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Geology Diving in the Keweenaw Peninsula, North of Eagle Harbor. The large calcite vein in Lake Superior looks translucent and feels smooth. This was formed millions of years ago during the Mesoproterozoic Era. During this time period ancient lava flows from tectonic plate movements as part of the Midcontinent Rift. Super heated minerals like silica created the calcite, quartz, and amethyst we can see underwater and on land in this area. The Volcanic activity in this area produced the only strat
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Geology Diving in the Keweenaw Peninsula, North of Eagle Harbor. The large calcite vein in Lake Superior looks translucent and feels smooth. This was formed millions of years ago during the Mesoproterozoic Era. During this time period ancient lava flows from tectonic plate movements as part of the Midcontinent Rift. Super heated minerals like silica created the calcite, quartz, and amethyst we can see underwater and on land in this area. The Volcanic activity in this area produced the only strat
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PROTEROZOIC EON Introduction The Proterozoic Eon is the geological eon that lasted from about 2.5 billion years ago (Ga) to 541 million years ago (Ma), coming after the Archean Eon and before the Phanerozoic Eon. It is one of the most significant intervals in Earth’s history, as it witnessed major geological, biological, and atmospheric changes that set the stage for complex life. FEATURES 1. Continental Development Stable cratons and large continental landmasses formed. Supercontinents such as
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The calcite vein in the Keweenaw Peninsula near Eagle Harbor, Michigan. This was formed millions of years ago from midcontinent rift and had some of the oldest exposed rock in the world. Many crystals and agates are found around the Keweenaw peninsula because the lava flows in the Mesoproterozoic Era. | Chris Roxburgh
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