theme 3. plate tectonics theory - jurnalul lui Ştefan · theme 3. plate tectonics theory 3.1....

41
Theme 3. Plate tectonics theory 3.1. General principles 3.2. Mantle convection 3.3. Types of plate boundaries

Upload: hadang

Post on 13-Apr-2018

219 views

Category:

Documents


5 download

TRANSCRIPT

Theme 3.

Plate tectonics theory

3.1. General principles

3.2. Mantle convection

3.3. Types of plate boundaries

3.1. General principles

The lithosphere is underlain by a plastic layer of the

mantle, the asthenosphere, over which the plates

can move.

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever

The theory of plate tectonics describes:

-the movement of plates;

3.1. General principles

-the movement of plates;

-the forces acting between them.

The theory of plate tectonics explains:

-continental drift;

-volcanoes;

3.1. General principles

-volcanoes;

-earthquakes;

-the distribution of mountain chains;

-rock assemblages;

-structures on the seafloor.

3.1. General principles

Continental drift

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

Source: USGS

3.1. General principles

Source: internet

3.1. General principles

Source: USGS

3.1. General principles

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

Source: Understanding Earth –

J.Grotzinger, T.H. Jordan, F.

Press, R. Siever

3.1. General principles

Plate tectonics theory – by whom?

3.1. General principles

Plate tectonics theory – by whom?

By the close of the

nineteenth century,

Eduard Suess hadEduard Suess had

put together some of

the pieces of the

puzzle.

Source: internet

3.1. General principles

Remarkable similarity of

rocks, geologic structures,

and fossils on opposite

Plate tectonics theory – by whom?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

and fossils on opposite

sides of the Atlantic –

Alfred Wegener (1915)

3.1. General principles

Plate tectonics theory – by whom?

In the early 1960s, Harry Hess and Robert Dietz proposed that the

crust separates along the rifts in mid-ocean ridges and that new

seafloor forms by upwelling of hot new crust into these cracks.

Source: internet

3.1. General principles

Plate tectonics theory – by whom?

- by a group of geologists and other scientists.

The basic elements of the plate tectonics

theory were established by the end of 1968.

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.1. General principles

PANGAEA?

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.2. Mantle convection

3.2. Mantle convection

3.2. Mantle convection

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.2. Mantle convection

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

The general process, in which hotter material rises

and cooler material sinks, is called convection.

3.2. Mantle convection

The general process, in which hotter material rises

and cooler material sinks, is called convection.

3.2. Mantle convection

The convecting mantle and its overlying mosaic of

lithospheric plates constitute the plate tectonic system.

Source: Understanding Earth – J.Grotzinger,

T.H. Jordan, F. Press, R. Siever

3.3. Types of plate boundaries

3.3. Types of plate boundaries

Source: USGS

3.3. Types of plate boundaries

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever

3.3. Types of plate boundaries

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever

3.3. Types of plate boundaries

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever

3.3. Types of plate boundaries

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever

3.3. Types of plate boundaries

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever

3.3. Types of plate boundaries

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever

3.3. Types of plate boundaries

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever

3.3. Types of plate boundaries

Source: Understanding Earth – J.Grotzinger, T.H. Jordan, F. Press, R. Siever