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177:. Geologists have evidence of repeated uplifts accompanied by dike intrusions and volcanic extrusions, erosion, and sedimentation with one coral reef having developed during a submergence. Much of the oil at the crest of the dome volatilized during a late uplift, but oil production wells numbered over a hundred in 1934.
311:. Natural gas accumulated in the Selma "gas rock" limestone underlying the Clayton limestone. The structure was noticed by Hopkins in 1917 and a successful gas well was drilled in 1930, but the field was nearly exhausted by 1939. Jackson Volcano ash within the Eutaw Formation produces oil in the
390:
Thomas, David C. and Benson, Sally M., editors. (2005) 1st ed. "Volume 2 -Geologic
Storage of Carbon Dioxide with Monitoring and Verification." in Carbon Dioxide Capture for Storage in Deep Geologic Formations. Amsterdam: Elsevier. pp.
302:
the Cotton Valley formation and deformed it into a dome structure. Thus, the
Tuscaloosa consists of ash and tuff at the dome and eroded igneous rock away from the dome. Volcanic material is also found in the overlying
533:
180:
Jackson
Volcano is believed to have been extinct for at least 66 million years. A hypothesis states that the Jackson Volcano and related igneous activity in Mississippi were a result of the
169:
beneath
Jackson in 1860 due to his observations of surface strata. The dome contains relatively pure carbon dioxide which is used in oil production in Gulf Coast oil fields. The
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360:
Moore, William H. (1965) Hinds County
Geology and Mineral Resources. Jackson, Miss: Mississippi Geological Survey Bulletin 105. p. 149.
643:
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Hilgard, E.W. (1860) Report on the
Geology and Agriculture of the State of Mississippi. Jackson: E. Barksdale, State Printer. p. 129
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Priddy, Richard
Randall (1960) Madison County Geology. University, Miss.: Mississippi State Geological Survey Bulletin 88. p. 36.
61:
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379:
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165:, an area of dense rock clearly noticeable in local gravity measurements. E.W. Hilgard published his theory of an
278:. Igneous activity progressed along an arc in the northern Gulf of Mexico Basin starting with the Prairie Creek
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66 million years ago. Alternatively, the volcanism may have been part of a worldwide eruption driven by
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315:, where oil was first discovered in the Woodruff Sandstone (Selma Chalk), an eroded sand from Jackson.
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Petrogenesis and
Provenance of Epiclastic Volcanic Cobbles From the Cretaceous Woodbine Formation
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Origin of the
Bermuda volcanoes and the Bermuda Rise: History, observations, models, and puzzles
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307:. Subsidence and sea level rise resulted in the deposition of the chalk and limestone of the
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574:. Washington: United States Government Printing Office. pp. 114–116, 122–125.
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Tinsley Oil Field, Yazoo County, Mississippi, in North
American Oil and Gas Fields
298:(80 Ma), and finally the Jackson Dome (70 Ma) in the east. The Jackson intrusion
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data suggests mantle origins with a date of 70 million years for the Jackson Dome
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411:"Mississippi Department of Environmental Quality: Frequently Asked Questions"
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Jackson structure contour map, top of the Clayton, with gas well locations
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439:. Tulsa: The American Association of Petroleum Geologists. p. 239.
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589:. LSU Historical Dissertations and Theses. 4933. pp. 155–159.
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Dockery III, David T.; John C. Marble; Jack Henderson (1997).
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The volcano is one of four total located inside cities in the
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Denbury Resources. "CO2 Sources" Retrieved 28 August 2015.
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Geology of the Jackson Area Mississippi, USGS Bulletin 986
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being the others. The volcano was discovered in 1819.
161:. The uplifted terrain around the volcano forms the
270:extended into present-day Mississippi forming the
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435:Shelton, M.F. (1976). Braunstein, Jules (ed.).
16:Extinct volcano in Mississippi, United States.
192:, similar to the conditions that created the
153:2,900 feet (880 m) beneath the city of
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532:Mississippi, University of (2003-12-12).
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294:(90 Ma), Monroe-Sharkey Uplift with its
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49:2,900 ft (880 m)below Jackson
634:Landforms of Hinds County, Mississippi
624:Extinct volcanoes of the United States
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460:Vogt, Peter R.; Woo-Yeol Jung (2007).
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619:Volcanoes of Mississippi
604:Jackson's Hidden Volcano
570:Monroe, Watson (1954).
268:Western Interior Seaway
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489:10.1130/2007.2430(27)
337:"The Jackson Volcano"
286:) in the west to the
272:Mississippi embayment
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182:North America Plate's
629:Cretaceous volcanoes
473:. pp. 553–591.
276:Tuscaloosa Formation
257:stratigraphic column
159:Mississippi Coliseum
155:Jackson, Mississippi
102:Jackson, Mississippi
344:Mississippi Geology
274:and depositing the
73: /
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128:(unknown, extinct)
39:Highest point
639:Hotspot volcanoes
498:978-0-8137-2430-0
469:. Vol. 430.
313:Tinsley Oil Field
184:passage over the
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77:32.300°N 90.172°W
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296:Midnight Volcano
292:Granite Mountain
118:66,000,000 years
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305:Eutaw Formation
264:Late Cretaceous
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186:Bermuda hotspot
151:extinct volcano
147:Jackson Volcano
82:32.300; -90.172
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515:|journal=
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415:the original
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209:Diamond Head
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194:Deccan Traps
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163:Jackson Dome
157:, under the
146:
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350:(3): 33–45.
309:Selma Group
288:Magnet Cove
262:During the
233:Mount Tabor
221:Pilot Butte
190:superplumes
114:Age of rock
80: /
55:Coordinates
613:Categories
556:2007-09-27
421:2008-07-11
319:References
290:(105 Ma),
139:Cretaceous
68:90°10′19″W
65:32°18′00″N
517:ignored (
507:cite book
475:CiteSeerX
280:lamproite
175:intrusion
171:noble gas
167:anticline
93:Geography
45:Elevation
255:Jackson
237:Portland
213:Honolulu
196:and the
98:Location
247:Geology
207:, with
108:Geology
495:
477:
443:
266:, the
241:Oregon
231:, and
229:Oregon
217:Hawaii
149:is an
550:(PDF)
537:(PDF)
467:(PDF)
391:691-2
340:(PDF)
282:(110
519:help
493:ISBN
441:ISBN
225:Bend
485:doi
235:in
223:in
211:in
615::
539:.
511::
509:}}
505:{{
491:.
483:.
348:18
346:.
342:.
327:^
284:Ma
239:,
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559:.
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
