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. You can also find volcanoes in Japan, Africa, the Land of Ice, Italy, Greece, Mexico, Argentina and Indonesia. the Karbers Ridge, IL US Topo Map quadrant. and at the apex of Hicks Dome (fig. Jackson, W.D., and Christiansen, Grey, 1993, International strategic minerals inventory summary report-- Rare-earth oxides: U.S. Geological Survey Circular 930-N, 68 p. Find additional scientific data near this location, 252 13 Ma and 269 13 Ma (K-Ar, bio, mica peridotite). It is associated with faults and fractured rock and is accompanied by igneous rocks and mineral deposits. The dome has small associated igneous dikes around its flanks. J.C. Bradbury and J.W. Related terms: ahu, berg, bald, butte, cerro, colina, cone, cumbre, dome, head, hill, horn, knob, knoll, mauna, mesa, mesita, mound, mount, mountain, peak, puu, rock, sugarloaf, table, volcano. All rights reserved. TRACE, R.D., 1960, SIGNIFICANCE OF UNUSUAL MINERAL OCCURRENCE AT HICKS DOME, HARDIN COUNTY, ILLINOIS: USGS PROF. PAPER 400B P. B63 - B64. Please search for specific craters. View of Hicks Dome, Hardin County, Illinois, looking East. Coppa, and B.V. Clingan, 1979, Principal thorium resources in the United States: U.S. Geological Survey, Circular 805, 42 p. Weller, J.M., R.M. Terms of use The origin of Hicks Dome is clearly related to igneous This page was last edited on 22 July 2021, at 16:20. It is associated with faults and fractured rock, and is accompanied by igneous rocks and mineral deposits. Intrusive Breccias at Hicks Dome, Hardin County, Illinois. For permissions information, contact the Illinois State Geological Survey. Is Hicks Dome a volcano? The roughly circular dome has prominent topographic Also, ultramafic igneous dikes, breccias, and diatremes are present near the center of Hicks Dome (Bradbury and Baxter, 1992). The dome is about 10 miles in diameter. V. 49 NO. Its called the Craters of the Moon, and its a very low threat. 1-16-11 DREAM: i was living in southern Wisconsin, and my mother-in-law came to visit our family. the center of Hicks Dome along a northwest-trending axis It has been suggested that Hicks Dome resulted from a meteorite impact, but the surficial and underground structure of the dome clearly indicate that the forces that formed the dome came from below, rather than above the surface. A correlation of formations between this and the earlier Fricker well is presented. Host breccia is richer in rock flour, which is porous and susceptible to fluoriterare earth mineralization (Larry Nuelle, personal communication with Ross Lillie, May 2018). Data sources include the United States Board on Geographic Names, National Weather Service, U.S. Census Bureau, NASA, and Google. How many volcanoes are there in the United States? 252 13 Ma and 269 13 Ma (K-Ar, bio, mica peridotite) REE minerals. This location's average precipitation levels are The answer isIllinois! Mann was ongoing here in 1939 (Davis and Trought 1940). Development work by the Big Creek Fluorspar Company and A.B. The Hicks Dome, a Permian crypto-volcanic feature (?) higher than 55% of other locations on record. breccias. Official websites use .gov The trip will conclude with a walking tour at the Garden of the Gods Recreational Area to view the Eagle Valley Syncline and Lower Pennsylvanian units. Category: Summits, Hardin County Cliffs (2) Klauea Volcano on Hawaiis Big Island is the most dangerous volcano in the United States, according to the latest National Volcanic Threat Assessment from the United States Geological Survey (USGS). and GLASFORD STRUCTURE. This location's average summer high temps are Bonfire and the day of surf at the beach, whether youre camping or on the beach, Fire load s |_| 514 SHARES Facebook Twitter Pinterest E s |_| hows my light, heat flickering of a fire on the beach, theres something magical about the sound of the crashing waves supported by the set. If so, we ask that you post a quick review of it below. expression on aerial photos and satellite images. Geologists working on the deposit designated the breccia as either complex breccia or host breccia. Most volcanoes are located in the Ring of Fire. activity, but no pluton or laccolith at depth is indicated, as in Plutonic Rock Nuelle Drilling into the core of Hicks Dome reveals greatly shattered sedimentary rocks, intermixed with igneous material. The Hicks Dome uplifted ~1200 meters, observed from the west. 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. Mulvaney-Norris, R.N. Freiburg, and W.H. This is interpreted as one of the explosion type breccias, or diatremes, common in this Illinois-Kentucky area, as well as in nearby Missouri. Map and location information for Hicks Dome in Illinois: Hicks Dome is one of the Summits in Hardin County, IL and can be found on the Karbers Ridge USGS topographic quad map. 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. magnetic high, interpreted as a mafic pluton, about 6 miles Explosion pipe in test well on Hicks Dome, Hardin County, Illinois. 363, 12 P. 1960 GEOLMAP ILL. STATE GEOLOGICAL SURVEY, BAXTER ET AL, 1964 GEOPHYS ILL. STATE GEOLOGICAL SURVEY; AEROMAG. (1.6 km) out from the apex and gradually diminish farther Rare earth element mines, deposits, and occurrences. Hardin County Trails (4). 7 PM Public is welcome! (1979) postulated that a large potential reserve of thorium (ThO2) was present at Hicks Dome. Heres an in-depth look at the question: How long do you need to file a police report? 1967, Hook 1974, Trace 1974, Nelson and Lumm 1987, Bradbury and Baxter 1992. Richard C. Berg, Director Ore mineralization has been found at this location, however the precise grade, tonnage, and extent of the mineralization are not known. Longitude: -88.3683731W The "volcano" is called Hicks Dome. There is also a lot of information on Hicks Dome in Geology of Illinois including images showing the fault zones and the underlying and surrounding formations. Geologically, the region of volcanic rocks is called the Midwest Permian Ultramafic district The district lies within the southern part of the Illinois Basin at the juncture between the Reelfoot Rift and Rough Creek Graben. The nearest weather station for both precipitation and Middle Devonian rocks at the center are surrounded concentrically by younger rocks out to Pennsylvanian on the rim. Secure .gov websites use HTTPS In the application for financial assistance in minerals exploration that the Hicks Dome Corporation submitted to the Office of Mineral Exploration, Porter stated that the ore deposit beneath Hicks Dome contained several mineralized purple breccia matrix blocks that were located about 500 to 750 feet beneath the Maquoketa Shale. Idaho Idaho has four volcanic fields. The Hicks Dome is a structural dome in which the central Devonian core is displaced approximately 4,000 feet upward relative to the surrounding strata. Denny, F.B., A.H. Maria, J.L. Tippie, 1952, Geology of the fluorspar deposits of Illinois: Illinois State Geological Survey, Bulletin 76, 147 p. This page was last edited on September 16, 2021, at 15:41. 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. 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. Middle part of the Fluorspar Area Fault Complex, played a key role 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. Several test holes drilled near the crest of Hicks Dome disclosed significant mineralization in the Ordovician strata over a thickness of more than 200 feet. However, slightly elevated values of copper and rare earth elements were suggested. 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. The northwest- known as US Topo Maps. The Hicks Dome Rare-Earth Thorium Rare Earth Occurrence is near Herod, Illinois. The geologist in charge of the Hicks Dome project for Carroll was Joe Porter. Devonian chert and limestone form a hill at the center. 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. The Hicks Dome is underlain by ultramafic igneous rocks and igneous diatremes or breccia pipes. however, for many people in such cases it is not cut and dried. intended to be printed at 22.75"x29" or larger. of fluorite, apatite, and metal sulfides (Brown et al. fracturing at the juncture of the Reelfoot Rift and Rough Creek Graben provided pathways for mantle-derived magmas to intrude into the sedimentary column. Find the best cruise lines for New Orleans, John Cena confirms his retirement from WWE after SummerSlam loss to Roman Reigns. Overview Fingerprint Abstract Hick's Dome is a crypto-volcanic feature within the south-central portion of the Illinois Basin. Sources/Usage Image courtesy of L.M. The deepest exploration hole was more than 2,500 feet and the shallowest was 2,200 feet. > Volcanic Breccia (Agglomerate), New Madirio Fault Zone, 38th Parallel Lineament, Hicks Dome - An Incipient Cryptovolcanic Structure. Middle Devonian rocks at the center are surrounded concentrically by younger rocks out to Pennsylvanian on the rim. 1952). Is there a volcano on the Big Island of Hawaii? It goes through the longest tunnel in Illinois. Drilling into the core of Hicks Dome reveals greatly shattered sedimentary rocks, intermixed with igneous material. Hicks Dome in Hardin County Illinois. There are many craters documented on this site. weak Valmeyeran and Chesterian strata produce concentric 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). Thanks for sharing your experience at Hicks Dome! BROWN, J.S., EMERY, J.A., AND MEYER, P.A., JR., 1954, EXPLOSION PIPE IN TEST WELL ON HICKS DOME, HARDIN COUNTY, ILLINOIS: ECON. 6. The dome is about 10 miles in diameter, and rocks at its apex are uplifted 4,000 feet. A topographical view of Hicks Dome Having spent much of my life traversing the pancake-flat terrain of Illinois, learning about its geologic history has yielded some big surprises. Clicking anywhere within a quandrant will display an info window with the map name, as approximately 4,000 feet (1,200 m). Almost a Volcano: The Geology of Hicks Dome Thursday, Dec. 10, 2015 216 East Monroe St (alley) Carbondale, Illinois Entrance and parking in rear, off Marion and Monroe Streets, across from Rockhill Baptist Church Presenter Brett Denny is an Economic Geologist with the Illinois State Geological Survey. In southeastern Illinois' Hardin County, Hicks Dome rises above the land surface over 300 feet and is about 10 miles wide. Data were collected along east-west flight lines spaced 200 meters apart with north-south tie lines flown every 3,000 meters. 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. 1 Oil Test Well and Other Prospects. The Reelfoot Rift and Rough Creek Graben are thought to have formed 750 million years ago during the Precambrian. Hicks Dome is approximately 10 Tell us the time of year, what your goal was, and how your trip went. 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. 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 possibility is suggested that this could have been picked up from the formerly overlying New Albany, or Chattanooga, shale (Brown 1954). The USGS (U.S. Geological Survey) publishes a set of topographic maps of the U.S. commonly 8 P. 891 - 902. Have you been to Illinois's Hicks Dome before? In which states are there volcanoes in the United States? Hicks Dome is a structural dome which has its central Devonian core displaced upward some 4,000 feet (1,200 m) in relation to the surrounding strata. 4. temperature measurements is ROSICLARE 5 NW which is approximately 5 miles away and has an elevation of 400 feet (266 feet lower than Hicks Dome). to explosive, alkaline igneous activity at depth. Hawaii owes its existence to volcanoes, of which there are five on the island. There are actually four types of mountains that can be created by molten rock. The dome is about 10 miles in diameter, and rocks at its apex are uplifted 4,000 feet. In 1969 and 1970, the Industrial Minerals Company excavated additional pits and recovered approximately 436 tons of ore grading 53% CaF. in the structural evolution of the region. Free program, no charge Washington. The site was first discovered in 1952 by Saint Joseph Lead Company. a maximum of about 20 (as much as 45 locally) about 1 mile Geologic forces uplifted the rocks at the apex of Hicks Dome 1200 meters forming a circular feature that can be observed on aerial photographs and geologic maps. 1952). cuestas and strike valleys. The Rose Mine, located east of the apex of Hicks Dome, produced gravel spar and some bedding replacement ore. Middle Devonian chert and limestone form a hill at the center. (2017) reported the geochemical analysis of a sample composed of a mixture of calcite and fluorite collected from the mine dump in this area. in Illinois, will also be discussed. 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. The earthquakes were by far the largest east of the Rockies in North America. The intense S. Weller et al. Most geologists accept the theory that the older rocks at the center of the uplift are a result of this deep-seated igneous activity. Carbonatite. Although their findings are highly speculative, Staatz et al. 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. there is evidence that the Hicks Dome is of volcanic origin. 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. No. Privacy Statement. The core samples also contained anomalous concentrations of rare earth elements, thorium, and beryllium. outward. The Illinois-Kentucky Fluorite District, Hicks Dome, and Garden of the Gods in southeastern Illinois and northwestern Kentucky | From the Cincinnati Arch to the Illinois Basin: Geological Field Excursions along the Ohio River Valley | GeoScienceWorld Books | GeoScienceWorld All Books By Publisher Prev Next Book Chapter Emery, P.A. In the 1970s, mineral exploration for fluorspar, beryllium, thorium, and rare earth elements was conducted through a cost-sharing agreement between the USGS Office of Mineral Exploration and a private entity operated by John Lee Carroll named the Hicks Dome Account (HDA; Office of Mineral Exploration docket no. 1952) and may have been owned by D.C. Peyton before 1917 (Pogue 1918). Dome apparently developed during its formation. 1967). Bradbury et al. Brownfield, M.R. The trip will conclude with a walking tour at the Garden of the Gods Recreational Area to view the Eagle Valley Syncline and Lower Pennsylvanian units. The region of Hicks Dome is rich in fluorite and other minerals. Mines in the Illinois Portion of the Illinois-Kentucky Fluorspar District. But it is important to take into account the environment every time you light a fire. Hicks Dome is covered by In 1952, St. Joseph Lead Company drilled a well on the apex of Hicks Dome in Hardin County, Illinois, primarily to explore for oil or gas, and with the objective of testing the St. Peter sand horizon, which had not been reached in a previous well on the flank of the dome. The map now contains brown squares outlining nearby US Topo Map quadrants. Surrounding 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. 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. McGinnis and Bradbury (1964) showed no magnetic high Most geologists concur with Bradbury and Baxter (1992) that the dome is the product of large-scale igneous intrusion and brecciation at depth. Hicks Dome: Pilots flying over this hill were amazed to see the shape of a volcano from the air. Flanking dips increase to The small radial and arcuate faults that surround Hicks Its rocks are uplifted about 4,000 feet, with older rocks (Devonian) in the center, concentric rings of younger rocks (Pennsylvanian being the youngest), and many faults within. the case of Omaha Dome. J.S. Brock, J.F. 217-333-4747 The Hicks Dome, a Permian crypto-volcanic feature (?) and M.E. b40Ar/39Ar dating of biotite and hornblende from igneous rocks throughout the region has consistently produced crystallization ofEarly-Middle Permian age (Morehead 2013). 1954). These are the places where one of the Earths oceanic plates is pushed under another plate, another oceanic plate or a continental plate. 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