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The Canadian Cascade Arc, also called the … The Canadian Cascade Arc, also called the Canadian Cascades, is the Canadian segment of the North American Cascade Volcanic Arc. Located entirely within the Canadian province of British Columbia, it extends from the Cascade Mountains in the south to the Coast Mountains in the north. Specifically, the southern end of the Canadian Cascades begin at the Canada–United States border. However, the specific boundaries of the northern end are not precisely known and the geology in this part of the volcanic arc is poorly understood. It is widely accepted by geologists that the Canadian Cascade Arc extends through the Pacific Ranges of the Coast Mountains. However, others have expressed concern that the volcanic arc possibly extends further north into the Kitimat Ranges, another subdivision of the Coast Mountains, and even as far north as Haida Gwaii (formerly known as the Queen Charlotte Islands). Over the last 29 million years, the Canadian Cascade Arc has been erupting a chain of volcanoes along the British Columbia Coast. At least four volcanic zones in British Columbia are related to Cascade Arc volcanism. This includes a large volcanic plateau in The Interior and three linear volcanic belts on The Coast. They were formed during different geological periods, separated by millions of years, and occur in three regions referred to as the back-arc, main-arc and fore-arc. The youngest of the three belts has been sporadically active over the last 4.0–3.0 million years, with the latest eruption having taken place possibly in the last 1,000 years. About 2,350 years ago, a major explosive eruption occurred, sending a massive ash column into the atmosphere. This is recognized as the largest volcanic eruption throughout Canada within the last 10,000 years. In historical times, the Canadian Cascade Arc has been considerably less active than the American portion of the volcanic arc. It also has no records of historical eruptions. Nevertheless, the volcanic arc poses a threat to the surrounding region. Any volcanic hazard—ranging from landslides to eruptions—could pose a significant risk to humans and wildlife. Even though there are no historical eruptions in the Canadian Cascade Arc, eruptive activity is very likely to resume; if this were to happen, relief efforts would be quickly organized. Teams such as the Interagency Volcanic Event Notification Plan (IVENP) are prepared to notify people threatened by volcanic eruptions.y people threatened by volcanic eruptions.
, El Arco de las Cascadas Canadienses, tambi … El Arco de las Cascadas Canadienses, también llamado Cascadas Canadienses, es el segmento canadiense del de América del Norte. Situado completamente dentro de la provincia canadiense de Columbia Británica, se extiende desde las Montañas Cascada en el sur hasta las Montañas de la Costa en el norte. Específicamente, el extremo sur de las Cascadas Canadienses comienza en la frontera entre Canadá y los Estados Unidos. Sin embargo, no se conocen con precisión los límites específicos del extremo septentrional y la geología de esta parte del arco volcánico no se conoce bien. Los geólogos aceptan ampliamente que el arco de las Cascadas Canadienses se extiende a través de las cordilleras del Pacífico de las Montañas Costeras. Sin embargo, otros han expresado su interés por el hecho de que el arco volcánico se extienda posiblemente más al norte en la , otra subdivisión de las montañas costeras, e incluso tan al norte como Haida Gwaii (antes conocida como las islas Reina Carlota). Durante los últimos 29 millones de años, el Arco de las Cascadas Canadienses ha entrado en erupción en una cadena de volcanes a lo largo de la costa de la Columbia Británica. Al menos cuatro zonas volcánicas de la Columbia Británica están relacionadas con el vulcanismo del Arco de las Cascadas. Esto incluye una gran en el interior y tres cinturones volcánicos lineales en la costa. Se formaron durante diferentes períodos geológicos, separados por millones de años, y se producen en tres regiones denominadas back-arc, main-arc y fore-arc. El más joven de los tres cinturones ha estado esporádicamente activo durante los últimos 4,0-3,0 millones de años, y la última erupción ha tenido lugar posiblemente en los últimos 1.000 años. Hace unos 2.350 años, se produjo una importante erupción explosiva, que envió una masiva columna de cenizas a la atmósfera. Esta es reconocida como la mayor erupción volcánica en todo Canadá en los últimos 10.000 años. En tiempos históricos, el Arco de la Cascada Canadiense ha sido considerablemente menos activo que la porción americana del arco volcánico. Tampoco tiene registros de erupciones históricas. No obstante, el arco volcánico representa una amenaza para la región circundante. Cualquier peligro volcánico -desde los deslizamientos de tierra hasta las erupciones- puede suponer un riesgo importante para los seres humanos y la vida silvestre. Aunque no hay erupciones históricas en el arco de cascada canadiense, es muy probable que se reanude la actividad eruptiva; si esto ocurriera, se organizarían rápidamente actividades de socorro. Equipos como el Plan Interinstitucional de Notificación de Eventos Volcánicos (IVENP) están preparados para notificar a las personas amenazadas por las erupciones volcánicas. amenazadas por las erupciones volcánicas.
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| rdfs:comment |
El Arco de las Cascadas Canadienses, tambi … El Arco de las Cascadas Canadienses, también llamado Cascadas Canadienses, es el segmento canadiense del de América del Norte. Situado completamente dentro de la provincia canadiense de Columbia Británica, se extiende desde las Montañas Cascada en el sur hasta las Montañas de la Costa en el norte. Específicamente, el extremo sur de las Cascadas Canadienses comienza en la frontera entre Canadá y los Estados Unidos. Sin embargo, no se conocen con precisión los límites específicos del extremo septentrional y la geología de esta parte del arco volcánico no se conoce bien. Los geólogos aceptan ampliamente que el arco de las Cascadas Canadienses se extiende a través de las cordilleras del Pacífico de las Montañas Costeras. Sin embargo, otros han expresado su interés por el hecho de que el arco do su interés por el hecho de que el arco
, The Canadian Cascade Arc, also called the … The Canadian Cascade Arc, also called the Canadian Cascades, is the Canadian segment of the North American Cascade Volcanic Arc. Located entirely within the Canadian province of British Columbia, it extends from the Cascade Mountains in the south to the Coast Mountains in the north. Specifically, the southern end of the Canadian Cascades begin at the Canada–United States border. However, the specific boundaries of the northern end are not precisely known and the geology in this part of the volcanic arc is poorly understood. It is widely accepted by geologists that the Canadian Cascade Arc extends through the Pacific Ranges of the Coast Mountains. However, others have expressed concern that the volcanic arc possibly extends further north into the Kitimat Ranges, another subdivision of the Ctimat Ranges, another subdivision of the C
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| rdfs:label |
Canadian Cascade Arc
, Arco de las Cascadas Canadienses
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