Though we aren’t searching for gold, some of here in the Geo department do “rush” to California, but in search of a different mineral. Zircon is the keystone to much of the petrographic and volcanological research going on this summer. As Liz wrote earlier, there are different ways to get from a chunk of outcrop to the tiny zircon crystals that we can date.
At last we have gotten to the zircon! This last step requires mad-scientist lab gear and some heavy liquids. They’re called heavy liquids because they are relatively dense- and this is what we are using for the final type of separation to get to the teeny tiny zircon. Zircon is a dense mineral (about 4.6 g/cm3) and will sink to the bottom of the slightly less dense heavy liquid, methylene iodine (3.3 g/cm3), while the majority of the other grains will float.
Summer has arrived in Granville. Warm winds suddenly change to thunder, and the Bluecoats’ music rumbles through campus. For some of us geoscientists, this signals the time to become enthralled in summer research. My second week of research work is coming to a close, and I’m not getting down to the nitty-gritty of why I’m here.
Hello all! This summer I am back at Denison working on a project with Professor Erik Klemetti involving the magmatic evolution of the Lassen volcanic system in Northern California. Lassen is the southernmost volcano in the Cascades Range and has had eruptions as recently as 1915. Our goal is to analyze the zircon minerals that we extract from various samples representing different eruptions and phases of the system.