geology of southern oklahoma

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Geology of Southern Geology of Southern Oklahoma Oklahoma Group #6 Ronnie Miller Amy Miller Kim Scott Kristi Birdsong Hannah Benson Amy Benson Reina Womack Tammara Cook Brenda Wright Lee Vertrees

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Geology of Southern Oklahoma. Group #6 Ronnie Miller Amy Miller Kim Scott Kristi Birdsong Hannah Benson Amy Benson Reina Womack Tammara Cook Brenda Wright Lee Vertrees. Sedimentary Rocks of Bryan County. Quaternary Period. Alluvium 20-30 ft deep - PowerPoint PPT Presentation

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Page 1: Geology of Southern Oklahoma

Geology of Southern OklahomaGeology of Southern OklahomaGroup #6

Ronnie Miller

Amy Miller

Kim Scott

Kristi Birdsong

Hannah Benson

Amy Benson

Reina Womack

Tammara Cook

Brenda Wright

Lee Vertrees

Page 2: Geology of Southern Oklahoma

Sedimentary Rocks Sedimentary Rocks of Bryan Countyof Bryan County

Page 3: Geology of Southern Oklahoma

Quaternary PeriodQuaternary Period

• Alluvium• 20-30 ft deep• Sediment that will eventually form conglomerate

rocks• 10,000 years –present• Qt

Page 4: Geology of Southern Oklahoma

Cretaceous PeriodCretaceous Period

Page 5: Geology of Southern Oklahoma

Dexter SandstoneDexter Sandstone

• 85-90 ft thick• Kwd• Shallow ocean formation• Natural Aquifer• Yellow brown, iron

containing sedimentary rock

Page 6: Geology of Southern Oklahoma

Bennington LimestoneBennington Limestone

• 7-13 feet thick• Kb• Deep Ocean

Formation• Hard limestone

w/fossil• Blue-gray, very

dense, fossilized limestone

Page 7: Geology of Southern Oklahoma

Fossilized Bennington LimestoneFossilized Bennington Limestone

• 7-13 feet thick• Kb• Deep Ocean Formation• Hard limestone w/fossil• Blue-gray, very dense,

fossilized limestone

Page 8: Geology of Southern Oklahoma

Pawpaw SandstonePawpaw Sandstone

• 40-45 feet thick• Kbp• Youngest of the

Bokchito Formation

Page 9: Geology of Southern Oklahoma

Evidence of SandstoneEvidence of Sandstone

• Sandstone is permeable to water. Natural Aquifer

• Plant Growth– Willow Trees– Mimosa Tres– Cat tails– Horse tail rush

Page 10: Geology of Southern Oklahoma

Soper LimestoneSoper Limestone

• 0-2 feet thick• Kbs• Deep Ocean Deposit• Gray, fossilized

limestone

Page 11: Geology of Southern Oklahoma

Caddo FormationCaddo Formation

• 150-160 feet thick• Kc• Alternating layers of

limestone and shale• Cream colored

limestone, gray colored shale

Page 12: Geology of Southern Oklahoma

Kiamichi FormationKiamichi Formation

• 30-40 feet thick• Kk• Deep Ocean

Formation• Dark-gray to black

limestone• Fossilized with

ammonites

Page 13: Geology of Southern Oklahoma

Geology of Johnston CountyGeology of Johnston County

Page 14: Geology of Southern Oklahoma

Antlers SandstoneAntlers Sandstone

• 250-600 feet thick• Ka• Poorly cemented,

unfossilized, white to yellow sandstone

• Used by Cardinal Glass in Durant

• Also used as frac sand by oil companies

Page 15: Geology of Southern Oklahoma

Wapanuka FormationWapanuka Formation

• Limestone and Shale interbedded

• Shallow Ocean formation

• Calcium Carbonate from coral reefs

• Crinoids fossils abundant

Page 16: Geology of Southern Oklahoma

Springer FormationSpringer Formation

• Limestone on the ground

• Lichens tend to grow on limestone giving them a darker appearance

• Found at the edge of the Arbuckle-Simpson Aquifer

Page 17: Geology of Southern Oklahoma

Woodford ShaleWoodford Shale

• Dark colored shale• Presence of phosphate

nodules• Natural gas deposits are

found in Woodford shale• MDsw• Deep Ocean Deposit• 360-408 million years

Page 18: Geology of Southern Oklahoma

DolomiteDolomite

• Thick deposit of Magnesium Carbonate

• Ocm• 438-500 million years

Page 19: Geology of Southern Oklahoma

GranodioriteGranodiorite

• P€gr• Medium-grained

hornblende-biotite

Page 20: Geology of Southern Oklahoma

Troy GraniteTroy Granite

• P€tr

• Medium-grained pink granite

Page 21: Geology of Southern Oklahoma

Tishomingo GraniteTishomingo Granite

• 1.37 billion years• P€ti

Page 22: Geology of Southern Oklahoma

Granitic GneissGranitic Gneiss

• 1.39 billion years • P€gg

Page 23: Geology of Southern Oklahoma

Trip Through the Arbuckles

Page 24: Geology of Southern Oklahoma

Anticlines

• Form when convergent forces in the earth fold rock layers upward.

• Causing the oldest layers at the core with younger layers progressing outward from the core

Page 25: Geology of Southern Oklahoma

Synclines

• Form when convergent forces in the earth fold rock layers downward.

• Causing the oldest layers at the core with younger layers progressing outward from the core

Page 26: Geology of Southern Oklahoma

Faults

• Occur where forces inside earth have caused layers to break and fall at different angles.

Page 27: Geology of Southern Oklahoma

Collins Ranch Conglomerate

• IPcr• 3000 ft thick est.

Page 28: Geology of Southern Oklahoma

Woodford Shale

• MDw• Blake shale

Page 29: Geology of Southern Oklahoma

Viola Group

• Limestones that form steep resistant ridges

• Ov• 684 feet thick

Page 30: Geology of Southern Oklahoma

Oil Creek Formation

• Basal Sandstone• Ooc• 747 ft thick

Page 31: Geology of Southern Oklahoma

Joins Formation

• Thin bedded, fossiliferous light gray limestone

• Oj• 294 feet thick

Page 32: Geology of Southern Oklahoma

West Spring Creek Limestone

• 284 ft thick• Ow• Mostly gray to tan

limestones

Page 33: Geology of Southern Oklahoma

Butterly Dolomite

• Oldest member of the upper Arbuckle group

• Ob

Page 34: Geology of Southern Oklahoma

Sylvian Shale

• Mostly olive green plastic to fissile clay shale

• Os• At contact zone with

Keel Limestone of the Hunton Group

Page 35: Geology of Southern Oklahoma

Kindblade Formation

• Gray, fine grained limestone

• Ok• 1440 feet thick

Page 36: Geology of Southern Oklahoma

Royer Dolomite

• Only Cambrian sample• Pink to gray massive

dolomite• Cry