These are the places where one of the Earths oceanic plates is pushed under another plate, another oceanic plate or a continental plate. J.C. Bradbury and J.W. Data were collected along east-west flight lines spaced 200 meters apart with north-south tie lines flown every 3,000 meters. Three very large seismic events shook the region; more than 200 moderate to large aftershocks also occurred. 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. 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. miles (16 km) in diameter and its total structural relief is however, for many people in such cases it is not cut and dried. . > Mafic Intrusive Rock, Volcanic Rock (Aphanitic) 252 13 Ma and 269 13 Ma (K-Ar, bio, mica peridotite) REE minerals. 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. 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). BROWN, J.S., EMERY, J.A., AND MEYER, P.A., JR., 1954, EXPLOSION PIPE IN TEST WELL ON HICKS DOME, HARDIN COUNTY, ILLINOIS: ECON. Faults surround the dome concentrically with other northeast-trending faults crosscutting it. 7 PM Public is welcome! View of Hicks Dome, Hardin County, Illinois, looking East. 1967, Hook 1974, Trace 1974, Nelson and Lumm 1987, Bradbury and Baxter 1992. Antrim. Plutonic Rock Mann was ongoing here in 1939 (Davis and Trought 1940). Where are dormant Illinois volcanoes? 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. The dome has small associated igneous dikes around its flanks. Champaign, IL 61820 activity, but no pluton or laccolith at depth is indicated, as in Overview Fingerprint Abstract Hick's Dome is a crypto-volcanic feature within the south-central portion of the Illinois Basin. The origin of Hicks Dome is clearly related to igneous Richard C. Berg, Director identified (Brown et al. Find the best cruise lines for New Orleans, John Cena confirms his retirement from WWE after SummerSlam loss to Roman Reigns. The deepest exploration hole was more than 2,500 feet and the shallowest was 2,200 feet. approximately 4,000 feet (1,200 m). much breccia, but no conclusively igneous rock was Middle Devonian rocks at the center are surrounded concentrically by younger rocks out to Pennsylvanian on the rim. 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. a maximum of about 20 (as much as 45 locally) about 1 mile to explosive, alkaline igneous activity at depth. Additional seismic data sources. The Pankey No. 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. 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). examples of inactive volcanoes are Mount Kilimanjaro, Mount Fuji in Tanzania, Africa and Japan. 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. site were radioactive and contained unusual concentrations Servant from Season 4: Date, time and departure details, A LOT OF HONEYED MELONS COLLECTED BEFORE RIPENING, Are there crocodiles in Lake Anna? 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. While many volcanoes are like this, others are not. The possibility is suggested that this could have been picked up from the formerly overlying New Albany, or Chattanooga, shale (Brown 1954). [4] While the general rule is as soon as possible, the law sets a time limit, called the statute of limitations, to manage how much time you have to report a crime before it is essentially forgiven.in the eyes of the law. For permissions information, contact the Illinois State Geological Survey. 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). Privacy Statement. 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. Because the nearest station and this geographic feature may have are younger than the dome and ultramafic intrusions. 6873). Devonian chert and limestone form a hill at the center. 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. Rohrer (Weller et al. - Answers Illinois State Geological Survey Formation of Hicks Dome . S. Weller et al. An official website of the United States government. Prominent elevation rising above the surrounding level of the Earth's surface; does not include pillars, ridges, or ranges. Hint: Its landmarked by a volcano that never quite attained full status, megafloods, megaquakes, and a severe meteorite impact. Most geologists concur with Bradbury and Baxter (1992) that the dome is the product of large-scale igneous intrusion and brecciation at depth. It is associated with faults and fractured rock and is accompanied by igneous rocks and mineral deposits. Category: Summits, Hardin County Cliffs (2) official weather station. breccias. Located southwest of Hicks Dome, this prospect comprises several surface pits that follow veins striking N 4047 E (Weller et al. higher than 54% of other locations on record. Drilling into the core of Hicks Dome reveals greatly shattered sedimentary rocks, intermixed with igneous material. 2 . Hicks Dome Rare - Earth, Thorium Prospects Occurrence in Hardin county in Illinois, United States with commodities Fluorine-Fluorite, REE, Thorium Map XML JSON KML B Geologic information Identification information Geographic coordinates Geographic areas Public Land Survey System information Comments on the location information 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. 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. If so, we ask that you post a quick review of it below. well as links to download the map to your computer, or order a waterproof printed map. It goes through the longest tunnel in Illinois. IN THE BRECCIA ZONE, FLUORITE WAS 2 TO 5% AND ONE SAMPLE CONTAINED 12.8% CAF2. Compare with the OMAHA DOME, DES PLAINES DISTURBANCE, Historically the site has been associated with the Illinois-Kentucky Fluorspar Mining District which is now part of the Shawnee National Forest. The dome is about 10 miles in diameter. An aeromagnetic survey by Intrusive Breccias at Hicks Dome, Hardin County, Illinois. (2017) reported the geochemical analysis of a sample composed of a mixture of calcite and fluorite collected from the mine dump in this area. Hick's Dome was caused by a volcano 150 - 250 million years ago. Mines in the Illinois Portion of the Illinois-Kentucky Fluorspar District. Utah Utah has four volcanic fields. and GLASFORD STRUCTURE. However, as time passes, it becomes difficult to investigate the crime, as witnesses may forget what happened, or the evidence may become contaminated. Bradbury et al. The December 16th event had a magnitude estimated to be as great as 7.5, and ground shaking was felt as far away as the East Coast. The volcano never broke the surface but created a crypto-volcanic implosion (a violent collapse inward). Idaho Idaho has four volcanic fields. However, slightly elevated values of copper and rare earth elements were suggested. (Zartman et al. Save my name, email, and website in this browser for the next time I comment. Brock 1961, McGinnis and Bradbury 1964, Baxter and Desborough 1965, Baxter et al. 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. For more information purchase Geology of Illinois. Most geologists accept the theory that the older rocks at the center of the uplift are a result of this deep-seated igneous activity. > Pyroclastic Rock Igneous diatremes are scattered throughout the region, and nearly vertical dike-like intrusive breccia bodies radiate from the center of Hicks Dome (Baxter et al. Topo Map Name: Karbers Ridge b40Ar/39Ar dating of biotite and hornblende from igneous rocks throughout the region has consistently produced crystallization ofEarly-Middle Permian age (Morehead 2013). 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. 6. Sources/Usage Image courtesy of L.M. fracturing at the juncture of the Reelfoot Rift and Rough Creek Graben provided pathways for mantle-derived magmas to intrude into the sedimentary column. In 1969 and 1970, the Industrial Minerals Company excavated additional pits and recovered approximately 436 tons of ore grading 53% CaF. The feature resulting from a large meteorite impact is known as the Des Plaines Disturbance. Hicks Dome, a cryptovolcanic feature in the northwestern part of the Fluorspar Area Fault Complex, played a key role in the structural evolution of the region. A peak's prominence, also known as topographic prominence or relative height, is a measure of how distinct a peak is from other peaks. 2 hole was drilled to 2,485 feet, and the core was composed of breccia cemented by white calcite, with sparse fluorite in the upper portion, but fluorite averaged between 2% and 8% from 2,000 to 2,240 feet. 615 E. Peabody Southern Illinois Hiking Attractions Near Willowbrook Cabins (618) 672-4815. 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. Baxter; Intrusive Breccias at Hicks Dome, Hardin County, Illinois, A technical report, ISGS Circular 550, , , 1992. The borehole at the apex encountered Also, ultramafic igneous dikes, breccias, and diatremes are present near the center of Hicks Dome (Bradbury and Baxter, 1992). 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. Flanking dips increase to How Long Do You Need to File a Police Report For? Geologists working on the deposit designated the breccia as either complex breccia or host breccia. Results were inconclusive because of poor fluorine results along with total weight percentage calculations of 68%. ). Baxter, 1992, provides more details and can be purchased from ISGS for $5.00. 1952). SURVEY, Hicks Dome Rare - Earth, Thorium Prospects, Jr. No. 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 V. 49 NO. Mulvaney-Norris, R.N. The region of Hicks Dome is rich in fluorite and other minerals. The diameter of the dome is about 10 miles. this is a circular valley underlain by shale of the New Albany Group. Where are the extinct volcanoes? 12201 Sunrise Valley Drive Reston, VA 20192, Region 2: South Atlantic-Gulf (Includes Puerto Rico and the U.S. Virgin Islands), Region 12: Pacific Islands (American Samoa, Hawaii, Guam, Commonwealth of the Northern Mariana Islands). Nuelle 1 Oil Test Well and Other Prospects. Illinois' megaquakes are the well-documented New Madrid events that occurred between Dec. 16, 1811, and March 15, 1812. magnetic high, interpreted as a mafic pluton, about 6 miles 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. 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. Don't show this message again Hicks Dome | U.S. Geological Survey Breadcrumb Images Photography Hicks Dome By Communications and Publishing Original Thumbnail Medium Detailed Description View of Hicks Dome, Hardin County, Illinois, looking East. GEOL. Tell us the time of year, what your goal was, and how your trip went. Terms of use 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. Is Hicks Dome a volcano? xenotime. The answer isIllinois! Its called the Craters of the Moon, and its a very low threat. at Hicks Dome: shatter breccias, vent breccias, and carbonatitic 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). 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