Genvr102 nc 0_nc_geology_cms_greg11
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Transcript of Genvr102 nc 0_nc_geology_cms_greg11
North Carolina North Carolina GeologyGeology
Dr. Greg PillarDr. Greg Pillar
Assistant Professor of Assistant Professor of Environmental Science and ChemistryEnvironmental Science and Chemistry
Queens University of CharlotteQueens University of Charlotte
Rock Cycle
WeatheringAnd erosion
Deposition andlithification
Sediments
MetamorphicRock
SedimentaryRock
IgneousRock
Deposition andlithification
Sediments
Weathering and erosion
Melting
Melting
Magma
Magma
Cooling
Cooling
Heat andpressure
Heat andpressure
Most recent (lots of mammals)Most recent (lots of mammals)Four main Four main parts of parts of geologic time geologic time scale (based scale (based on fossils)on fossils)
Dinosaurs and first Dinosaurs and first flowering plantsflowering plants
Appearance of fish, plants, Appearance of fish, plants, insects, reptiles, etc.insects, reptiles, etc.
Before shells and Before shells and hard partshard parts
If Earth history If Earth history were 1 yearwere 1 year
600 MYA
Supercontinent of Rodinia
550 MYA
Iapetus
Ocoee Basin
**
500 MYA
Parts of Asia
North America
Parts of Europe
500 MYA
Taconic Orogeny
**
370 MYA
Avalonia
Parts ofAsia
North Americaand
Parts of Europe
Africa andSouth Amer.(Gondwana)
370 – 400 MYA
AcadianOrogeny*
**
300 - 330 MYA
AlleghenianOrogeny
**
280 MYA
Supercontinent of Pangaea
North America
Appalachian Mtns.
South America.
Africa.
Tethys Sea
Africa,Antarctica,Australia
North America
150 MYA
South America
Parts of Europeand Asia
NorthAmerica
Africa
India, Australiaand Antarctica
**
How did the state of North Carolina develop?
What caused the formation of the geologic belts within North Carolina?
What type of rocks would you expect to find within each belt (physiographic province)?
Geologic Belts: Areas with similar rock types and geologic history
Brevard Fault (blue ridge escarpment)
Inner Piedmont Belt: most deformed/metamorphosed portion of the Piedmont, rocks are about 500 – 700 myo (Iapetus Rocks)
Rocks
Gneiss andSchist with (younger) granitic intrusions
Kings Mountain Belt: moderately deformed and metamorphosed volcanic and sedimentary rocks about 400 – 500 myo
Rocks
Schistt, marblephyllite, quartzitegneiss
monadnocks
Charlotte Belt: consists mostly of igneous rocks, 300-500 myo(tactonic orogeny)
Rocks
Granite, diorite,gabbro (mafic)
Carolina Slate Belt: consists of heated and deformed volcanic and sedimentary rocks (gondwana terranes)
Rocks
granite, argillite, slate, schist, phyllite, gneiss, quartzite, and gold
Triassic basins: the basins are filled with sedimentary rocks about 190-200 mya.
Rocks
conglomerate,sandstone,mudstone
Coastal Plain: wedge of marine sedimentary rocks that thickens as you move toward the east
Orangeburg scarp (fall zone)(2 myo)
Suffolk scarp(125,000 y)