| 词条 | Round Mountain (volcano) |
| 释义 |
| name = Round Mountain | photo = | photo_caption = | elevation_m = 1646 | elevation_ref = | prominence_m = 225 | prominence_ref = | location = British Columbia, Canada | range = Garibaldi Ranges | coordinates = {{coord|49|45|53.5|N|123|01|27.1|W|type:mountain_region:CA|display=inline,title}} | topo = NTS 92G/14 | type = Outcrop | age = Pleistocene | last_eruption = Pleistocene | first_ascent = | easiest_route = gravel road }} Round Mountain is an eroded volcanic outcrop in the Garibaldi Volcanic Belt in British Columbia, Canada, located 8 km southwest of Eanastick Meadows, {{convert|9|km|mi|0|abbr=on}} east of Brackendale and {{convert|10|km|mi|0|abbr=on}} south of Mount Garibaldi. It is the highpoint of Paul Ridge and is located in the southwest corner of Garibaldi Provincial Park. Round Mountain formed as a result of subduction of the Juan de Fuca Plate beneath the North American Plate, known as the Cascadia subduction zone. Round Mountain last erupted during the Pleistocene. See also
External links
5 : Subduction volcanoes|Pleistocene volcanoes|Volcanoes of British Columbia|Mountains of British Columbia|Garibaldi Lake volcanic field |
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