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smoky quartz devils playground utah

West Route: From the northern I- 15/I-80 interchange in Salt Lake City, head west on I-80 153 miles to Oasis, Nevada (exit 378). Basin and Range faulting and uplift of the Grouse Creek Mountains (approximately 13 million years ago) subjected the region to extensive physical weathering (surface water runoff and freeze-thaw), which over millions of years slowly peeled off the overlying sediments and sedimentary rocks. Salt Lake City, Utah 84116, Mailing Address: Located on the east side of the Grouse Creek Mountains, the Devil's Playground in an awesome place to explore. Camping at the Devil’s Playground area in Box Elder County, Utah. The Mineral Mountains, located in Beaver County, make up the largest exposed plutonic body in Utah.

The Utah Geological Survey (UGS) is a division of the Utah Department of Natural Resources. Quartz crystals, garnet, epidote, kyanite. Excellent crystals of smoky quartz and feldspar are found in …

More realistic theories are that the treeless patches are the result of past clearing, animal grazing or burning.

Located on Bureau of Land Management and state land, Devils Playground is a relatively unknown geologic curiosity found in a remote region of northwestern Utah. Excellent crystals of smoky quartz and feldspar are found in vugs or cavities in the granite. Devils Playground is not your typical playground at the park, but a playground of granitic rock weathered into fantastic forms and eerie shapes. Quartz crystals can be found throughout the area in vugs and veins within the granite formations. Turn left (southwest) and proceed 74.5 miles to the Emigrant Pass road. They represent the last and most hydrous (waterrich) portion of magma to crystallize. Several specialized programs comprise the UGS: Energy & Minerals, Geologic Hazards, Geologic Information & Outreach, Geologic Mapping, Groundwater & Wetlands, and Paleontology. These peaks, also called “balds” are where trees won’t grow, legendarily because the devil himself stepped there.

Turn right (east) and proceed 0.2 miles to first granitic outcrops of Devils Playground on the right (south) side of the road. At Devils Playground, spires of rock greet the visitor. Travel northwest on I-84 for 37 miles to exit 5. Well you're in luck, because here they come. Eventually, physical and chemical weathering will destroy all of these artistic forms of nature. Turn right (north) and drive approximately 8.5 miles to the Devils Playground sign. Garnet has also been found west towards Ingraham pass and North along Dove Creek Road. Do watch out for rattlesnakes though, they are all over out there. Agloe, NY 12776 | 777-765-4321 | info@example.com. Turn left (north) and travel approximately 8.5 miles to the Devils Playground sign. Though rare, smoky, and rose crystals are occasionally discovered. The most popular color? The area is loaded with old mines, odd rock formations and old mine camps. Turn left (west) on Highway 30 and travel 16 miles to Curlew Junction (a junction with Highway 42).

Take the left fork which slowly takes you south into the playground.

In spheroidal weathering, joints or fractures create initial openings allowing surface water to access the rock from all sides. Water seeping along these fractures slowly decomposes or alters the mineral composition of the granitic rock, causing the rock to weather inward. Though rare, smoky, and rose crystals are occasionally discovered. The pegmatites are fairly common, several inches in thickness, and extend hundreds of feet. A thickness of roughly 3 to 6 miles of rock and sediment was removed before exposing the granitic rocks of the Emigrant Pass pluton. However, these processes will continue to sculpt new features as long as physical and chemical weathering expose granitic rock at Devils Playground. To see the contents of this page, you need to enable JavaScript. North Route: From the northern I- 15/I-80 interchange in Salt Lake City, head north on I-15 for 69 miles to Tremonton (exit 382). We recommend that you update your browser to the latest version. Glad You Asked: Igneous, Sedimentary, & Metamorphic Rocks. If you proceed on this road for several miles, the road will end up in the heart of Devils Playground. Click, County road 18 Alpine Loop Ouray, Colorado, Golden Spike historical site/Spiral Jetty, Utah. Glad You Asked: How Do Geologists Know How Old a Rock Is. JavaScript support is not enabled in your browser. Natural Resources Map & Bookstore 8 a.m. to 5 p.m. during traveling i have experienced and learned all about the world of hand craft and jewelry . Your browser version is outdated. smoky quartz is a small company started in 2004 and was inspired by my travels in the world mostly in the far east. Geologic Background: Devils Playground consists of Tertiary-age (approximately 38 million years old) granitic rock formed from a cooling magma body that intruded overlying Paleozoic (400 to 300 million years old) sedimentary rocks. © 2015-2020  MTNMAD.com All Rights Reserved. Devils Playground, Utah.

Devils Playground is not your typical playground at the park, but a playground of granitic rock weathered into fantastic forms and eerie shapes. Turn right (northeast) on Nevada State Highway 233 (also Utah State Highway 30) for 57 miles to Emigrant Pass road. © 2017 | 202 Grid Blvd. You guessed it: brown. This remote area in west Box Elder county is well known by northern Utah rock hounds. LEARN MORE ABOUT THE UTAH GEOLOGICAL SURVEY, © Copyright - Utah Geological Survey - State of Utah.

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