Dinosaur National Monument, Moffat Co, CO 5/25/2013 |
How would we do that? The same way we would read the story we see here:
Black Oak (Quercus velutinus), Illinois Beach State Park, Lake County, IL 4/25/2014 |
Much of this story probably predates my moving into the area -- oaks are slow growers. Despite that, I feel quite confident that we can know what happened to this tree. We can watch these processes happen elsewhere, and observe the signs that those processes leave behind. That gives us the knowledge we need to infer those processes when all we have are the signs that remain.
This is how we would read the story of Dinosaur National Monument, too. We can observe sediments settling in various settings, we can compress and heat small samples of those same sediments to see how rock forms, and we can compare the fossil remains that Dinosaur is famous for to modern creatures and to fossils from other locations on Earth. Those modern processes tell us, for instance, that the most famous fossils in the park came from animals that were buried in a river's floodplain, in an otherwise rather dry area. And they tell us that sediments form in horizontal layers -- when we see angled layers of rock, or curls like we see here, then we can confidently say that the land itself has been folded by the immense forces of continental drift.
I sometimes tell my students that every place has a story to tell, if we take the time to learn the language. Sometimes the story is short, in a script best read by ecologists. Sometimes, as here, it's a Russian novel, set in a font defined by millions of years of geology.
I sometimes tell my students that every place has a story to tell, if we take the time to learn the language. Sometimes the story is short, in a script best read by ecologists. Sometimes, as here, it's a Russian novel, set in a font defined by millions of years of geology.
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