Glacial till |
First, about those pictures you dug up from various websites, Rose: they're awfully pretty but our staff glaciologist noticed that they're all of glaciers -- none are of till. We put an image of till at the top of this page, just for reference. But that's not why we've brought you here today. You see, Ms Guastella, you didn't do your research properly. You really cite only one resource in your article, a geologist by the name of Michael Pidwirny (University of British Columbia Okanagan). We appreciate that you seem to have gone to an expert, but Rose? You should have gone to more than one expert. Here's why: your introduction to glaciers says,"A glacier is a mass of accumulated snow and ice that originates in a mountain range..."and while the definition is technically true, it's only half of the story. If you had gone to, oh, we don't know, any of thousands of websites, you would have learned something: what you describe is an alpine glacier, such as you might see in Glacier National Park. But there have also been enormous sheets of ice that cover huge areas, even whole continents, called -- can you guess? -- continental glaciers. You'd think that someone from SUNY Stony Brook would have at least heard of continental glaciation, right? Guess it's that MA in "liberal studies"... |
¹ Leaf called in a rewrite specialist to rework Rose's text, but his version is no better than what she wrote. Bummer...
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SI - GLACIERS
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