Lecture 3: Plate Tectonics Flashcards

(57 cards)

1
Q

1858: Snider – existence of a great region of *
1890: Edward Suess – *
1915: Alfred Wegener – * {Challenge: not able to provide the mechanism on how continents drifted apart}

A

dry land before the Great Flood
breakup of supercontinent; Gondwanaland
Continental drift

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2
Q
  • – existence of a great region of dry land before the Great Flood
  • – breakup of supercontinent; Gondwanaland
  • – Continental drift
A

1858: Snider
1890: Edward Suess
1915: Alfred Wegener

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3
Q

Challenge for continental drift

A

{Challenge: not able to provide the mechanism on how continents drifted apart}

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4
Q

All lands

A

Pangaea

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5
Q

All water

A

Panthalassa

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6
Q

Pangaea Breakup:
Laurasia {}
Gondwanaland {
}

A

(North America, Europe, Asia)

South America, Africa, India, Australia, Antarctica

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7
Q

Evidence for Continental drift

A
  1. Global geography
  2. Rock sequences
  3. Fossil
  4. Paleoclimate
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8
Q

Clue from global geography

A

Continental fit

Coastlines of Africa + South America

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9
Q

{Challenge: coastlines are constantly modified by erosion and deposition}
What did Edward Buller use?

A

– used continental shelf

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10
Q

Clues from Rock Sequences

A
Mountain Ranges
Appalachian Mountains (N America), 
British Isles, Caledonian Mountains (Scandinavia)
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11
Q

remains, trace, imprints of organisms that have been preserved in the Earth’s crust for 10,000 years +

A

Fossils

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12
Q

Fossil Distribution

A
  1. Mesosaurus – aquatic reptile; eastern South America and South Western Africa
  2. Lystrosaurus – strictly land-dwelling reptile; (Africa, Antarctica, Inda)
  3. Glossopteris “fossil seed fern” – too large to be carried by wind (Africa, Australia, India, South America)
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13
Q

aquatic reptile; eastern South America and South Western Africa

A

Mesosaurus

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14
Q

strictly land-dwelling reptile; (Africa, Antarctica, Inda)

A

Lystrosaurus

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15
Q

too large to be carried by wind (Africa, Australia, India, South America)

A

Glossopteris “fossil seed fern”

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16
Q

Glacial deposits – SA. Africa, India, Australia {tropical countries = rocks related to glaciers}; Coal fields in the northern hemisphere
Southern continents are joined together and located near the South Pole (Antarctica, Arctic}

A

Paleoclimate

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17
Q

Glacial deposits in

A

SA. Africa, India, Australia

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18
Q

Proponent of seafloor spreading

A

Harry Hess

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19
Q

Place of continuous generation of oceanic crust;

A

Mid-oceanic ridge:

ridge crest

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20
Q

7 major plates

A
African Plate
Indo-Australian Plate
Antarctic Plate
Eurasian Plate
North American Plate
Pacific Plate
South American Plate
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21
Q

MINOR PLATES

A
Somali Plate · Nazca Plate
Philippine Sea Plate · Arabian Plate
Caribbean Plate
· Cocos Plate
Caroline Plate · Scotia Plate
Burma Plate · New Hebrides Plate
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22
Q

Elaborate Plate Tectonics:

A

Continental drift + seafloor spreading

*Earth is composed of lithospheric plates

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23
Q

Further Evidence of Plate Tectonics

A
  1. Hotspots
  2. Paleomagnetism
  3. Seismic Activity
24
Q

area of high temperature

*Examples: Hawaii, Emperor Seamount chain

25
Hawaii, Emperor Seamount chain | * interacts with *
*Pacific Plate interacts with Eurasia
26
form magnetic stripes depending on Earth’s polarity. Record magnetic mineral; generate oceanic lithosphere.
Paleomagnetism
27
– temperature at which a mineral’s magnetism is lost
Curie point
28
Curie point of Magnetite
585 C
29
* deep earthquakes --> trenches | * shallow earthquakes --> boundaries of plate
Seismic Activity
30
Divergent plate boundary | centers, margin, where?
{Spreading centers} *Constructive margin Mid-oceanic ridge
31
Process involving divergent plate boundary
*Magma upwelling --> Rifting Event --> produce body of water
32
Convergent plate boundary | margin, where?
Destructive margin * subduction zones – trenches * orogenic belts – mountain
33
O-C Convergence Float: Sink: Product:
Float: C Sink: O Product: Continental volcanic arc, trench
34
O-O Convergence Sink: Product:
Sink: Denser, older, faster Product: Island Arcs
35
C-C Convergence | Product:
Product: Mountains
36
Collision of * to * forming the Himalayas | What type of convergent boundary?
India, Eurasia | C-C
37
Transform | Define, Margin, Example
Two plates slide past each other Conservative margin San Andreas Fault; East Pacific Rise
38
Driving mechanism of Plate Tectonics
Plate-Mantle Convection, | Slab pull and ridge push
39
* is the underlying driving force for plate movement | * models
Convective flow (Plate-Mantle Convection) TWO LAYER MANTLE CONVECTION MODEL WHOLE MANTLE CONVECTION MODEL
40
Results from the sinking of a cold, dense slab of lithosphere
Slab pull
41
Gravity driven force that results from the elevated position of the ridge where
Ridge push | oceanic ridge
42
Philippine Tectonics | seismically active island arc origin
1. Philippine Mobile Belt
43
aseismic continental origin
2. Palawan Microcontinental Block
44
Oceanic-Oceanic Convergence | West and East
``` {West} 1. Manila Trench 2. Negros Trench 3. Sulu Trench 4. Cotobato Trench {East} 1. East Luzon Trough 2. Philippine Trench ```
45
Marginal Basins
1. West Philippine Sea 2. Sulu Sea 3. Celebes Sea 4. Philippine Sea
46
Oceanic Bathymetric Highs (emerged, elevated sea floor)
1. Scarborough Seamounts | 2. Philippine Rise
47
Another distinct feature of Philippine Tectonics
Philippine Fault Zone
48
The concept of a floating lithosphere in gravitational equilibrium with the Earth’s asthenosphere such that the tectonic plates "float" at an elevation which depends on their thickness and density.
Isostasy
49
Isostasy is the concept of a * in gravitational * with the Earth’s * such that the tectonic plates "*" at an elevation which depends on their thickness and density.
floating lithosphere, equilibrium, asthenosphere | float
50
Isostasy is the concept of a floating lithosphere in gravitational equilibrium with the Earth’s asthenosphere such that the tectonic plates "float" at an elevation which depends on their *
thickness and density.
51
Mountains have “roots” which extend down into the mantle. Thus, elevation is proportional to the depth of the underlying “root”.
Airy-Heiskanen Model
52
Elevation is inversely proportional to density. Thus, the higher the mountain, the lower is its density; that is, light rocks “float” higher.
Pratt-Hayford Model
53
the lithosphere acts as an elastic plate and its inherent rigidity distributes local topographic loads over a broad region by bending.
Vening Meinesz/Flexural Model
54
Height is proportional to depth
Airy-Heiskanen
55
Elevation is inversely proportional to density
Pratt-Hayford
56
Weight of the load bends or flexes the lithosphere/asthenosphere
Vening Meinesz/Felxural Model
57
concept that explains a floating crust in a gravitational balance
Isostasy