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#unioncollege — Public Fediverse posts

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  1. is useful for fission-track cooling ages too -its closure temperature is ~220°C (the temperature when the fission tracks are annealed away). John Garver's group at Union college (@geo_garver) used ziron fission tracks to show that the same Adirondack rocks have been cooling since the late-Precambrian/Cambrian rifting of Rodinia.

  2. My students created infographics about a topic we studied in our #PlantEcology class at #UnionCollege. Here are some of my favorites: