Tuesday, 16 June 2026

KERALA PSC / PHYSICAL GEOGRAPHY / MOVEMENTS OF THE EARTH’S CRUST / NOTES

 KERALA PSC / PHYSICAL GEOGRAPHY / MOVEMENTS OF THE EARTH’S CRUST / NOTES


KERALA PSC / PHYSICAL GEOGRAPHY / MOVEMENTS OF THE EARTH’S CRUST / NOTES

 

·       The earth movements are to two types:

Ø Vertical Movements

Ø Horizontal Movements

·       Vertical movements are responsible for a rise or a fall of a portion of the earth’s surface

·       When a part of the earth’s crust rises in relation to surrounding portions it is known as uplift or emergence

·       When the sinking of a part of the earths crust relative to surrounding portion takes place, it is called subsidence

·       The formation of continents and plateaus are also due to vertical movement and hence these are also referred to as continent building or plateau building movements

·       Horizontal movements involve compression and tension

·       These compressional or tensional forces are horizontal or tangential movements

·       These movements are also referred to as mountain building movements

·       Warping and Isostasy constitute vertical movements, while folding, faulting and continental drift constitutes horizontal movement

·       Warping is the deformation of earth’s crust which affects very large areas on the earth’s surface. It results in the formation of domes, shields and depressions

·       Isostasy is a condition of gravitational balance between the crustal segments of different thickness.

·       Folding is the process whereby the rock strata are bent into a series of arches (anticlines) and troughs (synclines) as a result of the horizontal earth movements which cause compression within the crust.

·       Faulting is the process by which the tensional earth movements under the effect of considerable pressure creates a fracture in the earth’s crust.

·       Faulting gives rise to relief features such as block mountains and rift valleys

·       Continental drift refers to the horizontal movements of the continents on a vast scale.

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KERALA PSC / PHYSICAL GEOGRAPHY / MOVEMENTS OF THE EARTH’S CRUST / NOTES


KERALA PSC / PHYSICAL GEOGRAPHY / ROCKS AND MINERALS / NOTES

 

KERALA PSC / PHYSICAL GEOGRAPHY / ROCKS AND MINERALS / NOTES



KERALA PSC / PHYSICAL GEOGRAPHY / ROCKS AND MINERALS / NOTES

 

·       Rocks and minerals mainly constitute the upper part of the earth’s crust. Minerals are natural substances having characteristics properties and more or less specific chemical compositions

·       Rocks are solid materials that make up the earth’s crust. On the basis of texture, structure and composition, rocks may be classified into igneous, sedimentary and metamorphic

·       Igneous rocks are formed by the solidification of molten magma from the interior of the earth. About 95% of the earth’s crust is made up of this type of rocks. It generally do not occur in layers. Most of them are crystalline. Eg: Granite, volcanic rocks and Basalt

·       Also called primary rocks; they are generally hard, massive, crystalline and contain no fossils

·       They are also called Parent Rocks because all the types of rocks have emerged from these rocks

·       Igneous rocks are classified into intrusive and extrusive rocks

·       Intrusive igneous rocks formed due to solidification of lava under the surface of the earth. They have content of silica and poor in metallic minerals. Also called acid lava rocks

·       If the lava has very high melting point it may get solidified at great depths. Rocks thus formed are called plutonic rocks. Granite is a common plutonic rock.

·       Extrusive igneous rocks are formed when the lava reach the surface of the earth and then solidify. It is also called basic lava rocks, eg: Rhyolite, basalt etc…

·       Rocks are formed through solidification of lava in the beds or the layers of earth crust. Some of the molten materials rising from the interior is unable to reach the surface. This material penetrates the joints and fissures in the rocks and solidifier. Here it cools in the form of vertical wall-like structures called dykes

·       Sedimentary rocks are formed from the sediments deposited on the ocean beds. They comprise only about 5% of the earth’s crust, but covers about 75% of the total land surface.

·       Sedimentary rocks are generally softer, fossils are commonly found in these rocks. These rocks are also called stratified rocks.

·       Shale is the most abundant of all sedimentary rocks which is composed of silt and clay.

·       Sandstone is a common sedimentary rock which is formed mainly of quartz particles cemented together by silica, lime or iron oxide

·       Mineral oil or petroleum is derived from organic matter trapped between the layers of sedimentary rocks.

·       Metamorphic rocks are formed when pre-existing sedimentary or igneous rock is altered as a result of changes in physical or chemical conditions. Eg: Quartzite and Marble

·       The process which produces metamorphic rocks is called metamorphism

·       Quartzite is the metamorphic form of the sedimentary rock, sandstone.

·       Slate is formed by the compression of sedimentary rocks like shale and mudstone. Gneiss is formed by the metamorphosis of igneous rocks like granite

·       Chalk is a calcareous rock made up of microscopic skeletal elements from a variety of lime secreting organisms.

·       Coal and Peat represent the accumulation of vegetation which originated in swamps. Peat is the first stage in the transformation of vegetable matter into coal.

·       ‘Black Twins’ is the name given to iron and coal. ‘Black lead’ is graphite. Anthracite is the most superior type of coal.

 

KERALA PSC / PHYSICAL GEOGRAPHY / ROCKS AND MINERALS / NOTES



KERALA PSC / PHYSICAL GEOGRAPHY / COMPOSITION OF THE EARTH’S CRUST / NOTES

 

KERALA PSC / PHYSICAL GEOGRAPHY / COMPOSITION OF THE EARTH’S CRUST / NOTES



KERALA PSC / PHYSICAL GEOGRAPHY / COMPOSITION OF THE EARTH’S CRUST / NOTES

 

·       Most abundant element in atmosphere is Nitrogen (78%) the Oxygen (21%). But the most abundant element in the universe is hydrogen.

·       The crust is made up of rocks. The rocks are made up of minerals in a consolidated form

·       The process of rock formation, consolidation of mineral particles is called lithification

·       A rock can be defined as an aggregate of minerals

·       The ratio between the total amount of light reflected from an object in space and the total amount of light falling on an object is called albedo.

·       A perfect reflector has an albedo of 1 and earth has an albedo of 0.34 (34%)

 

Composition of Crust

 

Earth is made up of more than hundred elements

v Oxygen                            -                   46.5%

v Silicon                             -                   27.72%

v Aluminium                      -                   8.13%

v Iron                                 _                  5.01%

v Calcium                           -                   3.63%

v Sodium                            -                   2.85%

v Pottasium                         -                   2.62%

v Magnisium                       -                   2.09%

 

KERALA PSC / PHYSICAL GEOGRAPHY / COMPOSITION OF THE EARTH’S CRUST / NOTES


KERALA PSC / PHYSICAL GEOGRAPHY / STRUCTURE OF EARTH / NOTES

 

KERALA PSC / PHYSICAL GEOGRAPHY / STRUCTURE OF EARTH / NOTES



KERALA PSC / PHYSICAL GEOGRAPHY / STRUCTURE OF EARTH / NOTES

 

·       The earth is made up of a number of concentric layers of materials as in the bulb of an onion

·       Earth can be divided into different layers such as Crust, Mantle and Core

·       Crust: This is the outer layer of the Earth varying between 5 to 50 km in depth under the surface of the earth

Ø It is the outermost and thinnest layer of the earth’s surface

Ø The crust comprises about 5% of the earth body

Ø Thickness of the crust is more under the continents and lesser under oceans

Ø The outermost layer of the crust is composed of lighter silicates termed as sial (Silica + Aluminium)

Ø Moho or Mohorovicic discontinuity separates crust from mantle.

Ø The average density of this layer is 2.7

·       Mantle: a layer between crust and the core

Ø Mantle contains 83% of the total volume and 68% of the total mass of the earth. Average density of this layer is 5.68.

Ø Mantle is separated from the core by Gutenberg discontinuity

Ø It is largely composed of silicon and magnesium called sima

Ø The rocks in this layer may be in the glassy state.

Ø The temperature of this layer ranges up to 1600ºC and extends downwards to a depth of about 1000 km. The thickness of the lower mantle is about 1900 km.

·       Core: is the central region of the earth

Ø It is 3475 km in radius

Ø By volume, it is 16% of the earth body

Ø By mass, it constitutes 32% of the mass of the earth. The outer core, approximately 2100km thick, consists of molten iron and nickel with temperatures ranging between 2000ºC and 5000ºC. Below this is the solid inner core which has diameter of 2740 km.

Ø The temperature of the inner core is 6000ºC-7000ºC.

Ø The inner core is composed of NiFe (Ni for Nickel Fe for Iron)

Ø Density of this part is 17.2

Ø Average density of earth is 5.53

 

KERALA PSC / PHYSICAL GEOGRAPHY / STRUCTURE OF EARTH / NOTES


KERALA PSC / PHYSICAL GEOGRAPHY / LOCATION OF PLACE AND TIME ON THE EARTH’S SURFACE / NOTES

 

KERALA PSC / PHYSICAL GEOGRAPHY / LOCATION OF PLACE AND TIME ON THE EARTH’S SURFACE / NOTES



KERALA PSC / PHYSICAL GEOGRAPHY / LOCATION OF PLACE AND TIME ON THE EARTH’S SURFACE / NOTES

 

·       Equator is an imaginary line passing round the earth midway between the north and south poles, dividing the earth into two equal halves.

·       Latitude is the angular distance in degrees on the earth’s surface measured north and south of the equator. The latitude of any point on the earth is most precisely expressed in degrees, minutes and seconds.

·       There are about 180 parallel latitudes. The distance between any two parallel latitudes is always equal. One degree of latitude is approximately equal to 111 km.

·       All the parallel of latitude are not of equal length. The circles become smaller towards the poles.

·       Equator is at 0ºC is the most important latitude and is the largest circle that can be drawn on the globe

·       A meridian is an imaginary line extending from the north pole to the south pole at right angles to the equator.

·       Prime Meridian is the 0º meridian which passes through Greenwich, a place near London. It is also known as the Greenwich meridian.

·       Longitudes are equi-distant lines drawn east and west of the Greenwich meridian. They denote the angular distances of a place due east or west of the Greenwich meridian. There are 360 meridians of longitudes.

·       One hour is equal to 15º of longitude

·       Longitude is an important factor in determining the time in all parts of the world. Local time of a place is calculated with respect to the midday position of the sun at that place.

·        Local time varies from Greenwich time (London) at the rate of four minutes/ degree of longitude.

·       Standard time is the uniform time fixed by each country

·       Standard time in India is the local time of a place near Allahabad at 82½ºE longitude.

·       Greenwich Mean Time is the standard time of UK. It is based on the local time of the meridian passing through Greenwich near London.

·       If a person going east of Greenwich for 180º, he would put his clock forward by 12 hours. At the same time if another person is going to west of Greenwich for 180º, he would put his clock backward by 12 hours. When they meet on the International Date Line, there would be one day’s difference between them.

·       Earth is divided into 23 full time zones and two half time zones each having longitudinal width of 15º and 7½º respectively

·       The International Date Line is situated at 180º meridian from Greenwich. It runs down the mid Pacific Ocean, veering to keep all of the islands in a group.

·       When one crosses the International Date Line from east to west the date is to be advanced by one day (loses on day). Similarly, when one crosses the Date Line from west to east, the date is to be set back by one day.

·        The International Date Line (the meridian 180º) was chosen because it passes through the mid-Pacific, where there are no land masses.

·       It goes zig-zag in some places to avoid land and leaves some island groups wholly on the same side of the line

·       It deflects to the east of 180º the Bering Strait, between Siberia and Alaska

·       It deflects to the West of 180 º to leave the Hawaiian group of islands on the East of the line

·       It deflects again to the East, South of the equator to avoid the Fiji and Tonga islands, on the same side as New Zealand. If the date line is drawn exactly North and South, it will cut inhabited islands making what is Tuesday to one man, a Wednesday his next door neighbour.

·       A ship while crossing the Date Line eastwards gains a day, while it loses a day crossing westwards.

·       The local time of Arunachal Pradesh is two hours ahead of that of Gujarat because Arunachal Pradesh is 30 º east of Gujarat.

·       Russia, the largest country in the world, extends 165 º from East to West. Therefore it is divided into eleven time zones, each differing in one hour.

·       The distance between any two meridians is not equal. They get closer from the equator to poles

·       Since earth rotates 15 º in one hour, there is a difference of one hour in local time in every 15 º

·       Sidereal day is the time between two observed passages of a star over the same meridian of longitude.

·       Sidereal day = 23 hrs.56 min.4.09 seconds

·       Solar day is the time between two successive transits of the sun over the same meridian.

·       Mean solar day = 24 hrs.

 

KERALA PSC / PHYSICAL GEOGRAPHY / LOCATION OF PLACE AND TIME ON THE EARTH’S SURFACE / NOTES