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  1. Rocks are made of collections of mineral grains that are held together in a firm, solid mass. They are made of minerals (which are crystalline ), or other mineral-like substances. The Earth's outer solid layer, the lithosphere, is made of rock. That means the Earth's crust is made of rock.

  2. Oct 14, 2021 · Some of the best rockhounding sites in Wisconsin include Ounce Creek, Big Falls Park, Iron County, Highway 182, Jackson County, Outagamie County, Saukville, Racine, Eastabrook Park, Oshkosh, Hazel Green, Platteville, Werley, Cobb & Mifflin, and Dodgeville, among many others. Let’s look at some of these locations and see what you can find.

  3. Rockhounding is the hobby of collecting rocks, minerals, and crystals. It’s a great way to get outside and explore nature. Plus, you can find some cool specimens to add to your collection. There are many great places to go rockhounding near Milwaukee.

  4. Jan 12, 2024 · Updated January 12, 2024. Quartz photo provided by Spirifer Minerals - spiriferminerals.com. Rockhounding in Wisconsin is an absolute gem! With its diverse geological landscape, this state offers rock enthusiasts a treasure trove of opportunities. Wisconsin has got plenty of great options for rockhounding success.

  5. Organized in 1967, the HEART OF WISCONSIN GEM AND MINERAL SOCIETY is a non-profit, educational club dedicated to promoting interest and education in the earth sciences and lapidary arts . Members are of all ages and occupations and share a common interest in the earth and the mineral kingdom. Member: Midwest Federation of Mineralogical and ...

  6. Dec 6, 2021 · December 6, 2021. View the story map. Ever wonder what Wisconsin’s most important rocks and minerals are? We’ve created a story map that will help satisfy that curiosity! Adapted from the WGNHS Rock Kit, this interactive story map takes viewers on a virtual tour of our state’s rocks and minerals.

  7. INTRODUCTION. The bedrock geologic record in Wisconsin is divided into two major divisions of time: the Pre-cambrian, older than 600 million years, and the Paleozoic, younger than 600 million years. The Precambrian rocks are at the bottom and consist predominantly of crystalline rocks.

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