Study of plate tectonics of the earth, or plate movement, Jahangir Alam
a) Wegener’s Evidence (Continental Drift)
b) History of Plate Tectonics
c) Breakup and Appearence of Pangea
WHAT IS A PLATE?
Major continental and oceanic plates include:
Types of Earth’s Crust:
Plate tectonics (from the Late Latin tectonicus) is a scientific theory which describes the large scale motions of Earth's lithosphere.
THE DYNAMIC EARTH:
The earth is a dynamic planet, continuously changing both externally and internally. The earth’s surface is constantly being changed by endo-genetic processes resulting in volcanism and tectonism, and exogenetic processes such as erosion and deposition. These processes have been active throughout geological history. The processes that change the surface feature are normally very slow (erosion and deposition) except some catastrophic changes that occur instantaneously as in the case of volcanism or earthquakes. The interior of the earth is also in motion. Deeper inside the earth, the liquid core probably flows at a geologically rapid rate of a few tenths of mm/s. Several hypotheses attempted to explain the dynamism of the earth.
+ Horizontal movement hypothesis
+ Continental drift, displacement hypothesis
Development of the plate tectonic theory.
Plate tectonic theory arose out of the hypothesis of continental drift proposed by Alfred Wegener in 1912. He suggested that the present continents once formed a single land mass that drifted apart, thus releasing the continents from the Earth's core and likening them to "icebergs" of low density granite floating on a sea of denser basalt.
Seafloor Spreading
The first evidence that the lithospheric plates did move came with the discovery of variable magnetic field direction in rocks of differing ages.
Plate Tectonics is the driving force of geologic structures th.docxrandymartin91030
Plate Tectonics is the driving force of geologic structures that shape the world that we live in. The
first indication that continents might have been linked physically took place as soon as there was
mapping. It was known by the sixteenth and seventeenth century that the continents fitted together like
pieces of a puzzle. This and other proofs listed below lead to the concept of continental drift, that the
large continents had once been linked together. The scale movements of continents across the across
the surface of the planet was mind boggling.
By the close of the nineteenth century the geologist Edward Suess postulated that the southern
continents were joined together. This was from evidence seen by fossil animal distribution. Ancient life
forms have ranges just as modern animals. Tigers are found in India and Siberia, not in North America.
These ancient animals couldn’t get from South America to Africa, from Antarctica to Australia to India.
There were rock layers both sedimentary and igneous that were continuous on all of the five continents.
He christened this large continent Gondwanaland.
In 1915 Alfred Wegener wrote a book on continental drift. He proposed another super continent
called Pangaea. This continent included all of the modern continents. His mechanism for the movement
of the continents was that the continents moved through ocean crust, drifting until they joined then
breaking apart again. Wegener and others argued for their evidence pointing out rock similarities
type, similarities in rock trends and ages using all of the information gathered from Steno's laws and
fossil assemblages. They also showed that certain distant continents had similar plants and animals that
entered a different evolutionary path after the continents separated. An example of this is the fresh
water fish the Arowana found in both South America and Australia. Another example of this is the large
amount of marsupial
fossils found in South
America and Australia.
Placental mammals
were the dominant
mammalian life forms
in Eurasia, North
America and Africa.
Only in South America
and Australia were
marsupial fossils
dominated. It wasn't
until 3 million years ago
North and South
America joined
allowing placental
mammals to gain
dominance in South America. Despite this evidence Wegener and his followers mechanism for
continental movement was badly flawed. They proposed that the tidal forces from the Sun and Moon
like the tides in the ocean. This force is much too weak to move a continent so the theory was rejected.
Fossil plants and animal distribution on southern continents
In 1928 a geologist Arthur Holmes proposed the convection currents split the continents and that
these currents were in the mantel. Remember the knowledge of a mantel was already known at this
time. Ironically this was a mechanism had been proposed by Benjamin Franklin in 1782. Many
geologi.
Study of plate tectonics of the earth, or plate movement, Jahangir Alam
a) Wegener’s Evidence (Continental Drift)
b) History of Plate Tectonics
c) Breakup and Appearence of Pangea
WHAT IS A PLATE?
Major continental and oceanic plates include:
Types of Earth’s Crust:
Plate tectonics (from the Late Latin tectonicus) is a scientific theory which describes the large scale motions of Earth's lithosphere.
THE DYNAMIC EARTH:
The earth is a dynamic planet, continuously changing both externally and internally. The earth’s surface is constantly being changed by endo-genetic processes resulting in volcanism and tectonism, and exogenetic processes such as erosion and deposition. These processes have been active throughout geological history. The processes that change the surface feature are normally very slow (erosion and deposition) except some catastrophic changes that occur instantaneously as in the case of volcanism or earthquakes. The interior of the earth is also in motion. Deeper inside the earth, the liquid core probably flows at a geologically rapid rate of a few tenths of mm/s. Several hypotheses attempted to explain the dynamism of the earth.
+ Horizontal movement hypothesis
+ Continental drift, displacement hypothesis
Development of the plate tectonic theory.
Plate tectonic theory arose out of the hypothesis of continental drift proposed by Alfred Wegener in 1912. He suggested that the present continents once formed a single land mass that drifted apart, thus releasing the continents from the Earth's core and likening them to "icebergs" of low density granite floating on a sea of denser basalt.
Seafloor Spreading
The first evidence that the lithospheric plates did move came with the discovery of variable magnetic field direction in rocks of differing ages.
Plate Tectonics is the driving force of geologic structures th.docxrandymartin91030
Plate Tectonics is the driving force of geologic structures that shape the world that we live in. The
first indication that continents might have been linked physically took place as soon as there was
mapping. It was known by the sixteenth and seventeenth century that the continents fitted together like
pieces of a puzzle. This and other proofs listed below lead to the concept of continental drift, that the
large continents had once been linked together. The scale movements of continents across the across
the surface of the planet was mind boggling.
By the close of the nineteenth century the geologist Edward Suess postulated that the southern
continents were joined together. This was from evidence seen by fossil animal distribution. Ancient life
forms have ranges just as modern animals. Tigers are found in India and Siberia, not in North America.
These ancient animals couldn’t get from South America to Africa, from Antarctica to Australia to India.
There were rock layers both sedimentary and igneous that were continuous on all of the five continents.
He christened this large continent Gondwanaland.
In 1915 Alfred Wegener wrote a book on continental drift. He proposed another super continent
called Pangaea. This continent included all of the modern continents. His mechanism for the movement
of the continents was that the continents moved through ocean crust, drifting until they joined then
breaking apart again. Wegener and others argued for their evidence pointing out rock similarities
type, similarities in rock trends and ages using all of the information gathered from Steno's laws and
fossil assemblages. They also showed that certain distant continents had similar plants and animals that
entered a different evolutionary path after the continents separated. An example of this is the fresh
water fish the Arowana found in both South America and Australia. Another example of this is the large
amount of marsupial
fossils found in South
America and Australia.
Placental mammals
were the dominant
mammalian life forms
in Eurasia, North
America and Africa.
Only in South America
and Australia were
marsupial fossils
dominated. It wasn't
until 3 million years ago
North and South
America joined
allowing placental
mammals to gain
dominance in South America. Despite this evidence Wegener and his followers mechanism for
continental movement was badly flawed. They proposed that the tidal forces from the Sun and Moon
like the tides in the ocean. This force is much too weak to move a continent so the theory was rejected.
Fossil plants and animal distribution on southern continents
In 1928 a geologist Arthur Holmes proposed the convection currents split the continents and that
these currents were in the mantel. Remember the knowledge of a mantel was already known at this
time. Ironically this was a mechanism had been proposed by Benjamin Franklin in 1782. Many
geologi.
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.
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Prepare a presentation or a paper using research, basic comparative analysis, data organization and application of economic information. You will make an informed assessment of an economic climate outside of the United States to accomplish an entertainment industry objective.
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Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
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2. * In 1910,Alfred Wegener
developed the hypothesis that all
the continents had been joined
together in a single land mass and
have drifted apart.
*The idea that the
continents are slowly drifting
apart is known as continental
drift.
* He published his
evidence in a book called origin of
continents in 1915.
3. Evidence From Landforms
* Wegener pieced together maps that showed mountain ranges that matched
up in South Africa and South America.
* European coal mines matched up with coal mines in North America.
Evidence From Fossils
*A fossil is a trace of an organism that has been
preserved in rock.
*Fossil for Mesosaurus and Lystrosaurus were
found in places now separated by oceans .
*Neither reptile could have swum long distances
across salt water.
4. Evidence From Climate
*Spitsbergen is an island in the Artic Ocean north of Norway.
*The island is ice-covered with harsh polar climates.
*Fossil of tropical plants were found on this island . When these plants lived
300 million years ago , the island must have had a warm and mild climate.
*Wegener concluded that the island must have been located near the equator.
*There is evidence that continental glaciers once covered South Africa.
*The climate of South Africa today is too mild to have sustained continental
glaciers.
5. Explanations
*Wegener also attempted to explain how the drift took place and
offer a new explanation for how mountains form.
*He thought that when the drifting continents collide , their
edges fold or crumble.
*The folding continents slowly push up huge chunks of rock to
form mountains.
6. Scientists Reject Wegener’s Hypothesis
*What forced or pulled the continents apart?
*Geologists would have to reject their own theories of how mountains
form.
*Geologists in the early 1900 thought that the earth was cooling and
shrinking.
*According to this idea, the crust would wrinkle all over the earth.
*Mountains are formed in narrow bands along the edges of all continents.
*Wegener’s theory was rejected until in the 1950’s when new evidence
about
the Earth’s structure caused scientists to reconsider the hypothesis.
7.
8. * The Wilson cycle is a model that
describes the opening and closing of ocean
basins and the subduction and divergence
of tectonic plates during the assembly and
disassembly of supercontinents.
* A classic example of the Wilson
cycle is the opening and closing of the
Atlantic.
9. ●The earliest stage , called the embryonic stage , involves uplift and
crustal extension of continental areas with the formation of rift
valleys(e.g. the East African Rift System).
►This satellite view
(this photo, looking south
from the Nile Delta)show the
young ocean basin of the Red
sea. The oldest sea floor
rocks in the Red Sea are
about five million years old ,
indicating that the Red Sea
began to form at that time.
10. ●The youngest stage involves the evolution of rift valleys into spreading
centers with strips of ocean crust between the rifted continental segments.
The result is narrow , parallel–side sea , for example the Red Sea that is
opening between NE Africa and Arabia.
►This satellite
view(photo, looking south
from the Nile delta) shows the
young ocean basin of the Red
Sea . The oldest Seafloor rocks
in the Red Sea are about five
million years old, indicating
that the Red Sea began to form
at that time.
11. ● Eventually , this
expanding system becomes
unstable and , away from the
ridge , the oldest oceanic
lithosphere sinks back into the
asthenosphere , forming an
oceanic trench subduction
system with a Wadati –Benioff
zone marking the descending
plate and associated island arcs
, such as the situation in the
western Pacific Ocean , or
Andean – type Volcanism. The
onset of subduction at the
ocean boundary marks the
subduction stage of the cycle (e
.g . The Specific Ocean).
12. ●Once subduction
outpaces the formation of
new crust at the
constructive boundary , the
ocean begins to contract .
Island arc complexes ,
complete with their
inventory of sedimentary
rocks &volcanic rocks ,
collide and create young
mountain ranges around
the periphery of the ocean .
These features mark the
thermal stage of the cycle
(e.g. the Mediterranean).
13. ●The end stage occurs
once all the oceanic crust between
the continental masses has
subducted , and the continents
coverage along a collision zone
characterised by an active fold
mountain belt, such as the
Himalayas. Finally the plate
boundary becomes inactive , but
the site of the join , or suture,
between the two continental
masses is a zone of weakness in
the lithosphere that has the
potential to become the site of a
new rift and so the cycle
continues.
16. Sonar
Sonar: A device that determines the
distance of an object under water by recording
echoes of sound waves.
The sonar is used to map the ocean floor
●Sonar bounces sound waves off underwater objects and then
records the echoes of these sound waves.
●The time it takes for the echo to arrive indicates the distance
to the object.
17. Evidence for Sea-Floor Spreading
►In the 1960s, Harry Hess examined maps of
the mid ocean ridge. He proposed that the ocean
floors move like conveyor belts, carrying the
continents with them.
19. What evidence did scientists find
for sea-floor spreading in the 1960s?
• Evidence from molten material
• Evidence from magnetic stripes
• Evidence from drilling samples
20. Evidence From Molten Material
• Alvin’s crew found strange rocks shaped like pillows or like
toothpaste squeezed from a tube.
• Such rocks can form only when molten material hardens quickly
after erupting under water.
• The presence of these rocks showed that molten material has
erupted again and again from cracks along the central valley of
the mid-ocean ridge.
21. Evidence From Magnetic Stripes
●Scientists discovered that the rock
that makes up the ocean floor lies in a
pattern of magnetized “stripes”
780,000 years ago, magnetic poles
reversed themselves.
● If they reversed today, the needle
in a compass would point south instead
of north.
●The rock in the ocean is made of
iron, which began as molten material.
22. Evidence From Drilling Samples
• When scientists sampled the rocks, they found that the
further away from the ridge the rocks were the older they
were.
• The younger rocks were always in the center of the ridges.
24. Deep-Ocean Trenches
● A deep valley along the ocean floor
through which oceanic crust slowly sinks
towards the mantle.
• Subduction: The process by which oceanic
crust sinks through a deep-ocean trench and
back into the mantle; a convergent plate
boundary.
26. Subduction in the Pacific Ocean
●Subduction in the Pacific Ocean is occurring at a greater rate
than sea-floor is expanding.
●This is caused by the large amount of trenches.
Subduction in the Atlantic
●The Atlantic Ocean is expanding at a greater rate than
subducting.
●This is because of the low number of trenches in the Atlantic.
●Over time the entire ocean gets larger and pushes against the
continents.