INTERNAL DYNAMICS OF

THE EARTH

Studying our planet SEISMIC WAVES

Internal Seismic Waves

Primary 6-10 Kmh Longitudinal movement

Secundary 4-7 Kmh Vertical They can be transmitted only in solids

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files385B15Dswf

Studying our planet SEISMIC WAVES

Internal Seismic Waves

Primary 6-10 Kmh Longitudinal movement

Secundary 4-7 Kmh Vertical They can be transmitted only in solids

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files385B15Dswf

Internal Seismic Waves

Primary 6-10 Kmh Longitudinal movement

Secundary 4-7 Kmh Vertical They can be transmitted only in solids

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files385B15Dswf

Secundary 4-7 Kmh Vertical They can be transmitted only in solids

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files385B15Dswf

Changes in Seismic Wavesrsquo Speed

Seismic Discontinuities

Crust (70 Km) Less dense materials

Mantle (2900 Km) Denser rocks Upper Lower

Core (6378 Km)

Made up of iron Outer Inner

Compositional Layers

Physical Layers Considering their mechanical behaviour bull Lithosphere Solid and rigid bull Asthenosphere Mostly molten and ductile bull Lower Mantle bull Core

It has a double cause Residual heat from its formation Heat released during radiactive desintegrations

in the core As a result we obtein that there is a rate of change of temperature with depth 3ordmC 100m (Geothermal Gradient)

The Internal Heat of The Earth

CONTINENTAL DRIFT THEORY

During the 19th and 20th centuryhellip

hellipthere was controversy among scientists about the geological history of the continents Some believed their position was fixed while others proposed that they had move great distances over long periods of time Alfred Wegener was the first to collect evidences to demonstrate continents had previously been joined In 1914 he proposed his theory about the ldquoContinental Driftrdquo

250 MILLIONS OF YEARS AGOhelliphellip

PANGAEA

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Seismic Discontinuities

Crust (70 Km) Less dense materials

Mantle (2900 Km) Denser rocks Upper Lower

Core (6378 Km)

Made up of iron Outer Inner

Compositional Layers

Physical Layers Considering their mechanical behaviour bull Lithosphere Solid and rigid bull Asthenosphere Mostly molten and ductile bull Lower Mantle bull Core

It has a double cause Residual heat from its formation Heat released during radiactive desintegrations

in the core As a result we obtein that there is a rate of change of temperature with depth 3ordmC 100m (Geothermal Gradient)

The Internal Heat of The Earth

CONTINENTAL DRIFT THEORY

During the 19th and 20th centuryhellip

hellipthere was controversy among scientists about the geological history of the continents Some believed their position was fixed while others proposed that they had move great distances over long periods of time Alfred Wegener was the first to collect evidences to demonstrate continents had previously been joined In 1914 he proposed his theory about the ldquoContinental Driftrdquo

250 MILLIONS OF YEARS AGOhelliphellip

PANGAEA

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Crust (70 Km) Less dense materials

Mantle (2900 Km) Denser rocks Upper Lower

Core (6378 Km)

Made up of iron Outer Inner

Compositional Layers

Physical Layers Considering their mechanical behaviour bull Lithosphere Solid and rigid bull Asthenosphere Mostly molten and ductile bull Lower Mantle bull Core

It has a double cause Residual heat from its formation Heat released during radiactive desintegrations

in the core As a result we obtein that there is a rate of change of temperature with depth 3ordmC 100m (Geothermal Gradient)

The Internal Heat of The Earth

CONTINENTAL DRIFT THEORY

During the 19th and 20th centuryhellip

hellipthere was controversy among scientists about the geological history of the continents Some believed their position was fixed while others proposed that they had move great distances over long periods of time Alfred Wegener was the first to collect evidences to demonstrate continents had previously been joined In 1914 he proposed his theory about the ldquoContinental Driftrdquo

250 MILLIONS OF YEARS AGOhelliphellip

PANGAEA

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Physical Layers Considering their mechanical behaviour bull Lithosphere Solid and rigid bull Asthenosphere Mostly molten and ductile bull Lower Mantle bull Core

It has a double cause Residual heat from its formation Heat released during radiactive desintegrations

in the core As a result we obtein that there is a rate of change of temperature with depth 3ordmC 100m (Geothermal Gradient)

The Internal Heat of The Earth

CONTINENTAL DRIFT THEORY

During the 19th and 20th centuryhellip

hellipthere was controversy among scientists about the geological history of the continents Some believed their position was fixed while others proposed that they had move great distances over long periods of time Alfred Wegener was the first to collect evidences to demonstrate continents had previously been joined In 1914 he proposed his theory about the ldquoContinental Driftrdquo

250 MILLIONS OF YEARS AGOhelliphellip

PANGAEA

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

It has a double cause Residual heat from its formation Heat released during radiactive desintegrations

in the core As a result we obtein that there is a rate of change of temperature with depth 3ordmC 100m (Geothermal Gradient)

The Internal Heat of The Earth

CONTINENTAL DRIFT THEORY

During the 19th and 20th centuryhellip

hellipthere was controversy among scientists about the geological history of the continents Some believed their position was fixed while others proposed that they had move great distances over long periods of time Alfred Wegener was the first to collect evidences to demonstrate continents had previously been joined In 1914 he proposed his theory about the ldquoContinental Driftrdquo

250 MILLIONS OF YEARS AGOhelliphellip

PANGAEA

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

CONTINENTAL DRIFT THEORY

During the 19th and 20th centuryhellip

hellipthere was controversy among scientists about the geological history of the continents Some believed their position was fixed while others proposed that they had move great distances over long periods of time Alfred Wegener was the first to collect evidences to demonstrate continents had previously been joined In 1914 he proposed his theory about the ldquoContinental Driftrdquo

250 MILLIONS OF YEARS AGOhelliphellip

PANGAEA

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

During the 19th and 20th centuryhellip

hellipthere was controversy among scientists about the geological history of the continents Some believed their position was fixed while others proposed that they had move great distances over long periods of time Alfred Wegener was the first to collect evidences to demonstrate continents had previously been joined In 1914 he proposed his theory about the ldquoContinental Driftrdquo

250 MILLIONS OF YEARS AGOhelliphellip

PANGAEA

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

250 MILLIONS OF YEARS AGOhelliphellip

PANGAEA

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Geological evidences

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Paleobiological evidences

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Paleoclimatical Evidences

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

httpwwwesobioygeoinfoAnimacionesPlateMoTimeswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

The future world +250 millions of years

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

When asked about the mechanisms which cause continents to movehellip

The Moon gravitational attraction The Earth rotation

This was a problem Wegener could not solvehellip So his theory was (wrongly) ignored

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

And he died in 1930 during an expedition in Groenland

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

WHAT WEGENER NEVER COULD EXPLAINEDhellip

The Asthenosphere and Covection Currents

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Convection Currents

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

And that is why the lithosphere moveshellip

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

THE TECTONIC PLATES

THEORY

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

LITHOSPHERIC PLATES

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Types of Lithospheric Plates

bull Continental Plates composed of continental lithosphere

bull Oceanic Plates composed of oceanic lithosphere

bull Mixed Plate composed of both oceanic and continental lithosphere

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

Convergent Boundaries Plates move apart

Divergent Boundaries Plates move together

Transform Boundaries Plates slide horizontally

Types of Tectonic Boundaries

httpwwwesobioygeoinfoAnimacionesPlateMotionswf

LIacuteMITES DIVERGENTES

LIacuteMITES DIVERGENTES OCEAacuteNICOS

httpwwwesobioygeoinfoAnimacionesSeafloorMagnetswf

LIacuteMITES DIVERGENTES OCEAacuteNICOS

httpwwwesobioygeoinfoAnimacionesSeafloorMagnetswf

httpwwwesobioygeoinfoAnimacionesSeafloorMagnetswf

Dorsales Oceaacutenicas (formacioacuten de litosfera oceaacutenica)

LIacuteMITES DIVERGENTES CONTINENTALES

Separacioacuten de las placas araacutebiga y africana que

origina una depresioacuten en la que se forman lagos y posteriormente llegaraacute a establecerse un mar

Rift Valley Apertura de nuevos mares u oceacuteanos

Se originan por la presencia de un Punto Caliente (Hot Spot) en la astenosfera

Cuando el Punto Caliente afecta a litosfera oceaacutenica el resultado son las cadenas de islas volcaacutenicas

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files555B15Dswf

LIacuteMITES CONVERGENTES

Se dan cuando las corrientes convectivas de la astenosfera

convergen en superficie y provocan el choque de las placas Si las placas que colisionan tienen distinta densidad se

produce el hundimiento de una (la maacutes densa) bajo la otra fenoacutemeno que llamamos Subduccioacuten

En caso de que ambas sean placas ligeras (continentales) no

se produce subduccioacuten sino Obduccioacuten Asiacute los fenoacutemenos que se producen y sus consecuencias son

distintos en funcioacuten del tipo de placas que colisionan

Colisioacuten de dos Placas Continentales

Se forma un Oroacutegeno (cordillera) Intracontinental

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

LIacuteMITES DIVERGENTES CONTINENTALES

Separacioacuten de las placas araacutebiga y africana que

origina una depresioacuten en la que se forman lagos y posteriormente llegaraacute a establecerse un mar

Rift Valley Apertura de nuevos mares u oceacuteanos

Se originan por la presencia de un Punto Caliente (Hot Spot) en la astenosfera

Cuando el Punto Caliente afecta a litosfera oceaacutenica el resultado son las cadenas de islas volcaacutenicas

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files555B15Dswf

LIacuteMITES CONVERGENTES

Se dan cuando las corrientes convectivas de la astenosfera

convergen en superficie y provocan el choque de las placas Si las placas que colisionan tienen distinta densidad se

produce el hundimiento de una (la maacutes densa) bajo la otra fenoacutemeno que llamamos Subduccioacuten

En caso de que ambas sean placas ligeras (continentales) no

se produce subduccioacuten sino Obduccioacuten Asiacute los fenoacutemenos que se producen y sus consecuencias son

distintos en funcioacuten del tipo de placas que colisionan

Colisioacuten de dos Placas Continentales

Se forma un Oroacutegeno (cordillera) Intracontinental

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

Separacioacuten de las placas araacutebiga y africana que

origina una depresioacuten en la que se forman lagos y posteriormente llegaraacute a establecerse un mar

Rift Valley Apertura de nuevos mares u oceacuteanos

Se originan por la presencia de un Punto Caliente (Hot Spot) en la astenosfera

Cuando el Punto Caliente afecta a litosfera oceaacutenica el resultado son las cadenas de islas volcaacutenicas

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files555B15Dswf

LIacuteMITES CONVERGENTES

Se dan cuando las corrientes convectivas de la astenosfera

convergen en superficie y provocan el choque de las placas Si las placas que colisionan tienen distinta densidad se

produce el hundimiento de una (la maacutes densa) bajo la otra fenoacutemeno que llamamos Subduccioacuten

En caso de que ambas sean placas ligeras (continentales) no

se produce subduccioacuten sino Obduccioacuten Asiacute los fenoacutemenos que se producen y sus consecuencias son

distintos en funcioacuten del tipo de placas que colisionan

Colisioacuten de dos Placas Continentales

Se forma un Oroacutegeno (cordillera) Intracontinental

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

Se originan por la presencia de un Punto Caliente (Hot Spot) en la astenosfera

Cuando el Punto Caliente afecta a litosfera oceaacutenica el resultado son las cadenas de islas volcaacutenicas

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files555B15Dswf

LIacuteMITES CONVERGENTES

Se dan cuando las corrientes convectivas de la astenosfera

convergen en superficie y provocan el choque de las placas Si las placas que colisionan tienen distinta densidad se

produce el hundimiento de una (la maacutes densa) bajo la otra fenoacutemeno que llamamos Subduccioacuten

En caso de que ambas sean placas ligeras (continentales) no

se produce subduccioacuten sino Obduccioacuten Asiacute los fenoacutemenos que se producen y sus consecuencias son

distintos en funcioacuten del tipo de placas que colisionan

Colisioacuten de dos Placas Continentales

Se forma un Oroacutegeno (cordillera) Intracontinental

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

Cuando el Punto Caliente afecta a litosfera oceaacutenica el resultado son las cadenas de islas volcaacutenicas

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files555B15Dswf

LIacuteMITES CONVERGENTES

Se dan cuando las corrientes convectivas de la astenosfera

convergen en superficie y provocan el choque de las placas Si las placas que colisionan tienen distinta densidad se

produce el hundimiento de una (la maacutes densa) bajo la otra fenoacutemeno que llamamos Subduccioacuten

En caso de que ambas sean placas ligeras (continentales) no

se produce subduccioacuten sino Obduccioacuten Asiacute los fenoacutemenos que se producen y sus consecuencias son

distintos en funcioacuten del tipo de placas que colisionan

Colisioacuten de dos Placas Continentales

Se forma un Oroacutegeno (cordillera) Intracontinental

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

LIacuteMITES CONVERGENTES

Se dan cuando las corrientes convectivas de la astenosfera

convergen en superficie y provocan el choque de las placas Si las placas que colisionan tienen distinta densidad se

produce el hundimiento de una (la maacutes densa) bajo la otra fenoacutemeno que llamamos Subduccioacuten

En caso de que ambas sean placas ligeras (continentales) no

se produce subduccioacuten sino Obduccioacuten Asiacute los fenoacutemenos que se producen y sus consecuencias son

distintos en funcioacuten del tipo de placas que colisionan

Colisioacuten de dos Placas Continentales

Se forma un Oroacutegeno (cordillera) Intracontinental

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

Se dan cuando las corrientes convectivas de la astenosfera

convergen en superficie y provocan el choque de las placas Si las placas que colisionan tienen distinta densidad se

produce el hundimiento de una (la maacutes densa) bajo la otra fenoacutemeno que llamamos Subduccioacuten

En caso de que ambas sean placas ligeras (continentales) no

se produce subduccioacuten sino Obduccioacuten Asiacute los fenoacutemenos que se producen y sus consecuencias son

distintos en funcioacuten del tipo de placas que colisionan

Colisioacuten de dos Placas Continentales

Se forma un Oroacutegeno (cordillera) Intracontinental

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

Colisioacuten de dos Placas Continentales

Se forma un Oroacutegeno (cordillera) Intracontinental

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_filessubduccion5B25Dswf

Colisioacuten de dos placas oceaacutenicas

Se forma un Arco de Islas Volcaacutenicas

httpwwwjuntadeandaluciaesaverroesmanualestectonica_animadatect_swf_files025B15Dswf

Colisioacuten de una placa continental y una oceaacutenica

Se forma una cordillera volcaacutenica costera

LIacuteMITES TRANSFORMANTES

VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL

PHENOMENA ASSOCIATED TO PLATES TECTONICS

EARTHQUAKES VULCANISM

DEFORMACIONES DE LAS ROCAS

TIPO DE LIacuteMITE

DIVERGENTE CONVERGENTE TRANSFORMANTE

TERREMOTOS SI SI SI

VULCANISMO SI SI NO

EARTHQUAKES

bull Earthquakes are sudden tremblings of the Earthrsquos crust produced by the movements of the lithospheric plates

VULCANISM

bull The danger and violence of a volcanic eruption depend mostly on the viscosity of the magma (which is related to its silca content) and on the quantity of gases it contains

bull There are different types of volcanic eruptions

DEFORMACIONES DE LAS ROCAS

bull Elaacutesticas bull Plaacutesticas plegamientos bull Fraacutegiles roturas diaclasas y fallas

PLIEGUES

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL

PHENOMENA ASSOCIATED TO PLATES TECTONICS

EARTHQUAKES VULCANISM

DEFORMACIONES DE LAS ROCAS

TIPO DE LIacuteMITE

DIVERGENTE CONVERGENTE TRANSFORMANTE

TERREMOTOS SI SI SI

VULCANISMO SI SI NO

EARTHQUAKES

bull Earthquakes are sudden tremblings of the Earthrsquos crust produced by the movements of the lithospheric plates

VULCANISM

bull The danger and violence of a volcanic eruption depend mostly on the viscosity of the magma (which is related to its silca content) and on the quantity of gases it contains

bull There are different types of volcanic eruptions

DEFORMACIONES DE LAS ROCAS

bull Elaacutesticas bull Plaacutesticas plegamientos bull Fraacutegiles roturas diaclasas y fallas

PLIEGUES

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

PHENOMENA ASSOCIATED TO PLATES TECTONICS

EARTHQUAKES VULCANISM

DEFORMACIONES DE LAS ROCAS

TIPO DE LIacuteMITE

DIVERGENTE CONVERGENTE TRANSFORMANTE

TERREMOTOS SI SI SI

VULCANISMO SI SI NO

EARTHQUAKES

bull Earthquakes are sudden tremblings of the Earthrsquos crust produced by the movements of the lithospheric plates

VULCANISM

bull The danger and violence of a volcanic eruption depend mostly on the viscosity of the magma (which is related to its silca content) and on the quantity of gases it contains

bull There are different types of volcanic eruptions

DEFORMACIONES DE LAS ROCAS

bull Elaacutesticas bull Plaacutesticas plegamientos bull Fraacutegiles roturas diaclasas y fallas

PLIEGUES

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

TIPO DE LIacuteMITE

DIVERGENTE CONVERGENTE TRANSFORMANTE

TERREMOTOS SI SI SI

VULCANISMO SI SI NO

EARTHQUAKES

bull Earthquakes are sudden tremblings of the Earthrsquos crust produced by the movements of the lithospheric plates

VULCANISM

bull The danger and violence of a volcanic eruption depend mostly on the viscosity of the magma (which is related to its silca content) and on the quantity of gases it contains

bull There are different types of volcanic eruptions

DEFORMACIONES DE LAS ROCAS

bull Elaacutesticas bull Plaacutesticas plegamientos bull Fraacutegiles roturas diaclasas y fallas

PLIEGUES

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

EARTHQUAKES

bull Earthquakes are sudden tremblings of the Earthrsquos crust produced by the movements of the lithospheric plates

VULCANISM

bull The danger and violence of a volcanic eruption depend mostly on the viscosity of the magma (which is related to its silca content) and on the quantity of gases it contains

bull There are different types of volcanic eruptions

DEFORMACIONES DE LAS ROCAS

bull Elaacutesticas bull Plaacutesticas plegamientos bull Fraacutegiles roturas diaclasas y fallas

PLIEGUES

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

VULCANISM

bull The danger and violence of a volcanic eruption depend mostly on the viscosity of the magma (which is related to its silca content) and on the quantity of gases it contains

bull There are different types of volcanic eruptions

DEFORMACIONES DE LAS ROCAS

bull Elaacutesticas bull Plaacutesticas plegamientos bull Fraacutegiles roturas diaclasas y fallas

PLIEGUES

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

DEFORMACIONES DE LAS ROCAS

bull Elaacutesticas bull Plaacutesticas plegamientos bull Fraacutegiles roturas diaclasas y fallas

PLIEGUES

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

PLIEGUES

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

Tipos de Pliegues

bull Anticlinal en el nuacutecleo se encuentran las capas maacutes antiguas

bull Sinclinal en el nuacutecleo se encuentran las capas maacutes modernas

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

Tipos seguacuten la posicioacuten del plano y los flancos

bull Recto el plano es vertical bull Inclinado el plano estaacute entre la vertical y la

horizontal bull Tumbado el plano es horizontal bull En Rodilla los flancos quedan formando 90ordm

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

DIACLASAS

bull Roturas de las rocas sin que haya desplazamiento de los fragmentos que quedan en su posicioacuten original

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

Disyuncioacuten Columnar

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

FALLAS

bull Son roturas de las rocas con desplazamiento de los bloques

bull Partes de una falla

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

Tipos de Fallas

bull Normal

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

bull Inversa

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

bull De Desgarre

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103

• INTERNAL DYNAMICS OF THE EARTH
• Studying our planet SEISMIC WAVES
• Nuacutemero de diapositiva 3
• Nuacutemero de diapositiva 4
• Nuacutemero de diapositiva 5
• Changes in Seismic Wavesrsquo Speed
• Seismic Discontinuities
• Nuacutemero de diapositiva 8
• Compositional Layers
• Physical Layers
• Nuacutemero de diapositiva 11
• The Internal Heat of The Earth
• CONTINENTAL DRIFT THEORY
• During the 19th and 20th centuryhellip
• Nuacutemero de diapositiva 15
• Nuacutemero de diapositiva 16
• Geological evidences
• Paleobiological evidences
• Nuacutemero de diapositiva 19
• Nuacutemero de diapositiva 20
• Paleoclimatical Evidences
• Nuacutemero de diapositiva 22
• Nuacutemero de diapositiva 23
• The future world +250 millions of years
• Nuacutemero de diapositiva 25
• Nuacutemero de diapositiva 26
• WHAT WEGENER NEVER COULD EXPLAINEDhellip
• Convection Currents
• And that is why the lithosphere moveshellip
• Nuacutemero de diapositiva 30
• THE TECTONIC PLATES THEORY
• LITHOSPHERIC PLATES
• Types of Lithospheric Plates
• Nuacutemero de diapositiva 34
• Types of Tectonic Boundaries
• Nuacutemero de diapositiva 36
• Nuacutemero de diapositiva 37
• Nuacutemero de diapositiva 38
• LIacuteMITES DIVERGENTES
• LIacuteMITES DIVERGENTES OCEAacuteNICOS
• Nuacutemero de diapositiva 41
• Nuacutemero de diapositiva 42
• Nuacutemero de diapositiva 43
• Nuacutemero de diapositiva 44
• Nuacutemero de diapositiva 45
• Rift Valley Apertura de nuevos mares u oceacuteanos
• Nuacutemero de diapositiva 47
• Nuacutemero de diapositiva 48
• Nuacutemero de diapositiva 49
• Nuacutemero de diapositiva 50
• Nuacutemero de diapositiva 51
• Nuacutemero de diapositiva 52
• Nuacutemero de diapositiva 53
• Nuacutemero de diapositiva 54
• Nuacutemero de diapositiva 55
• Nuacutemero de diapositiva 56
• Nuacutemero de diapositiva 57
• LIacuteMITES CONVERGENTES
• Nuacutemero de diapositiva 59
• Colisioacuten de dos Placas Continentales
• Nuacutemero de diapositiva 61
• Colisioacuten de dos placas oceaacutenicas
• Nuacutemero de diapositiva 63
• Colisioacuten de una placa continental y una oceaacutenica
• Nuacutemero de diapositiva 65
• Nuacutemero de diapositiva 66
• Nuacutemero de diapositiva 67
• Nuacutemero de diapositiva 68
• LIacuteMITES TRANSFORMANTES
• Nuacutemero de diapositiva 70
• VISIOacuteN DE CONJUNTO TECTOacuteNICA GLOBAL
• Nuacutemero de diapositiva 72
• Nuacutemero de diapositiva 73
• PHENOMENA ASSOCIATED TO PLATES TECTONICS
• Nuacutemero de diapositiva 75
• EARTHQUAKES
• VULCANISM
• Nuacutemero de diapositiva 78
• Nuacutemero de diapositiva 79
• DEFORMACIONES DE LAS ROCAS
• PLIEGUES
• Tipos de Pliegues
• Nuacutemero de diapositiva 83
• Tipos seguacuten la posicioacuten del plano y los flancos
• Nuacutemero de diapositiva 85
• Nuacutemero de diapositiva 86
• Nuacutemero de diapositiva 87
• Nuacutemero de diapositiva 88
• Nuacutemero de diapositiva 89
• Nuacutemero de diapositiva 90
• DIACLASAS
• Nuacutemero de diapositiva 92
• Nuacutemero de diapositiva 93
• Nuacutemero de diapositiva 94
• FALLAS
• Nuacutemero de diapositiva 96
• Tipos de Fallas
• Nuacutemero de diapositiva 98
• Nuacutemero de diapositiva 99
• Nuacutemero de diapositiva 100
• Nuacutemero de diapositiva 101
• Nuacutemero de diapositiva 102
• Nuacutemero de diapositiva 103