Thanks for watching....<br />Meehaz Mountain<br />https://en.wikipedia.org/wiki/Meehaz_Mountain<br /><br />Meszah Peak<br />https://en.wikipedia.org/wiki/Meszah_Peak<br /><br />Moraine Cone<br />https://en.wikipedia.org/wiki/Moraine_Cone<br /><br />Mosquito Mound<br />https://en.wikipedia.org/wiki/Mosquito_Mound<br /><br />Nahta Cone<br />https://en.wikipedia.org/wiki/Nahta_Cone<br /><br />Nanook Dome<br />https://en.wikipedia.org/wiki/Nanook_Dome<br /><br />Nazko Cone<br />https://en.wikipedia.org/wiki/Nazko_Cone<br /><br />Nuthinaw Mountain<br />https://en.wikipedia.org/wiki/Nuthinaw_Mountain<br /><br />Mount Noel<br />https://en.wikipedia.org/wiki/Mount_Noel<br /><br />Opal Cone<br />https://en.wikipedia.org/wiki/Opal_Cone<br /><br />Oshawa Seamount<br />https://en.wikipedia.org/wiki/Oshawa_Seamount<br /><br />Ospika pipe<br />https://en.wikipedia.org/wiki/Ospika_pipe<br /><br />Outcast Hill<br />https://en.wikipedia.org/wiki/Outcast_Hill<br /><br />Mount Overill<br />https://en.wikipedia.org/wiki/Mount_Overill<br /><br />Pali Dome<br />https://en.wikipedia.org/wiki/Pali_Dome<br /><br />Peirce Seamount<br />https://en.wikipedia.org/wiki/Peirce_Seamount<br /><br />Perkin's Pillar<br />https://en.wikipedia.org/wiki/Perkin%27s_Pillar<br /><br />Pharaoh Dome<br />https://en.wikipedia.org/wiki/Pharaoh_Dome<br /><br />Pillow Creek<br />https://en.wikipedia.org/wiki/Pillow_Creek<br /><br />Pillow Ridge<br />https://en.wikipedia.org/wiki/Pillow_Ridge<br /><br />Plinth Peak<br />https://en.wikipedia.org/wiki/Plinth_Peak<br /><br />Pointed Stick Cone<br />https://en.wikipedia.org/wiki/Pointed_Stick_Cone<br /><br />Powder Mountain (British Columbia)<br />https://en.wikipedia.org/wiki/Powder_Mountain_(British_Columbia)<br /><br />Mount Price (British Columbia)<br />https://en.wikipedia.org/wiki/Mount_Price_(British_Columbia)<br /><br />Pylon Peak (British Columbia)<br />https://en.wikipedia.org/wiki/Pylon_Peak_(British_Columbia)<br /><br />The Pyramid (volcano)<br />https://en.wikipedia.org/wiki/The_Pyramid_(volcano)<br /><br />Pyramid Mountain (Wells Gray-Clearwater)<br />https://en.wikipedia.org/wiki/Pyramid_Mountain_(Wells_Gray-Clearwater)<br /><br />Pyroclastic Peak<br />https://en.wikipedia.org/wiki/Pyroclastic_Peak<br /><br />Rainbow Range (Chilcotin Plateau)<br />https://en.wikipedia.org/wiki/Rainbow_Range_(Chilcotin_Plateau)<br /><br />Mount Ray (British Columbia)<br />https://en.wikipedia.org/wiki/Mount_Ray_(British_Columbia)<br /><br />Ridge Cone<br />https://en.wikipedia.org/wiki/Ridge_Cone<br /><br />Ring Mountain (British Columbia)<br />https://en.wikipedia.org/wiki/Ring_Mountain_(British_Columbia)<br /><br />Round Mountain (volcano)<br />https://en.wikipedia.org/wiki/Round_Mountain_(volcano)<br /><br />Ruby Mountain<br />https://en.wikipedia.org/wiki/Ruby_Mountain<br /><br />Satah Mountain<br />https://en.wikipedia.org/wiki/Satah_Mountain<br /><br />The Saucer<br />https://en.wikipedia.org/wiki/The_Saucer<br /><br />Seminole Seamount<br />https://en.wikipedia.org/wiki/Seminole_Seamount<br /><br />Sezill Volcano<br />https://en.wikipedia.org/wiki/Sezill_Volcano<br /><br />Sham Hill<br />https://en.wikipedia.org/wiki/Sham_Hill<br /><br />Sidas Cone<br />https://en.wikipedia.org/wiki/Sidas_Cone<br /><br />Continue.....<br /><br />Source:<br />https://en.wikipedia.org/wiki/List_of_volcanoes_in_Canada<br /><br />Music: Bounce House,Silent Partner; YouTube Audio Library<br /><br />A volcano is a rupture on the crust of a planetary mass object, such as the Earth, which allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.<br /><br />Earth's volcanoes occur because the planet's crust is broken into 17 major, rigid tectonic plates that float on a hotter, softer layer in the Earth's mantle. Therefore, on Earth, volcanoes are generally found where tectonic plates are diverging or converging. For example, a mid-oceanic ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates coming together. Volcanoes can also form where there is stretching and thinning of the crust's interior plates, e.g., in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so-called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Volcanoes are usually not created where two tectonic plates slide past one another.<br /><br />Source:<br />http://en.wikipedia.org/wiki/Volcano
