Monday, 18 March 2013

Basic Concept of Mountains.


DEFINITION :-

A mountain may be defined as a huge landmass on the earth's surface,attending a great height above the surrounding with a series of oranges and loftly crests and peaks covered with snow.

DESCRIPTION :-

A mountain is a highland area with a series of ranges and peaks.It has many gorges and valleys.Between the high ranges,there are intermont plateaus.High mountains are regions of glacical activity.

FORMATION :-

Mountains are formed in various ways.They are formed by wrinkling up the earth,s surface.Giving away heat from its body,the earth wrinkles.As a result,compression and contraction take place and folds,fractures and faults are formed in the rock-beds which in time build up mountains and valleys.Volcanic eruption erects volcanic mountains.Erosional agents ( The sun,the rain,,the wind and the running water) wear away the soft rocks of the highlands ; the high resistant rocks are left there as erosional mountain.

An eminent German, Prof Alfred Wegner (1912) explained in his 'Continental Drift Theory ' how the mountains were formed .According to his theory,the lighter rocks-beds are in a floating state on the heavier rock-masses.In the primitive world there was a single landmass called 'Pangaea'.Natural forces broke it down into pieces ; the major pieces are know as continents.In time, they drifted apart. As they drifted away, the horizontal pressure pushed the rock-beds to form fold ; harder rock beds got fracture and faulting occurred. Thus the drifting of the continents caused the formation of the fold mountains and other landforms.

In the recent years, "Plate Tectonic Theory" has become popular. It has developed the idea on the former. This theory states that the continents and the oceanic beds consist of a series of plates; the continents plates are floating on the oceanic plates. The get motion when disturbances occur in the interior of the earth; sometimes intrusion takes place from the interior to the upper layer and the plates begin to move. As the plates move towards each other, friction sometimes occurs. It exerts pressure which forces the rock-beds to bend and thus (i) folds (ii) Faults and (iii) Eruption occur, resulting in the formation of mountains and different types of landform.

Classification of Mountain :-

Mountain can be classified into four major types, according to their mode of formation : (i) Fold mountain (ii) Block mountain (iii) Volcanic mountain and (iv) Relict mountain or Erosional mountain.

  

Basic Concept of Metamorphic Rock



DEFINITION AND FORMATION:-



 Metamorphic rock is formed by ( the change the greek word 'metamorphosis' means change of form ) in a rock from its original form by heat and by pressure beneath the surface of the earth. The igneous and sedimentary rocks undergo a great change in their physical appearance and chemical properties due to (1) Intense heat and (2) Great pressure. Thus internal changes take place within the rocks. The particles are rearranged and redistributed affecting the structure and character of the rocks. The crystal in the rocks are arranged in fine parallel layer.
Sometimes, the change is so thorough that the original characters are no longer present in the altered rock.

EXAMPLES :-


Gneiss, Marble, Quartzite, Graphite, Slate, Amphibolite etc.are the example of metamorphic rocks. Under the process of metamorphism (1) Granite changes into gneiss, (2) Basalt into Amphibolite, (3) Limestone into marble, (4) Shale into slate, (5) Sandstone into Quartzite and (6) Peat coal into graphite.



Fig : Gneiss
Fig :- Structure of Graphite 


Fig :- Structure of Graphite
Fig :- Quartizite

















Fig :- Slate

Fig :- Amphibolite











Fig :- Granite into Gneiss

Fig :- Basalt into Amphibolite












Fig :- Limestone into Marble

Fig :- Shale into Slate














METAMORPHISM :-



The greek word metamorphosis means change of form.The changes which take place in rocks due to intense heat and pressure is known as metamorphism.It is of two types : (1) Contact Metamorphism or local Metamorphism and (2) Regional Metamorphism.



CONTACT OR LOCAL METAMORPHISM :-



 When hot magma enters the fissures, it bakes the adjoining rocks in the contact zone.It produces chemical replacement and recrystallisation. As it affects by means of contact,it is know as contact metamorphism.As it also affects a small area, it is called local metamorphism.In this metamorphism,limestone is changed into marble.



REGIONAL METAMORPHISM :-



 Generally, it associates with great mountain building movements.Thus change which occurs,takes a long period and affects a large area.Hence,this is known as regional metamorphism.The pressure of the overlying rocks recrystallizes the rocks below.In this way, shale is changed into slate; and again state is changed to schist.



CHARACTERISTICS AND USES OF METAMORPHIC ROCKS :-



Metamorphic rocks are massive,completely crystalline and hard.They are resistant to erosion. They are very rich in minerals.they attract huge mining population.Since they are hard ,they are used as building and road materials.No fossil is found in metamorphic rock.when sedimentary rock undergoes changes,the fossils are destroyed by heat and pressure.





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