Me and friend on a proper volcano

One of the reasons I tend to be happy is I like to find out I’m wrong about things, because then I learn new things, and that makes me happy, and I’m constantly wrong about things.

Case in point: granite. I’m standing on big galloping humps of granite in Maine and wondering how they got there. Granite, I figured, is metamorphic. There are all these bits and flecks glommed together in granite, and I assumed the only way they got there in one place is that they got smashed together and rumpled up. And there was a lot of rumpling going on. For instance, North America and Africa once smashed into each other and collaborated on rumpling up the towering Appalachian mountain range. So clearly granite is not igneous rock like our own Oregon basalt. Volcanoes in Maine? I think not.

Guess what? Volcanoes in Maine! I had no idea. I was completely igneant about it.

It’s just not the same kind of igneous rock as we mostly have in Oregon. Volcanic activity didn’t write the whole story in Oregon but it dominated the plot line. Our (currently) tallest mountain range came about because the ocean floor shoved itself underneath our shoreline and by the time it had submerged sufficiently—about a hundred miles inland—it was under so much pressure it got stressed out and pooped up a nice string of volcanoes, as one does. That’s not precisely what happened, but it’s a good enough picture for armchair amateurs like myself.

Dave and friend on a proper volcano

So our Cascade range is all big explosive volcanoes, with the cone shape and the showy eruptions, which are ongoing, but about 17 million years ago the place transitioned toward puddly shield volcanoes from which basalt blooped out and blanketed much of the state, to the depth of a mile in places. So, not your big boomers, but a steady, leisurely flow you could outrun, assuming you were here millions of years ago and could keep it up for a hundred miles. Basalt, to my eye, looks like proper lava. And it looks nothing like granite.

But granite was molten once too. Instead of blasting out into the air and cooling quickly, it cools underground in a magma chamber more slowly, producing larger crystals of this and that, and making for a fancier countertop in its final stage. “Okay,” say I, chastened, “it’s igneous rock, but still not exactly a volcano proper. Not in Maine! Just a bunch of magma underground.”

Guess what? Volcanoes in Maine! Big-ass ones too. About 420 million years ago, producing government-issue basalt like anything. Supervolcanoes, they were.

Ayuh.

So learning that made me happy. I’m even happier now, knowing that–finally–I know everything.