Mont Meager (massís)
|
Mont Meager
| |
|---|---|
 Lo massís de mont Meager.
| |
| Geografia | |
| Altitud | 2 680 m |
| Massís | Cadenons del Pacific |
| Arc volcanic | Arc volcanic de las Cascadas (arc de las Cascadas canadian e la cencha volcanica de Garibaldi) |
| Coordenadas geo. | 50° 38′ N, 123° 30′ O |
| Administracion | |
| País |  Canadà
|
| Província |  Colómbia Britanica
|
| Districte | Lillooet Land District |
| Ascension | |
| Primièra ascension | 1931 per l'òbra de Tom Fyles, de Neal Carter, d'Alec Dalgliesh e de Mills Winram. |
| Via pus aisida | |
| Geologia | |
| Edat | Pliocèn |
| Ròcas | Dacita, andesita/andesita basaltica |
| Tipe | estratovolcan |
| Activitat | endormit |
| Darrièra erupcion | circa 410 avC |
| Còde [1] | 320180 |
| Observatòri volcanologic | Comission geologica de Canadà |
Lo mont Meager (en anglés Mount Meager o Mount Meager massif) es un grop de volcans canadencs situat dins los cadenons del Pacific al sud-oèst de Colómbia Britanica, 150 km al nòrd de Vancouver. Amb una altitud maximala de 2 680 m, fan partida de l'Arc volcanic dei Cascadas.
Tèxte anglés de traduire :
The massif is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits including Mount Meager which is the second highest of the massif.
The massif is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits including Mount Meager which is the second highest of the massif.