plate tectonics objectives learn the historical development of the plate tectonics theory learn the...
TRANSCRIPT
Plate Tectonics
Objectives
• Learn the historical development of the Plate tectonics theory
• Learn the plate tectonics theory as their preliminary step of learning landforms
• Raise interests about the earth
• Increase the awareness of the ever-changing Earth
Lesson Structure
1.The chemical and physical layers of the Earth
2.Historical development of the plate tectonic theory
3.The location and types of plate boundaries
4.Types of plate motion
Introduction
• Plate tectonics is a relatively new theory.
• It has revolutionized the way geologists
think about the Earth.
• The surface if the Earth is broken into large
plates.
• The edges if these plates, where they move
against each other, are sites of intense
geologic activity, such as earthquakes,
volcanoes, and mountain building.
• Plate tectonics is a combination of two
earlier ideas, continental drift and sea-floor
spreading.
Layers of the Earth
• Three chemical
layers: the core, the mantle and
the crust.Core
Upper mantle
Crust
Lower mantle
The core• divided into two layers: a solid inner core
and a liquid outer core.
The Mantle• middle part of the earth
• made of minerals rich in the elements iron, magnesium, silicon and oxygen.
The Crust• rich in elements oxygen and silicon with
lesser amounts of aluminum, iron, magnesium, calcium, potassium and sodium.
• Two types of crust: oceanic crust and continental crust
• Oceanic crust is made up of relatively dense rock called basalt
• Continental crust is made of lower density rocks, such as andesite and granite.
• The outermost layers
of the earth:
lithosphere and
asthenosphere.
• The lithosphere is
the “plate” of the
plate tectonic theory
• The asthenosphere is part of the mantle that flows, a characteristic called plastic behaviour.
• The flow of the asthenosphere is part of mantle convection, which plays an important role in moving lithospheric plates.
Time for a short quiz!
1.What are the three major layers of the Earth?
2.What are the two outermost layers of the Earth?
Continental Drift
• Wegener showed the present-day continents were once part of a single supercontinent called Panagea in 1912
Evidence for Continental Drift
• Fit of the continents
• distribution of fossils
• similar sequence of rocks at numerous locations
• ancient climates
• apparent wandering of the Earth’s polar regions
Continental Drift - Fossils
Continental Drifts - Fossils• Fossils of the same species found on the
several different continent
• e.g.: Glossopteris - found on the continents of South America, Africa, India and Australia
• if the continents are reassembled into Pangaea Glossopteris can be accounted for over a smaller contiguous geographic area
Continental Drift - Rock Sequences
• Rocks sequences in South America, Africa, India, Antarctica, Australia show similarities
– bottom - tillite (glacial deposit)
– middle - sandstone, shale and coal
– upper - basic lava flows
• glossopteris fossils are bottom and middle layers
Continental Drift - Rock Sequences
Basaltlava flows
sandstoneshalecoal
glacialtill
Glossopterisfossils
Continental Drift Glaciation
• Proposed by Wegener
• South America, Africa, India and Australia were covered by glaciers nowadays.
Problem:
The climate of these areas nowadays are warm which the evidence of glacial action cannot be found
These continents were adjacent to each other during glacial event
Evidence of Glaciation
• The distribution of specific rocktypes:
e.g glacial till and striations are shared among these polar, desert and tropical areas
• The distribution of climates zones:
the poles reminded fixed and that the continents changed their position relative to the poles
Problems with Wegener’s Model
• Lack of an adequate mechanism for moving the continents
Hess’s Sea-Floor Spreading
• Heat trapped in the earth caused convention
currents
• The current would rise and fall beneath continents
• Ocean Floor moved laterally away from the ridge and plunged into the oceanic trench along the continental margin
• Trench: steep-walled valley on the sea floor adjacent to a continental margin
lithosphere
Oceanic lithosphere
asthenosphere
trench
Volcanic (island) arc
Testing the Model
• Lava erupted at
different times along
the rift at the crest of
the mid-ocean ridges
preserved different
magnetic anomalies
Clear Pictures to Show…..
Positive magnetic anomaly
Negative magneticanomaly
Time for you to think…..
• If new oceanic lithosphere is created at mid-ocean ridges, where does it go?
Subduction
• Convention cell in the mantle help carry away from the ridge
• The lithosphere arrives at the continent and subducted into the asthenosphere
• Oceanic lithosphere is created at mid-ocean ridges and consumed at subduction at subduction zones
A picture to help you understand
Volcanic Eruption
• Natural Hazard
Feel the power of nature
by watching this short
movie yourself!!!
Birth of Plate Tectonics
• Firstly introduced by Tuzo Wilson (1965)
• Jason Morgan proposed the Earth’s surface consists of 12 rigid plates
• followed by the actual orientation and the location of the plates
• widely accepted by geologists
Plate tectonic theory - Why?
• According to the locations of frequent earthquakes and volcanic activity
• forming a belt that circle the Earth
• e.g. earthquake belt: mid-Atlantic belt, east Pacific ridges
• e.g.: volcanic activity belt: Pacific Ocean “Ring of Fire”
Location of Plate Boundaries
Location of Plates
EurasianPlate
Arabian Plate
Philippine Plate
AfricanPlate
Antarctica Plate
Juan de Fuca Plate
Pacific Plate
Cocos Plate
NazcaPlate
South American Plate
CarribeanPlate
North American Plate
Australian-Indian Plate
Structure of the plates
Continental crustOceanic crust
Rigid upper mantle
Asthenosphere
Lithosphere
Types of Plate Motion
The ways that plates interact depends:
• relative motion
• nature of the plates (continental or oceanic plates
3 types of boundary divergent, convergent and transform plate
boundary
Divergent Plate Boundary
Convergent Plate Boundary
Transform Plate Boundary
Produced by
• Hazel Lam Yeuk Wing 98560141
• Ricky Lau Chun Kit 98718233
• Gigi To Wai Chi 98658333