New Rocks and Their Tectonic Context
The rock collection is growing. As a geologist, you collect a lot of rocks and minerals in the field. You start to be more selective over time, and I have gotten to the point where I really only sample rocks that have “tectonic significance”. I will explain. In this video, I share some new samples I collected this summer during the UArizona Summer Field Geology course around the western interior USA. Arclogites, the Great Unconformity, corals, and pentacrinus fossils – it was a great HAUL. I hope you find it interesting and learn something valuable. Always feel free to ask questions about field geology or how you can become an Earth scientist. I will almost always respond. TIMESTAMPS: 0:00 Hi & Introduction 2:24 Arclogite 7:19 Flathead Sandstone 9:39 Madison Limestone Rugose Coral 12:45 Eocene Oncoids & Angular Unconformities 15:32 PENTACRINUS 17:30 Goodbye _LINKS TO PAPERS ABOUT ARCLOGITES:_ *Arclogites and their role in continental evolution; part 1: Background, locations, petrography, geochemistry, chronology and thermobarometry* https://www.sciencedirect.com/science/article/abs/pii/S0012825220304219 *Arclogites and their role in continental evolution; part 2: Relationship to batholiths and volcanoes, density and foundering, remelting and long-term storage in the mantle* https://www.sciencedirect.com/science/article/abs/pii/S0012825220305225 *Cyclicity in Cordilleran orogenic systems* https://www.nature.com/articles/ngeo469 If you would like to support my science communication efforts, I have a Patreon where I share my favorite films, music, books, podcasts, and more (https://www.patreon.com/cadenhowlett). There are an accumulating number of Patron-only YouTube videos on the platform. Any contribution on Patreon goes directly back into this platform. Follow Caden: Instagram: https://www.instagram.com/cadenhowlett/ Facebook: https://www.facebook.com/cadenjhowlett Twitter: https://twitter.com/cadenhowlett www.cadenhowlett.com #earth #geology #science #phd #gis #rocks #minerals
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