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Lithosphere 3
NC Geology
ppt. by Robin D. Seamon
1
NC GEOLOGY
VOCABULARY:
province Coastal Plains
craton Carolina Slate Belt
Rodinia Fall Line
Pangea Coastal Plain
Triassic Basin Barrier Islands
Appalachian Mountains sounds
Mt. Mitchell
Piedmont Plateau
monadnocks
Piedmont
Blue Ridge Mountains = Great Smoky Mountains
2
North America’s
Origins
Province- area of ancient geological sameness;
origin & history
Craton- a large stable block of crust forming the
nucleus of a continent
We can’t go back in time, so scientists must be
good observers, and put clues together to tell
the story… 3
OLDEST NC LAND AREA:
Appalachian Mountain Province
CLUES
• In these mountains today we see folded &
thrust faulted marine sedimentary rocks,
volcanic rocks, pieces of ancient ocean floor…
• evidence suggests mountain formation from
plate collision 480 mya… the building of
Pangea; ancient Apps near the center
RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html 4
5
Rodinia
forms
Rodinia
breaks
up
Pangea
forms
Pangea
breaks
up
6
7
RODINIA breaks up
700 mya
GONDWANA

(China,
India,
Africa, S
America,
Antarctica)
RODINIA forms
1.1 bya
Laurentia + Baltic
+ Siberia 
LAURASIA
EUROPE
NORTH
AMERICA
Laurentia
ASIA
AFRICA
S. AMERICA
8
9
VIDEO: How North America Got its Shape (5 min)
• 500mya Paleozoic Era, the area that
would later be N America was at the
equator, periodically submerged beneath
the shallow ocean
• layers of sediment & carbonate rock were
deposited on the ocean bottom
• Paleozoic Era; Ordovician Period (440-480mya)
a neighboring oceanic plate subducted under
the NA craton, building the first App Mtns
• volcanoes grew; thrust faulting uplifted &
changed old sedimentary rocks
WHAT WE CAN DEDUCE…
10
• Erosion wore down the App Mtns,
carrying sediments downstream
• mountain building continued
periodically for 250 million years as other
continents melded into the growing Pangea
supercontinent
• 350mya (Carboniferous period) the Ancient
African craton (Gondwana) crashed into
Pangea, pushing up the Appalachians again
• Climate was warm & wet … swamps
RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html
RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html
RESOURCE: http://www.jamestown-ri.info/northern_appalachians.htm
11
Paleozoic Era;
Carboniferous
Period
Paleozoic Era;
Devonian Period
Paleozoic Era;
Permian Period
SWAMPS:
warm &
wet: =
high plant
growth
12
13
• warm, swampy climate allowed much plant
growth on Pangea:
• increase in photosynthesis added much
oxygen to the atmosphere
• extra oxygen allowed for enormous
14
• huge forests of fern-like trees grew
• lignin (tough-like bark) in the trees was
not decomposed as decomposers had not
evolved the ability to decompose it yet
15
• As climate changed, the forests died, leaving
the un-decomposed trees to be buried
• 50 million years of accumulated plant matter
became buried
• Pressure & heat turned it into…
COAL
fossil fuels: coal, oil,
and natural gas from
this time period that
are mined for Energy
+ -
lots of energy
produced
when it is
burned
Polluting &
Non-
renewable
16
While NC is not a coal-mining state, shale deposits
from Chatham county are being considered for
fracking
hydraulic fracturing
(fracking)
fracking: a method of oil &
natural gas extraction by
injecting water, sand &
chemicals into
sedimentary shale rock
VIDEO: What is fracking? (5 min)
17
Where did the sedimentary shale rock come from?
• Mesozoic Era 245 mya Pangea split,
creating rift basins
• Newark Rift System pulled North
America from Africa, forming the Atlantic
Ocean in between
RESOURCE: https://deq.nc.gov/triassic-conglomerates-deep-river-triassic-basin-morrisville-nc18
NC’s
Triassic
Basin
200mya
Smaller inland rifts were formed and filled with
boulders, cobbles, sand, silt, & clay: turned into the
reddish sandstones, siltstones, shale & of mudstones
today
19
20
21
• By the end of the Mesozoic,
much of the old Appalachians were
eroded away
• Cenozoic Era, 50mya the area
uplifted again, streams cut
downward again forming mountain rivers &
canyons on the ancient-formed landscape
RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html
RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html
22
23
NC’s GEOLOGY
TODAY
24
Outer Banks
25
Outer Banks
B
A
D
C
NC’s modern geology determined by plate
tectonics & weather:
- Appalachian Mountains
- mountains were weathered and washed
downhill into rivers, producing the materials
that comprise the coastal plains
- these sediments created beaches and barrier
islands
RESOURCE:
https://www.ncpedia.org/geology
26
N C M O U N T A I N S
oldest
• Blue Ridge Mountains- part of N America’s
Appalachian Mtn chain
• ROCKS: igneous, metamorphic, & sedimentary
• 43 peaks of 6,000 ft
• Mt Mitchell 6,684 ft
• RESOURCES
Mining: deposits of
feldspar, mica, raw
materials
27
28
P I E D M O N T
• Piedmont Plateau- stretches
from Alabama to New Jersey
(includes NC)
• ROCKS: metamorphic, igneous rocks
• landscape worn down to hills
• some isolated hard rock outcroppings remain-
monadnocks- Pilot Mountain, Uwharries
• Carolina Slate Belt- evidence of ancient rift
zone
• RESOURCES
Mining: gneiss, schist, lithium, clay, sand, gravel,
building stone, gold 29
30
Pilot Mountain, Mt Airy NC
C O A S T A L P L A I N
largest region
• During Mesozoic era, the coastal plain
was a wide sloping region well above sea level
• loose soil eroded & deposited at the ocean
forming beaches
• During Cenozoic era, ocean covered then
receded across the NC Coastal Plain region
repeatedly; made terraces
• RESOURCES: sand- used for glass-making
Mining: clay, limestone, phosphates
31
32
33
T h e F A L L L I N E
• Fall Line: line of erosion between the Piedmont
and Coastal Plain regions; hard rocks sink into
softer, eastern rocks
• in rivers this creates natural falls & rapids;
(places to port)
• influenced NC transportation, settlement,
population distribution, and economic
development
• today, scientists look at fall lines to determine
pollution effects on
either side of the line
34
Fall Line Population Centers:
Tar River: Tarboro, Greenville, Rocky Mount
Neuse River: Kinston, Smithfield, Goldsboro
Roanoke River: Weldon
Eno River: Hillsborough
Alamance Creek: Alamance
Fall Line parallels
I-95 N/S
35
36
Great Falls, Potomac River: hard
metamorphic Piedmont Rock
O U T E R B A N K S
• chain of barrier islands 175 miles long;
• sounds separate mainland from the Outer
banks: 30 miles
• Pamlico Sound- largest NC sound
• Albemarle Sound- 2nd largest
• topography constantly changing due
to erosion & deposition: beaches
widen & narrow; inlets close &
open up
• RESOURCES: drill exploration for oil
on the East Coast currently (2018) buffer the
islands by 50 miles 37
38
39
Beach-Waves continually move sand on coastline
Shorelines influenced by:
• waves
• tides
• surface currents
crest crest
wavelength
wave break
Wave “feels” the bottom (slows down)
40
Headland- regions that project into the ocean:
EROSION
Bay- indentations in the shoreline
DEPOSITION
Bathymetry
- contour of
ocean floor
HEADLAND
BAY
41
Longshore current ocean current that moves
parallel to shore.
Creates:
• beach drift (zig-zag pattern)
• spits
42
Spit
• Sand deposit connected to land, extends into
water
Tombolo
• Spit with a hook-like end
These features can form:
Barrier Islands
• Long linear Islands of sand that are deposited
by waves parallel to shore; few km wide
• First line of defense during powerful storms
43
44
45
46
Lighthouses-
Used to navigate ships in the dark to warn them
of the shallow waters & to indicate shoreline
Groin (groyne)
• Man-made, rigid hydraulic structure built along
an ocean shore
• Slows down the longshore current, dropping
sand & building up shoreline
47
48
49
NC Geology LAB
1. Video
2. Labsheet:
• Minerals of NC
• NC Geology
3. Resources Page
50
51
BONUS RESOURCE:
BONUS
http://www.jamestown-ri.info/northern_appalachians.htm
52
53
BONUS
http://www.jamestown-ri.info/northern_appalachians.htm
54
55
56

More Related Content

Lithosphere 3 notes: NC Geology

  • 1. Lithosphere 3 NC Geology ppt. by Robin D. Seamon 1
  • 2. NC GEOLOGY VOCABULARY: province Coastal Plains craton Carolina Slate Belt Rodinia Fall Line Pangea Coastal Plain Triassic Basin Barrier Islands Appalachian Mountains sounds Mt. Mitchell Piedmont Plateau monadnocks Piedmont Blue Ridge Mountains = Great Smoky Mountains 2
  • 3. North America’s Origins Province- area of ancient geological sameness; origin & history Craton- a large stable block of crust forming the nucleus of a continent We can’t go back in time, so scientists must be good observers, and put clues together to tell the story… 3
  • 4. OLDEST NC LAND AREA: Appalachian Mountain Province CLUES • In these mountains today we see folded & thrust faulted marine sedimentary rocks, volcanic rocks, pieces of ancient ocean floor… • evidence suggests mountain formation from plate collision 480 mya… the building of Pangea; ancient Apps near the center RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html 4
  • 5. 5
  • 7. 7
  • 8. RODINIA breaks up 700 mya GONDWANA  (China, India, Africa, S America, Antarctica) RODINIA forms 1.1 bya Laurentia + Baltic + Siberia  LAURASIA EUROPE NORTH AMERICA Laurentia ASIA AFRICA S. AMERICA 8
  • 9. 9 VIDEO: How North America Got its Shape (5 min)
  • 10. • 500mya Paleozoic Era, the area that would later be N America was at the equator, periodically submerged beneath the shallow ocean • layers of sediment & carbonate rock were deposited on the ocean bottom • Paleozoic Era; Ordovician Period (440-480mya) a neighboring oceanic plate subducted under the NA craton, building the first App Mtns • volcanoes grew; thrust faulting uplifted & changed old sedimentary rocks WHAT WE CAN DEDUCE… 10
  • 11. • Erosion wore down the App Mtns, carrying sediments downstream • mountain building continued periodically for 250 million years as other continents melded into the growing Pangea supercontinent • 350mya (Carboniferous period) the Ancient African craton (Gondwana) crashed into Pangea, pushing up the Appalachians again • Climate was warm & wet … swamps RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html RESOURCE: http://www.jamestown-ri.info/northern_appalachians.htm 11
  • 12. Paleozoic Era; Carboniferous Period Paleozoic Era; Devonian Period Paleozoic Era; Permian Period SWAMPS: warm & wet: = high plant growth 12
  • 13. 13 • warm, swampy climate allowed much plant growth on Pangea: • increase in photosynthesis added much oxygen to the atmosphere • extra oxygen allowed for enormous
  • 14. 14 • huge forests of fern-like trees grew • lignin (tough-like bark) in the trees was not decomposed as decomposers had not evolved the ability to decompose it yet
  • 15. 15 • As climate changed, the forests died, leaving the un-decomposed trees to be buried • 50 million years of accumulated plant matter became buried • Pressure & heat turned it into… COAL fossil fuels: coal, oil, and natural gas from this time period that are mined for Energy + - lots of energy produced when it is burned Polluting & Non- renewable
  • 16. 16 While NC is not a coal-mining state, shale deposits from Chatham county are being considered for fracking hydraulic fracturing (fracking) fracking: a method of oil & natural gas extraction by injecting water, sand & chemicals into sedimentary shale rock VIDEO: What is fracking? (5 min)
  • 17. 17 Where did the sedimentary shale rock come from?
  • 18. • Mesozoic Era 245 mya Pangea split, creating rift basins • Newark Rift System pulled North America from Africa, forming the Atlantic Ocean in between RESOURCE: https://deq.nc.gov/triassic-conglomerates-deep-river-triassic-basin-morrisville-nc18
  • 19. NC’s Triassic Basin 200mya Smaller inland rifts were formed and filled with boulders, cobbles, sand, silt, & clay: turned into the reddish sandstones, siltstones, shale & of mudstones today 19
  • 20. 20
  • 21. 21
  • 22. • By the end of the Mesozoic, much of the old Appalachians were eroded away • Cenozoic Era, 50mya the area uplifted again, streams cut downward again forming mountain rivers & canyons on the ancient-formed landscape RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html RESOURCE: https://geomaps.wr.usgs.gov/parks/province/appalach.html 22
  • 26. NC’s modern geology determined by plate tectonics & weather: - Appalachian Mountains - mountains were weathered and washed downhill into rivers, producing the materials that comprise the coastal plains - these sediments created beaches and barrier islands RESOURCE: https://www.ncpedia.org/geology 26
  • 27. N C M O U N T A I N S oldest • Blue Ridge Mountains- part of N America’s Appalachian Mtn chain • ROCKS: igneous, metamorphic, & sedimentary • 43 peaks of 6,000 ft • Mt Mitchell 6,684 ft • RESOURCES Mining: deposits of feldspar, mica, raw materials 27
  • 28. 28
  • 29. P I E D M O N T • Piedmont Plateau- stretches from Alabama to New Jersey (includes NC) • ROCKS: metamorphic, igneous rocks • landscape worn down to hills • some isolated hard rock outcroppings remain- monadnocks- Pilot Mountain, Uwharries • Carolina Slate Belt- evidence of ancient rift zone • RESOURCES Mining: gneiss, schist, lithium, clay, sand, gravel, building stone, gold 29
  • 31. C O A S T A L P L A I N largest region • During Mesozoic era, the coastal plain was a wide sloping region well above sea level • loose soil eroded & deposited at the ocean forming beaches • During Cenozoic era, ocean covered then receded across the NC Coastal Plain region repeatedly; made terraces • RESOURCES: sand- used for glass-making Mining: clay, limestone, phosphates 31
  • 32. 32
  • 33. 33
  • 34. T h e F A L L L I N E • Fall Line: line of erosion between the Piedmont and Coastal Plain regions; hard rocks sink into softer, eastern rocks • in rivers this creates natural falls & rapids; (places to port) • influenced NC transportation, settlement, population distribution, and economic development • today, scientists look at fall lines to determine pollution effects on either side of the line 34
  • 35. Fall Line Population Centers: Tar River: Tarboro, Greenville, Rocky Mount Neuse River: Kinston, Smithfield, Goldsboro Roanoke River: Weldon Eno River: Hillsborough Alamance Creek: Alamance Fall Line parallels I-95 N/S 35
  • 36. 36 Great Falls, Potomac River: hard metamorphic Piedmont Rock
  • 37. O U T E R B A N K S • chain of barrier islands 175 miles long; • sounds separate mainland from the Outer banks: 30 miles • Pamlico Sound- largest NC sound • Albemarle Sound- 2nd largest • topography constantly changing due to erosion & deposition: beaches widen & narrow; inlets close & open up • RESOURCES: drill exploration for oil on the East Coast currently (2018) buffer the islands by 50 miles 37
  • 38. 38
  • 39. 39 Beach-Waves continually move sand on coastline Shorelines influenced by: • waves • tides • surface currents crest crest wavelength wave break Wave “feels” the bottom (slows down)
  • 40. 40 Headland- regions that project into the ocean: EROSION Bay- indentations in the shoreline DEPOSITION Bathymetry - contour of ocean floor HEADLAND BAY
  • 41. 41 Longshore current ocean current that moves parallel to shore. Creates: • beach drift (zig-zag pattern) • spits
  • 42. 42 Spit • Sand deposit connected to land, extends into water Tombolo • Spit with a hook-like end These features can form: Barrier Islands • Long linear Islands of sand that are deposited by waves parallel to shore; few km wide • First line of defense during powerful storms
  • 43. 43
  • 44. 44
  • 45. 45
  • 46. 46 Lighthouses- Used to navigate ships in the dark to warn them of the shallow waters & to indicate shoreline
  • 47. Groin (groyne) • Man-made, rigid hydraulic structure built along an ocean shore • Slows down the longshore current, dropping sand & building up shoreline 47
  • 48. 48
  • 49. 49 NC Geology LAB 1. Video 2. Labsheet: • Minerals of NC • NC Geology 3. Resources Page
  • 50. 50
  • 53. 53
  • 55. 55
  • 56. 56