A volcano is any location where magma comes to the surface, or has done so within the past several million years. This can include eruptions on the ocean floor (or even under the water of a lake), where they are called subaqueous eruptions, or on land, where they are called subaerial eruptions. Not all volcanic eruptions produce the volcanic mountains with which we are familiar; in fact most of Earth’s volcanism takes place along the spreading ridges on the sea floor and does not produce volcanic mountains at all—not even sea-floor mountains.

Canada has a great deal of volcanic rock, but most of it is old, some of it billions of years old. Only in B.C. and the Yukon are there volcanoes that have been active since 2.6 Ma (Pleistocene or younger), and the vast majority of these are in B.C. We’ll look at those in some detail toward the end of this chapter, but a few of them are shown on Figures 4.0.1 and 4.0.2.

The study of volcanoes is critical to our understanding of the geological evolution of Earth, and to our understanding of significant changes in climate. But, most important of all, understanding volcanic eruptions allows us to save lives and property. Over the past few decades, volcanologists have made great strides in their ability to forecast volcanic eruptions and predict the consequences—this has already saved thousands of lives.

Figure 4.0.1 Mount Garibaldi, near Squamish B.C., is one of Canada’s tallest (2,678 metres (m)) and most recently active volcanoes. It last erupted approximately 10,000 years ago.

Figure 4.0.2 Mount Garibaldi (background left, looking from the north) with Garibaldi Lake in the foreground. The lower volcanic peak in the centre is Mount Price and the dark flat–topped peak to the left of it is The Table. All three of these volcanoes were active during the last glaciation.

Media Attributions

• Figures 4.0.1, 4.0.2: © Steven Earle. CC BY.

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