カナダ · 火砕丘

クロー・ラグーン山

Crow Lagoon

タイプ: 火砕丘
標高: 335m
最終噴火: 不明

A geologist observes the contact between a basaltic Plinian fallout lapilli unit overlying marine clay. This deposit is part of thick beds of basaltic Holocene tephra originating from an unknown Quaternary volcanic center found near Crow Lagoon, north of Prince Rupert near the southern tip of the Alaskan panhandle. Ballistically emplaced bombs imply a nearby source. The tephra beds are located along the south side of the Khutzeymateen Inlet, about 40 km N of Prince Rupert. · 写真: Photo by Jack Souther (Geological Survey of Canada, courtesy of Cathie Hickson).

タイプ: 火砕丘
国: カナダ
地域: 北アメリカ / Northern Cordilleran Volcanic Province
標高: 335m
座標: 54.700, -130.230
最終噴火: 不明
テクトニクス環境: プレート内部 / 大陸地殻 (> 25 km)
火山地形: 小規模
主要岩石: 玄武岩 / ピクライト質玄武岩

地質学的概要

Thick deposits of Holocene basaltic tephra originating from an unknown volcanic center have been found near Crow Lagoon, ~40 km N of Prince Rupert near the southern tip of the SE Alaskan panhandle. The deposits are located along the S side of the Khutzeymateen Inlet. Ballistically emplaced bombs imply a nearby source, which remains unidentified (Souther and Weiland, 1993).

Wikipedia の要約

英語版の要約

Crow Lagoon is a little-known volcanic center located north of Prince Rupert, British Columbia, Canada. There are beds of thick, basaltic tephra that are of Holocene age.

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