Structural geology
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Or, rather, a folded gneiss. Near Edwards, New York.
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- Fault! by Ron Schott
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As a geologist sometimes you're just driving along when Wham! out of nowhere you spot something interesting in a roadcut. In the best of circumstances there's nobody tailgating you and there's a pullout where you can get off the road to photograph the roadcut. This was one of those good situations. I think this is...
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Probably a Basin & Range normal fault, you can see its trace distinctly where the orange Tertiary lacustrine sediments with hoodoos but up abrubtly against dark basalt.
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Exposed in a roadcut just south of Wawa, Ontario, this is one of the Banded Iron Formations (BIFs) in a greenstone belt of the Superior Province.
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This massive syncline is in the Devonian-aged cherty limestones and sandstones of the Helderburg Group. This is outcrop is featured along the newest stretch of the West Virginia new route 55, near the town of Forman. Image made as part of the MAGIC project (Mid-Atlantic Geo-Imagery Collection)
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