Title: The Earths Interior, Continental Drift and Theory of Plate Tectonics
1The Earths Interior,Continental Drift and
Theory of Plate Tectonics
2- Formation of oceanic crust at rift zones
located in the mid-oceanic floors. Upwelling of
magma later solidifies beneath the oceans to
produce the crust
3Earths Internal structure
- 5. The Crust the rigid outer cover of the earth
stretching about 5 miles under Oceans and about
40 miles under some mountains - 6. Lithosphere comprises all materials that
form the crust and the upper mantle (rocks, soil,
etc)
4Earths Internal Structure
- The Earth is composed of rocks of different
densities. - 1. Inner Core made up of solid iron
- 2. The Outer Core liquid iron
- 3. The Mantle - a dense solid material that
makes up about 80 of earth's material - 4. Astenosphere upper part of the mantle
5Theory of Continental Drift
- The idea that the continents have originated from
a single SUPER CONTINENT was first proposed as a
scientific hypothesis in 1920-s by Alfred Wegener
- He hypothesized that a single super continent
(Pangaea - "whole land") existed on Earth about
250 million years ago. - The super continent later broke down into two
pieces - a) a northern half called Eurasia and
- b) a southern portion called Gondwanaland.
- The Continental Drift Theory did not gain
worldwide support because it could not account
for the forces that break up and move the
continents
6Continental Drift Theory
1915 Alfred Wegener proposed that landmasses
were once united called Pangaea
Pangaea later split into Laurasia Gondwanaland
7During this time, land masses have formed and
moved (continental drift)
8Theory of Plate Tectonics
- In the 1960s, the Continental drift theory was
replaced by the theory of plate tectonics. The
discovery of alternating patterns of rock
magnetism in surface rocks and sea-floor
spreading aided in the creation of the plate
tectonics theory. - Modern plate tectonic theory states that the
surface crust of the Earth is composed of many
independent segments called plates. These plates
have the ability to move horizontally by gliding
over the plastic asthenosphere .
9Continental Plates
- Plate tectonics theory explains that the
Lithosphere consists of as many as 7 huge plates
about 5 smaller plates that move as distinct
units. - The plates form the continents, islands, and the
floor of the oceans.
10Convection Currents
- Modern tectonic theory explains that crustal
movements are caused by a very slow thermal
convection currents within the earth. - Hot magma is rising from deep inside the earth
until it reaches the crust, and crustal blocks
are submerging into mantle.
11Lithosphere moves over the asthenosphere
12Types of Plate Movements -- 1
- Divergence - Plates move away from each other
(e.g. mid-Atlantic ridge, East African rift
valley) - Lateral Movement as in Transform Plate boundaries
where plates slide past one another along
strike-slip faults such as the San Andreas Fault
in California.
13Types of Plate Movements --2
- Lateral movements as in Subduction Zones where
Oceanic plates slides beneath Continental
plates (e.g. the coasts of Peru and Chile,
Eastern Philippines and Japan). These are zones
of deep ocean trenches. - Lateral plate movements can cause Faulting and
the FOLDING of the crust into mountains (e.g.
Appalachian Rockies in US, the Alps of
Europe, the Andes mountains of South America and
the Himalayas mountains of Asia.
14 Sea Floor Spreading Plate Boundaries
15Tectonic features of the world
16Divergent plate movement
- At some plate boundaries, plates are moving away
from each other because of sea-floor spreading. - An example is the mid-Atlantic Ridge between
Africa and North America
17Collision of an Oceanic plate with a Continental
plate
- Subduction is fairly slow (2-3 cm per year)
- produces large earthquakes, volcanism, mountain
ranges - Nazca plate subducted under South America plate
18Formation of Himalayas Mountains
- Formation of the Himalaya Mountains.
Compressional forces due to the collision of the
Eurasian and Indian continental plates caused
ocean sediments and continental rocks to be
pushed upward in elevation. (Source U.S.
Geological Survey).
19Collision of two Continental Plates
- When two continental plates collide, one of
the crustal plates is subducted under the other
producing a mountain range at the plate
boundaries e.g. Himalayas. - Sometimes earthquakes also occur at the plate
boundaries.
20Collision of two Oceanic Plates
- In this type of a collision, (collision of North
America and Pacific Plates (Aleutian Islands) one
of the plates is subducted under the other
creating a deep oceanic trench - The Marianas trench in the Pacific ocean is
created by the collision of the fast-moving
Pacific Plate against the slower moving
Philippine Plate. - Convergence of two oceanic plates also creates a
chain of volcanic islands called Island arcs.
21Features along continental margins
- Marginal features found at the interface of
the continents and the ocean basins