Its pyroclastic deposits are remnants of explosive volcanism.

In the Garibaldi Volcanic Belt, eruptions occur less often, but it is the site of Canada's most explosive volcanism.

Pyroclastic rocks are the product of explosive volcanism.

The resulting explosive volcanism probably ejected large amounts of dust and debris into the stratosphere causing major cooling (see volcanic winter).

The region has undergone explosive volcanism 1.5-5 million years ago, which resulted in the volcanic tuff that characterizes the existing topography.

The consequences of these strong stresses on the crust initiated explosive volcanism already during the Paleocene.

This explosive volcanism produced almost all (more than 99 percent) of the volcanic material in the Yucca Mountain region.

The Pacific Ring of Fire runs parallel to the line and is the world's foremost belt of explosive volcanism.

Some of the progenitor bodies may even have undergone periods of explosive volcanism and formed magma oceans.

This is evidence of explosive volcanism from Fee's eruptive history, as well as its first volcanic event.