Evidence For Continental Drift. Introduction As Scientific Theories go, Plate Tectonics is a...
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Plate Tectonics Evidence For Continental Drift
Evidence For Continental Drift. Introduction As Scientific Theories go, Plate Tectonics is a relatively new scientific concept, introduced in the 1960’s
Introduction As Scientific Theories go, Plate Tectonics is a
relatively new scientific concept, introduced in the 1960s. It is
the most revolutionary idea in Earth Sciences it has changed our
notion of a generally quiet, unchanging planet (Uniformitarianism)
into the understanding that the Earth is a dynamic planet.
Slide 3
Plate Tectonics the Unifying Theory of Earth Sciences The
theory has unified the study of the Earth by drawing together many
branches of the earth sciences, from paleontology (the study of
fossils) to seismology (the study of earthquakes). It has provided
explanations to questions that scientists had speculated upon for
centuries -- such as why earthquakes and volcanic eruptions occur
in very specific areas around the world, and how and why great
mountain ranges like the Alps and Himalayas formed.
Slide 4
Look At The Globe By examining a globe, one can observe that
many of the continents seem to fit together like a puzzle: the west
African coastline seems to fit nicely into the east coast of South
America and the Caribbean sea; and a similar fit appears across the
Pacific. The fit is even more striking when the submerged
continental shelves are compared rather than the coastlines. In
1858, geographer Antonio Snider- Pellegrini made these two maps
showing his version of how the American and African continents may
once have fit together, then later separated
Slide 5
Alfred Wegener In 1912 Alfred Wegener (1880-1930) noticed that
fossil encyclopedias listed fossils that existed on opposite sides
of the ocean - he found this idea to be highly unusual. Wegener
then noticed that the continents seemed to fit together. By linking
continents together, the fossil regions would be joined together.
Wegener proposed that the continents were once joined into a single
supercontinent which he called Pangaea (meaning "all lands"). He
believed that over time the continents have drifted apart into
their current distribution. Wegener is generally regarded as the
father of the idea of Continental Drift Wegener was not only well
known for his theory of Continental Drift (Kontinentalverschiebung)
but also for his work in Meteorology. He studied polar air
circulation in Greenland which contributed to the discovery of the
Jet Stream. Wegener also collected ice drilling samples of the
Greenland Glaciers. Wegener died while working in Greenland at the
age of 50.
Slide 6
Continental Drift Wegener believed that Pangaea was intact
until the late Carboniferous period, about 300 million years ago,
when it began to break up and drift apart. Wegener's hypothesis
lacked a geological mechanism to explain how the continents could
drift across the earths surface as he proposed.
Slide 7
Background PowerPoint
http://faculty.uml.edu/Nelson_Eby/87.201/Instructor
%20pdfs/Plate%20Tectonics%20Class.pdf (University of Massachusetts
at Lowell) http://faculty.uml.edu/Nelson_Eby/87.201/Instructor
%20pdfs/Plate%20Tectonics%20Class.pdf
Slide 8
You Tube Video https://www.youtube.com/watch?v=X9_TIf2navc
(21:41 - Wegeners Evidence)
https://www.youtube.com/watch?v=X9_TIf2navc
https://www.youtube.com/watch?v=NwqX4OLJRe4 (10:42 - Continental
Drift) https://www.youtube.com/watch?v=NwqX4OLJRe4
https://www.youtube.com/watch?v=0KNqUwgqbZw (Bill Nye - 100
Greatest Discoveries - 47:00)
https://www.youtube.com/watch?v=0KNqUwgqbZw
Slide 9
Continental Drift Wegeners Hypothesis was not widely accepted
until the 1950s. The following evidence made his hypothesis more
acceptable to the Scientific community: 1) Coastline Matching 2)
Fossils collected in Africa and South America 3) Ocean Floor
Exploration 4) Patterns of Seismic Activity (Earthquakes and
Volcanoes) 5) Glaciation
Slide 10
1)Matching Coastlines Continents, especially if you include the
continental margins, fit together very clearly as seen in the globe
at right. The suggestion is that the continents were joined
together and broke apart and moved into their present positions.
More proof was needed to add strength to this hypothesis.
Geologists looked to match rock formations on continents now
separated by oceans. Similarly, paleontologists looked for similar
trends with fossil assemblages.
Slide 11
11 Continental Fit and Mountain Ranges TLTH, fig. 1.15 Major
time of mountain formation ended about 250 mya (million years ago),
before Pangaea split Appearance of same rock sequences and
mountains of the same age on continents now widely separated.
Slide 12
2)Fossil Data Fossils within specific stratigraphic sequences
were found on opposite sides of oceans. When the continents were
pieced together, the fossil sequences merged. Mesosaurus, a reptile
TLTH, fig, 1.13
Slide 13
Possible Explanations for Fossils being separated by oceans:
Possible explanations?
Slide 14
3)Ocean Floor Exploration In the 1950s and 1960s, the first
scientific exploration of the seafloor was undertaken. Among the
data collected were depth measurements (using precision depth
sounding), sea-floor sampling (and subsequent radiometric age
dating), paleomagnetic readings. Glomar Challenger
Slide 15
Harry Hess - Sea-Floor Spreading
https://www.youtube.com/watch?v=GyMLlLxbfa4&lis
t=PL8aTbGWgTg6U95JvrN-g2mCnz7QNPs9r4 (Bill Nye - 4:01)
https://www.youtube.com/watch?v=GyMLlLxbfa4&lis
t=PL8aTbGWgTg6U95JvrN-g2mCnz7QNPs9r4 Geology professor Harry Hess
acted as a naval transport captain during WWII. While travelling
the Pacific Ocean, Hess discovered that there was a mountain range
under the ocean. In 1953, Oceanographers discovered the mid-ocean
ridge. The ridge is as high as 2500 m above the sea floor.
Slide 16
Harry Hess - Sea-Floor Spreading Hess followed up by studying
the age of rocks and sediments on the ocean floor by using core
samples and sonar data. He makes the surprising discovery that the
sea floor is youngest at the mid-ocean ridges and that the crust
gets older as you move away from the ridge. He also learns that the
mid ocean ridge is a line of underwater volvcanoes where new crust
is being formed. Hess discovered that new crust is produced at the
mid ocean ridge and is pushed away from the ridge as new ocean
crust (basalt) is created. Hess discovers that the Sea Floor is
Spreading.
Slide 17
Sea Floor Spreading Hess reasoned that if: a)new crust is being
created at mid-ocean ridges b)the Earth is not increasing in size
Then crust must be destroyed somewhere else on the planet. Hess
suggests the idea of subduction zones at the margins of some
continents. Hess Sea-Floor Spreading resurrects Wegener waning
Hypothesis of Continental Drift and leads to the larger idea of
Plate Tectonics.
Slide 18
Ocean Floor Exploration Mapping of the ocean floor revealed the
presence of mid-ocean ridges and trenches. Mid-ocean ridges
constitute rift zones that form interconnected sub-sea mountain
ranges that span the globe. The Glomar Challenger was the famous
exploration craft used to sample the ocean floor.
Slide 19
Ocean Floor Exploration The following topographic features can
be found on the seafloor mid-ocean ridge, continental slope,
continental shelf, trenches, abyssal plains and volcanic
islands.
Slide 20
Ocean Floor Exploration A cross-section of an ocean does not
show a featureless topology. Exploration of the ocean floor showed
the existence of mid-ocean ridges, continental shelves and deep
trenches.
Slide 21
4)Patterns of Seismic Activity Seismic activity such as
earthquakes or volcanoes do not occur in random locations. The vast
majority of seismic activity occurs at the boundaries of plates
(large sections of oceanic and continental crust). In fact, by
plotting the location of major seismic events Trenches are deep
troughs associated with active earthquakes zones and chains of
volcanoes.
Slide 22
Location of Major Earthquakes
Slide 23
Location of Major Plates
Slide 24
Glaciation Patterns of Glaciation were matched across
continents. When continents were joined the patterns made more
sense.
New Evidence Emerges 1) Paleomagnetism 2) Magnetic Pole
Reversals 3) Magnetic Striping 4) Earthquake Mapping Still a
mechanism is required
Slide 27
1)Paleomagnetism 1) Since the Earth has a liquid iron-nickel
core, the planet generates a strong magnetic field (as seen in the
diagrams at right) 2) When igneous rocks containing a magnetic
element (iron, nickel and cobalt) cool from a liquid state, the
grains of the element will align with the magnetic field.
Slide 28
Paleomagnetism 3) As a result the direction of the magnetic
field at the time of their solidification is preserved. 4) These
rocks can be used to pinpoint the direction of magnetic north at
the time of solidification.
Slide 29
Paleomagnetism 5) Rocks that move across the globe due to
continental drifting can be traced back to their original location.
6) This allows geologists to track the movement of continents over
time. https://www.youtube.com/watch?v=uGcDed4xVD4 (Video showing
the movement of continents over the past 600 million years and 100
million years into the future).
https://www.youtube.com/watch?v=uGcDed4xVD4
Slide 30
2)Magnetic Pole Reversals
https://www.youtube.com/watch?v=BCzCmldi aWQ (2:35)
https://www.youtube.com/watch?v=BCzCmldi aWQ The direction of the
Earths magnetic poles has flipped many times in the past. We know
there have been about 170 magnetic pole reversals during the last
100 million years, and that the last major reversal was 781,000
years ago (see chart at right - black represents normal
polarity).
Slide 31
2)Magnetic Pole Reversals These shifts leave traces in rocks.
When lava cools, metal oxide particles within the rock become
frozen in the direction of the prevailing magnetic field. It is
believed that changes in the convection of the liquid outer core
cause these flips to occur (as well as changes in strength of the
Earths magnetic field) It is believed that the rate of reversals is
increasing (possibly due to the increase in the size of the solid
inner core) The layers of (iron-rich) lava show differing magnetic
pole directions.
Slide 32
3)Magnetic Striping 1) The most important application of this
property was done during Ocean Floor Mapping. 2) Magnetic detection
devices called magnetometers (developed during WWII to detect
submarines) measure the strength and direction of the magnetic
fields found in iron-bearing rocks such as basalt.
Slide 33
3)Magnetic Anomalies 3) Geologists noted a pattern of stripes
on the ocean floor of normal and reverse polarity. Most
importantly, the patterns mirrored each other on opposite sides of
a mid-ocean ridge. 4) Watch this brief YouTube video to see how
this works: https://www.youtube.com/watc h?v=YIAXiE8RedA
https://www.youtube.com/watc h?v=YIAXiE8RedA
Slide 34
3)Magnetic Anomalies 5) The magnetic striping leaves a
distinctive pattern across all oceans and can be used to date ocean
crust and sediments. 6) The oldest ocean crust is less than 250
million years old.
Slide 35
4) Earthquake and Volcano Mapping The Earths major tectonic
plates and the location of volcanoes. Note that the vast majority
are located on or near a plate boundary.
Slide 36
Earthquake Depths This depth vs distance chart (cross section)
shows the focus of earthquakes along an ocean crust-continental
crust boundary. This evidence gives the idea that slabs of ocean
crust descend underneath continental crust. Crust is subducted into
the Earths mantle.
Slide 37
Earthquake Depths The diagram shows a cross-section of the
subduction zone off Japans east coast. Ocean crust is subducted
under more ocean crust. Melting of the descending slab is
responsible for the chain of volcanoes that form the Japanese
islands. Suggest the rock type that forms these islands.
Slide 38
Putting the Evidence Together to Create a Theory
https://www.youtube.com/watch?v=X9_TIf2navc (start at 18:00)
https://www.youtube.com/watch?v=X9_TIf2navc
https://www.youtube.com/watch?v=0KNqUwgqbZw (Bill Nye - start at
15:25) https://www.youtube.com/watch?v=0KNqUwgqbZw
Slide 39
Mantle Convection Mantle Convection Video (short 0:45)
https://www.youtube.com/watch?v=p0dWF_3PYh4
https://www.youtube.com/watch?v=p0dWF_3PYh4 The mechanism that
Wegener needed to drive continental drift is the convection of the
mantle. The mantle is semi-molten and convects very slowly - this
is the reason continents drift at an average rate of 5 cm/year.
Rising mantle plumes drive sea-floor spreading and are also
responsible for mid-plate hot spots like Hawaii and
Yellowstone.
Slide 40
Sea Floor Spreading at Mid Ocean Ridges - New Crust Forms Why
is ocean crust subducted under continental crust? (Why does
continental crust float higher in the mantle)
Slide 41
Sea Floor Spreading at Mid Ocean Ridges - New Crust Forms Ocean
crust (dark blue) and continental crust (grey) sit on a semi-molten
layer called the lithosphere (brown).
https://www.youtube.com/watch?v=Kpoko_l34ZE (good video showing
mantle convection and discussing mantle layers. - 1:15)
https://www.youtube.com/watch?v=Kpoko_l34ZE
Slide 42
Mantle Hot Spots - Hawaii Some volcanism occurs in the middle
of plates. Rising mantle plumes are hot enough to punch through the
mantle and produce volcanoes that rise from the ocean floor and in
the case of Hawaiis big island, rise well above the surface.
Slide 43
Mantle Hot Spots - Hawaii These mantle plumes or hot spots
remain stationary while the oceanic plate moves over the hot spot.
As a result, the volcano loses its source of magma and becomes
extinct and is carried (westward in the case of the Hawaiian
Islands) and a new volcano forms. What type of rock do we expect to
find in Hawaii? What type of volcano do we expect?
Slide 44
Mantle Hot Spots - Hawaii The older extinct volcanoes are
eroded into smaller and smaller islands (often ringed by a lagoon)
and eventually disappear beneath the surface and are called
seamounts.
Slide 45
Mantle Hot Spots - Hawaii This oceanic map shows the Hawaiian
island chain and the Emperor seamounts that were created by the
same hot spot. The oldest seamount is 65 million years old. The
oldest Hawaiian island is 7 mya. The change in plate direction
occurred 42 mya Notice that the plate direction changed at some
point in the past.
Slide 46
Mantle Hot Spots Yellowstone happens to be hot spot located
beneath a continent. What type of rock do we expect to find at
Yellowstone? What type of volcanism? https://www.youtube.c
om/watch?v=bYv6V5EJ AKc (Great short video - Hawaiis hot spot
volcanoes - 3:05) https://www.youtube.c om/watch?v=bYv6V5EJ
AKc
Slide 47
Subduction Zones - Crust is Subducted and remelted into the
Mantle When heavier basaltic ocean crust (3.1 g/cm 3 ) is forced
beneath lighter (and thicker) granitic continental crust (3.1 g/cm
3 ), the subducting slab melts to produce volcanoes 50 - 300 km
from the plate boundary. An ocean trench is formed where the slab
begins its descent. The deepest trench (Marianas Trench) is almost
11 km deep. https://www.youtube.com/watch?v=K
8J7t3KYr9chttps://www.youtube.com/watch?v=K 8J7t3KYr9c (Model using
sand to simulate mountain growth near suduction zones - very
accurate)
Slide 48
Subduction Zones The west coasts of North and South America are
these types of subduction zones Volcanoes occur from Alaska down
the Rocky Mountains to the Andes Mountains. This whole region is at
risk from volcanoes, earthquakes and tsunamis. The Cascadia Zone
has been hit with massive tsunamis in the past. What type of rock
do we expect? What type of volcanism?
Slide 49
Subduction Zones Most of the largest earthquakes (and
subsequent tsunamis) are produced at subduction zones.
https://www.youtube.com/watch?v =f-nIb8JkFrg (Subduction zone
earthquakes - 2:50) https://www.youtube.com/watch?v =f-nIb8JkFrg
https://www.youtube.com/watch?v =Yukp0bPkQxs (45 minutes - Cascadia
Megaquake) https://www.youtube.com/watch?v =Yukp0bPkQxs
https://www.youtube.com/watch?v =j0YOXVlPUu4 (Japanese tsunami)
https://www.youtube.com/watch?v =j0YOXVlPUu4
https://www.youtube.com/watch?v =w3AdFjklR50 (Japanese tsunami -
short video) https://www.youtube.com/watch?v =w3AdFjklR50