovolcanoes and subglacial volcanoes that have been eroded by glacial ice. Less common volcanic landforms include cinder cones, volcanic plugs, lava domes and calderas. These diverse formations were created by different styles of volcanic activity, including Peléan and Plinian eruptions. (en)
- La cintura vulcanica Garibaldi è una cintura vulcanica che si estende in direzione nordovest-sudest nelle Pacific Ranges delle Montagne Costiere, da Watts Point a sud fino al a nord. La catena vulcanica si trova nella parte sudoccidentale della Columbia Britannica, in Canada. Forma il segmento più settentrionale dell'arco vulcanico delle Cascate, che include il Monte Sant'Elena e il Monte Baker. (it)
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