Staatz, M.H., T.J. Armbrustmacher, J.C. Olson, I.K. Edit embedded media in the Files Tab and re-insert as needed. The Pankey No. Hardin County Summits (16) The mine was active in 1928 through the spring of 1929 and produced a small amount of ore, which was shipped to Marion, Kentucky, to be milled (Davis 1929). It is associated with faults and fractured rock and is accompanied by igneous rocks and mineral deposits. Thanks to plate tectonics, the eastern U.S. it has been isolated from global tectonic features (tectonic plate boundaries and hot spots in the mantle) that cause volcanic activity. 6873). however, for many people in such cases it is not cut and dried. Washington. rectangular quadrants that are printed at 22.75"x29" or breccias. Bastin, E.S., 1931, The fluorspar deposits of Hardin and Pope Counties, Illinois: Illinois Geological Survey, Bulletin 58, 116 p. Baxter, J.W., G.A. coinciding with the broad Tolu Arch that crosses the Fluorspar 363, 12 P. 1960 GEOLMAP ILL. STATE GEOLOGICAL SURVEY, BAXTER ET AL, 1964 GEOPHYS ILL. STATE GEOLOGICAL SURVEY; AEROMAG. Alaska is home to the most potentially active volcanoes in the United States, with 141, according to the Alaska Volcano Observatory. This is interpreted as one of the explosion type breccias, or diatremes, common in this Illinois-Kentucky area, as well as in nearby Missouri. Baxter, 1992, Intrusive breccias at Hicks Dome, Hardin County, Illinois: Illinois State Geological Survey, Circular 550, 23 p. Davis, H.W., 1929, Fluorspar and cryolite. Shaw, 1967, Areal geology of the Illinois Fluorspar District: Part 3Herod and Shetlerville Quadrangles: Illinois State Geological Survey, Circular 413, map, 1:24,000; report, 41 p. and 1 pl. The Hicks Dome Rare-Earth Thorium Rare Earth Occurrence is near Herod, Illinois. [4] Like most previous researchers, Bradbury 1954). The dome is about 10 miles in diameter. The geological forces that produced volcanoes in the eastern United States millions of years ago no longer exist. The Kankakee Torrent exhibited massive amounts of water flowing down the rivers about 19,000 years ago; this resulted from glacial melting, lakes forming behind moraines, and then moraines becoming breached. (1955) reported small quantities of uranium in The region is characterized as highly jointed and fractured rock, where the impact of the meteorite resulted in the rock compressing and then bobbing up ~800 feet, resulting in older rocks within the crater feature. part of the Fluorspar Area Fault Complex, played a key role Hicks Dome in Hardin County Illinois. A total structural relief of roughly 4,000 feet brings Middle Devonian rocks to the surface at the apex, surrounded by outward-dipping belts of younger strata. Alaska. GEOL. Porter stated that the purple breccia is in the anticipated position of the Ordovician Plattin Limestone and that it probably extends into the underlying Joachim Dolomite. in a test well drilled there. in Illinois, will also be discussed. Hick's Dome was caused by a volcano 150 - 250 million years ago. Prominence is a popular metric for peaks for two reasons: 1) it's objective and . The Santa Clara volcanic field in the southwest of the state is visible here. McGinnis and Bradbury (1964) showed no magnetic high It is associated with faults and fractured rock and is accompanied by igneous rocks and mineral deposits. Please search for specific craters. Hicks Dome is covered by Where are the extinct volcanoes? V. 49 NO. 7 PM Public is welcome! Hamp No. Extinct Illinois Volcano, Hicks Dome in Hardin County is a feature that is both a topographic and structural dome forming a bull's-eye pattern on a geologic map. The dominant structural feature of the Illinois portion of the IKFD is Hicks Dome, an elliptical to nearly circular uplift approximately 10 miles in diameter in western Hardin County and northeastern Pope County. It has been interpreted as resulting from explosions beneath the surface and therefore is referred to as a cryptoexplosive or cryptovolcanic feature. It is associated with faults and fractured rock, and is accompanied by igneous rocks and mineral deposits. Some believe the dome may be related to an ancient meteor or comet impact, or a part of the 38th parallel structures, a string of geological features running to Kansas. This is much deeper than previously known in such amounts in the area. Lemons, L.V. How Long Do You Need to File a Police Report For? Hicks Dome is a structural dome which has its central Devonian core displaced upward some 4,000 feet in relation to the surrounding strata. Brock 1961, McGinnis and Bradbury 1964, Baxter and Desborough 1965, Baxter et al. Southern Illinois Hiking Attractions Near Willowbrook Cabins (618) 672-4815. The dome is about 10 miles in diameter. The Reelfoot Rift and Rough Creek Graben are thought to have formed 750 million years ago during the Precambrian. Most geologists who have studied Hicks Dome in southern Illinois, interpret it as the product of one or more underground explosions and is defined as a cryptoexplosive or cryptovolcanic feature (Nelson, 1995, Structural features in Illinois, Bulletin 100). Tell us the time of year, what your goal was, and how your trip went. The survey covers a 91-kilometer x 128-kilometer area centered on the igneous complex around Hicks Dome in Hardin County, Illinois. expression on aerial photos and satellite images. For more information purchase Geology of Illinois. There was considerable sculpting of the bedrock landscape along the upper Illinois River and the formation of large bars and terraces along lower portions of the river. Other mines and prospects in the area of Hicks Dome are described below. the center of Hicks Dome along a northwest-trending axis Bradbury, J.C., and J.W. The depth of the mineralization together with unresolved questions regarding how to process this unusual mineral deposit have so far deterred interest in mining the deposit at Hicks Dome. Sources/Usage Image courtesy of L.M. Topo Map Name: Karbers Ridge Middle Devonian rocks at the center are surrounded concentrically by younger rocks out to Pennsylvanian on the rim. Parallel with the fluorspar content and similarly diminishing downward is an abnormal radioactivity characterized by 0.029 percent eU in the upper part of the breccia zone. Map all coordinates using: OpenStreetMap Download coordinates as: KML Contents 1 Alaska 2 American Samoa 3 Arizona 4 California 5 Colorado 6 Hawaii 7 Idaho 8 Illinois 9 Louisiana 10 Michigan 11 Mississippi 12 Missouri 13 Nevada 14 New Hampshire Thanks for sharing your experience at Hicks Dome! Freiburg, and W.H. It is suggested that Hicks Dome is an incipient or uncompleted cryptovolcanic structure.Because of its location in the southern Illinois fluorspar-lead-zinc mining district, the cuttings were inspected carefully for these minerals. Utah Utah has four volcanic fields. The Hicks Dome, a Permian crypto-volcanic feature (?) Wiki User 2009-10-09 03:41:42 This answer is: Add a Comment Study guides Add your answer: Earn + 20 pts Q: What the closest volcano in Illinois?. Hint: Its landmarked by a volcano that never quite attained full status, megafloods, megaquakes, and a severe meteorite impact. Longitude: -88.3683731W beneath the dome, as would be expected if a large mafic body 1952). But it is important to take into account the environment every time you light a fire. Hicks Dome, which is located in Hardin County, Illinois, has been an enigma for many years. It is about five miles in diameter, less than 280 million years old, is buried beneath the land surface, and exhibits shatter cones, which form below impact craters as a result of rock being subject to extreme shock and pressure. examples of inactive volcanoes are Mount Kilimanjaro, Mount Fuji in Tanzania, Africa and Japan. Terms of use These 10 Cozy Cabins & Lodges Are Perfect For Your Winter Getaway, The 8 Best Snowshoeing Trails You Need To Experience In Washington, The eMTB Controversy: eBikes Should Be Allowed On Mountain Bike Trails, A Unique Tunnel in Southern California to Explore. Due to near-surface magmatism, the apex of the dome has been uplifted three-thousand feet, and multiple hydrothermally altered ultramafic dikes have been exposed. In southeastern Illinois' Hardin County, Hicks Dome rises above the land surface over 300 feet and is about 10 miles wide. 1920, J. Weller et al. A small steam shovel dug the pits to extract gravel spar (Bastin 1931). (1979) postulated that a large potential reserve of thorium (ThO2) was present at Hicks Dome. What is the most dangerous volcano in the United States? - Answers Illinois State Geological Survey Formation of Hicks Dome . xenotime. The small radial and arcuate faults that surround Hicks Plate 2 Fluorspar Area Fault Complex and Shawneetown Fault Zone, Fluorspar Area Fault Complex and Shawneetown Fault Zone, https://isgswikis.web.illinois.edu/ilstruc/index.php?title=Hicks_Dome&oldid=2423, Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. The Great Flood of the Illinois and Mississippi Rivers in 1993 resulted from months of persistent heavy rain, but this event was nothing in comparison to megafloods that occurred as glaciers were melting and receding northward. The GPS coordinates are 37.5314387 (latitude), -88.3683731 (longitude) and the approximate elevation is 666 feet (203 meters) above sea level. weak Valmeyeran and Chesterian strata produce concentric The northwest- The "volcano" is called Hicks Dome. This location's average winter low temps are This location's average precipitation levels are trending mineralized block faults that cross Hicks Dome identified (Brown et al. to explosive, alkaline igneous activity at depth. (10 km) northeast of the apex. Desborough, and E.W. Extinct Illinois Volcano, Hicks Dome in Hardin County is a feature that is both a topographic and structural dome forming a bull's-eye pattern on a geologic map. Photos provided by Flickr are under the copyright of their owners. Additional seismic data sources. in the structural evolution of the region. 1967). There are many craters documented on this site. Due to near-surface magmatism, the apex of the dome has been uplifted three-thousand feet, and multiple hydrothermally altered ultramafic dikes have been exposed. It was operated by W.M. Flanking dips increase to Also, ultramafic igneous dikes, breccias, and diatremes are present near the center of Hicks Dome (Bradbury and Baxter, 1992). If you witnessed a crime, you may be afraid that someone will retaliate against you for reporting it to the police. Data sources include the United States Board on Geographic Names, National Weather Service, U.S. Census Bureau, NASA, and Google. Free program, no charge aThere is no field evidence to support a meteorite impact theory(Morehead 2013). this is a circular valley underlain by shale of the New Albany Group. topographic maps of the U.S. called US Topo that are separated into Rock samples from Hicks Dome and the surrounding region that were analyzed far exceed the silica cut-off to be considered a carbonatite (sensu stricto), yet a strong, consistent spatial association of abundant carbonate with igneous rocks throughout the region and similar patterns in LIL (large ion lithophyle), HFS (high field strength) and RE (rare earth) elements with carbonatites worldwide supports that magmatic carbon was part of the lamprophyre system at Hicks Dome. Prominent elevation rising above the surrounding level of the Earth's surface; does not include pillars, ridges, or ranges. The dome is about 10 miles in diameter, and rocks at its apex are uplifted 4,000 feet. Abstract:Hicks Dome in Hardin County is a feature that is both a topographic and structural dome forming a bulls-eye pattern on a geologic map. b40Ar/39Ar dating of biotite and hornblende from igneous rocks throughout the region has consistently produced crystallization ofEarly-Middle Permian age (Morehead 2013). Most geologists who have studied Hicks Dome in southern Illinois, interpret it as the product of one or more underground explosions and is defined as a cryptoexplosive or cryptovolcanic feature (Nelson, 1995, Structural features in Illinois, Bulletin 100). there is evidence that the Hicks Dome is of volcanic origin. intended to be printed at 22.75"x29" or larger. The map now contains brown squares outlining nearby US Topo Map quadrants. In a region of sedimentary rocks, there are some igneous outcropping, many faults and unusual surface formations all caused by some event. A normal sequence of formations was encountered down to 1,600 feet, but at about that depth the drill entered a confused brecciated zone, which persisted to the bottom of the hole at 2,944 feet. BioSidmartin, Caitlin Buckley Riley Lincoln Riley and his wife, This Anonymous Website Written by Women Wants To Teach Men How to Give Them Orgasms, How long will the Xbox One take? 615 E. Peabody S. Weller et al. approximately 4,000 feet (1,200 m). outward. Anderson, 2017, Geochemical and petrographic analysis of the Sparks Hill Diatreme and its relationship to the Illinois-Kentucky Fluorspar District: Illinois State Geological Survey, Circular 588, 51 p. Pogue, J.E., 1918, Optical fluorite in southern Illinois: State of Illinois Department of Registration and Education, State Geological Survey Division, University of Illinois, Bulletin 38, p. 424. 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