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2. List of mapped rock formations in Pennsylvania - Wikipedia

   en.wikipedia.org/wiki/List_of_mapped_rock...

   The rocks are listed in stratigraphic order. [1] System Group name Formation name Member name Map symbol [2] Triassic: Newark Group: Passaic Formation: Trp Triassic ...

3. Ever gone rockhounding near the Tri-Cities area? You can find ...

   www.aol.com/news/where-collect-fun-rocks-near...

   Near the Tri-Cities, rockhounding is popular along the Columbia River, Horse Heaven Hills, Saddle Mountains, Bickleton and the Ginkgo Petrified Forest State Park. Rockhounding on WA DNR-managed land

4. List of rock formations in the United States - Wikipedia

   en.wikipedia.org/wiki/List_of_rock_formations_in...

   Spider Rock Pinnacle Balanced Rock The West and East Mitten Buttes Window Rock. Antelope Canyon; Canyon de Chelly National Monument. Spider Rock; Capitol Butte; Cathedral Rock, Red Rock State Park, Sedona; Cathedral Rock (Coconino County, Arizona) Chaistla Butte; Chiricahua National Monument. Big Balanced Rock; Duck on a Rock; Mushroom Rock ...

5. List of quarries in the United States - Wikipedia

   en.wikipedia.org/wiki/List_of_quarries_in_the...

   Walczak-Wontor Quarry Pit Workshop, near Cataract, Wisconsin, NRHP-listed. Address-restricted archeological site. Krukowski Quarry, a sandstone quarry near Mosinee, Wisconsin. It yields late Cambrian period fossils, in the course of quarrying rock slabs for countertops and other purposes.

6. Flatirons - Wikipedia

   en.wikipedia.org/wiki/Flatirons

   The Flatirons are rock formations in the western United States, near Boulder, Colorado, consisting of flatirons.There are five large, numbered Flatirons ranging from north to south (First through Fifth, respectively) along the east slope of Green Mountain (elev. 8,148 ft or 2,484 m), and the term "The Flatirons" sometimes refers to these five alone.

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9. Geology of Massachusetts - Wikipedia

   en.wikipedia.org/wiki/Geology_of_Massachusetts

   In eastern Massachusetts, other Cambrian-age rocks are found in the Nashoba Formation, which has alternating layers of biotite- and hornblende-gneiss, schist, quartzite and amphibolite. The source rock for the Nashoba Formation was likely a low-grade bauxite clay, highly enriched in aluminum, helping to produce large quantities of muscovite.