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THE EARTH'S CRUST

GRANITE ROCKS SIAL- The Oceanic Crust

    Si - silicon and A1 - aluminum.

    High density.

    Iron and calcium are also present.

    Younger part of crust - 200 million years old.

BASALTIC ROCKS

SIMA - The Continental Crust

    Si - silicon and Ma - Magnesium.

    Low density.

    Aluminum, potassium, and sodium.

    Older part of the crust - 3600 million years.

Mantle forms the second layer

    Second layer of the interior of the earth.

    Two sub - layers -1. Upper mantle and 2. Lower mantle.

    Thickness varies between 35km - 2900 km.

    Average density is 4.5 g/cm3

    Upper portion of mantle and crust together known as Lithosphere, lower mantle - Aesthenosphere.

Core

    Third layer of the earth.

    Formed by nickel and iron.

    Also called as Nife

    Nife - Ni - nickel and Fe - ferrous or iron

    Two parts

1.    Outer core.

2.    Inner core.

    Temperature is 11000° C.

    Inner core is in solid state.

CORE - divided in two layers

1.    Inner core

    Molten in stage

    Depth varies from 2900km - 5150 km.

    Density - 10.7 g/cm3.

2.    Outer core

    Solid in state

    High temperature

    High pressure

    Depth varies from - 5150 km - 6371 km

    Density - 15 g/cm3

The Classification of Rocks

 Rocks are Igneous Rocks, Sedimentary Rocks, Metamorphic Rocks.

Igneous Rocks

    Formed through cooling & solidification of molten material magma (

Erupted from volcanoes, molten material moves towards surface of earth through crack).

    Normally crystalline in structure, do not occur in strata & do not contains fossils.

    Can be subdivided on the basis of mineral composition.

    Basic rocks contain high proportion of basic oxides mainly of iron, aluminium & magnesium

    When they contain high proportion of silica they are said to be Acidic, which are less dense & lighter in color than basic rocks for ex. Granite

    Most igneous rocks are extremely hard & resistant hence are quarried for road making & polished as monuments & grave stones.

    Are parent / primary rocks as all other rocks are derived from it.

    In terms of origin they can be divided into mainly 2 classes viz.

GC Leong: Summary of The Earth`s Crust Notes | EduRev


Sedimentary Rocks

    Formed due to deposition of layers of sediment usually along the water bodies over a long period of time

    Sediment is deposited layer by layer in form of strata hence also known as

stratified rocks

    Process of turning sediments into hard rock layers by pressure is known as 

lithification.

    Rocks may be fine grained or coarse, soft or hard & material forming them may be brought by streams, glaciers, winds or even animals.

    May be derived from Igneous, Metamorphic or Sedimentary rocks.

    Hence, Sedimentary rocks are most varied in formation of all rocks.

    They are non-crystalline & often contains fossils of animals, plants & other microorganisms.

    May be classified under 3 categories with respect to their origin & composition viz

GC Leong: Summary of The Earth`s Crust Notes | EduRev


Metamorphic Rocks

Formed when original structure of igneous & sedimentary rocks partially or wholly change under the action of heat & pressure.

    Contains no fossils

    No stratification

    For ex. Clay —> Slate Igneous to Metamorphic Granite —> Gneiss

Mica —» Schist Gabro —> Serpentite Sedimentary to Metamorphic Limestone —> Marble Sandstone —> Quartzite Shale —*■ Schist Coal —» Graphite

Bituminous coal —> Anthracite coal

Types of Mountains

1.    Fold Mountains

    Formed by folding of geosyncline sediments under compressible tectonic forces.

    For Ex. Himalaya, Alps, Rockies, Andes, Alapchhian, Ural, Aravalis

    Since the rock strata have been elevated to great heights, Fold Mountains are also called mountains of elevation.

    Are closely associated with volcanic activities.

    Contains many active volcanoes, especially in circum Pacific fold mountain system.

    Are rich in mineral resources such as Tin, Copper, Gold & Petroleum

2.    Block Mountains

    Formed due to faults caused by tension or compression forces which lengthen or shorten earth’s crust.

    It causes a section of it to subside or rise above the surrounding level.

    For Ex. Vosges (France), Black Forest (Germany)

    Faulting results in formation of Block Mountains & their counterparts in rift valleys.

    In general, large scale Block Mountains & rift valleys are due to tension rather than compression.

3.    Volcanic Mountains

    Also known as mountains of accumulation.

    Formed due to accumulation of thick lava as a result of volcanic eruption.

    Common in circum pacific belt.

    For Ex. Fuji Yama (Japan), Mt. Popa (Myanmar), Mt. Mauna loa (Hawai), Mt. Mayon (Phillipines), Mt. Agung (Bali), Mt. Merapi (Sumatra) & Mt. Catopaxi (Ecuador)

4.    Residual / Dissected / Relict Mountains

    Formed due to waning of previously existing elevated regions by erosion.

    For Ex. Nilgiris, Parshavnath, Hills of Peninsula India, Mt. Manodnock

(USA).

    Mountains evolved by denudation, where the general level of land have been lowered by agents of denudation; also known as mountains of denudation.

Types of Plateaus

    An elevated area compared to its surroundings, having a large almost flat top area (Also known as tableland).

    Like all highlands, Plateaus are also subjected to erosional processes, as a result their original characteristics are highly altered.

    According to their mode of formation & their physical appearance, plateaus may be divided into 3 types viz.

1.    Tectonic Plateaus

    Formed by earth movements which causes uplift, of a considerable size with fairly uniform altitude.

    For ex. Deccan plateaus, Mesera plateau (tilted of central Iberia) & Harz plateau (Faulted of Germany).

    When plateaus are surrounded by mountains they are known as intermontane plateaus for ex. Tibetian plateau, Bolivian Plateau.

    When plateaus are surrounded by sea or plains they are known as Continental Plateaus For ex. Deccan plateau, Greenland plateau, South Africa plateau

2.    Volcanic Plateau

    Molten lava from the volcanic eruption may solidify to form successive sheets of basalatic lava, known as Lava plateau.

    For ex. Antrim Plateau of Northern island, NW part of Deccan Plateau & Columbia Snake Plateau (Biggest one).

3.    Dissect Plateaus

    Formed due to continuous weathering & erosion by running water, wind & ice.

    High plateaus worn down & their surface becomes irregular.

    For Ex. Scottish Highland

    Generally Plateaus have rich mineral resources & have been actively mined for ex.

    African plateau yields gold, diamonds, copper, Manganese & Chromium.

    Brazilian plateau yields iron & Manganese

    Deccan Plateau yields Manganese, Iron & Coal

    Western Australian plateau yields Gold & Iron.

Types of Plains

Plains

    Plains usually are the best land of a country & are heavily cultivated & populated.

    Even more at places where rivers transverse the plains.

    For ex: Indo Gangetic Plains, Mississippi Plains & Yang-Tze plain .Some of the most extensive temperate plains are Grasslands like Russian Steppes, 

North American Prairies & Argentinian Pampas.

    Plains may be grouped into 3 major types based on their mode of formation viz.

1.    Structural Plains

    Structurally depressed areas of the world that makes up some of the most extensive natural lowlands on the earth’s surface.

    Rock layers on the earth’s crust are aligned almost horizontally.

    They are formed by horizontally bedded rocks, relatively undisturbed by the crustal movements of the earth.

    Examples include Russian Platforms, Great plains of USA & Central lowlands of Australia.

2.    Depositional Plains

    Plains formed by deposition of materials brought by various agents of transportation.

    Comparatively of equal level but rise gently towards adjacent highlands.

    Depositional work by rivers form extensive alluvial plains, flood plains & deltaic plains; that form most productive agricultural plains of the world.

    For ex. Gangetic plain (for rice & jute), Nile delta of Egypt (for rice & cotton) & Hwang ho plain in China.

3.    Glacial Depositional plains

    Glaciers & ice sheets may deposit fluvio glacial sands & gravels in outwash plains.

    May also drop boulder clay (mixture of various sizes of boulders & clay) to form till plain or drift plain.

    Outwash plains are usually barren lands but boulder clay may be very valuable for farming.

4.    Aeolian Depositional plains

    Winds may blow Aeolian deposits, very fine particles known as loess, from interior deserts or barren surfaces & deposit them upon hills, valleys or plains forming a loess plateau (ex. in NW China) or a loess plain (Ex. In Pampas of Argentina)

    The loess help in leveling the undulating plain by filling up groves & depressions

    Many of the loess covered plains in the world are fertile agricultural regions.

5.    Erosional Plains

    These plains are carved by the agents of erosion (Rain, river, ice, and wind)

    Such plains of denudation are described as Peneplains, which means almost plains.

    In glaciated regions, glaciers & ice sheets scours & levels the land forming ice

scoured plains.

    However scooped out by the ice are now filled by the lakes for ex. In Northern Europe & Northern Canada.

    Finland is estimated to have 35000 lakes occupying 10 % of total land surface of the country

    In arid & semi-arid regions, wind erosion lowers the level of the land which are called Reg in Africa.

    Mechanical weathering in arid & semi-arid areas woms mountain slopes leaving a gentle slope, known as Pediplains or Pediments; with remaining steep hills known as Inselbergs.

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