UPSC GEOGRAPHY
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This channel provides notes from different major books like D.R. khullar, G.C leong etc No copyright material allowed. Queries - @Upscgeographybot
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“This channel provides notes from different major books like D.R. khullar, G.C leong etc
No copyright material allowed.
Queries - @Upscgeographybot”
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■ IGNEOUS ROCKS
#Rocks #Geomorphology
◇ The word igneous has been derived form a Latin word ‘Ignis’, meaning thereby fire.
◇ The rocks are formed due to cooling, solidification and crystallization of hot and molten materials known as magmas and lavas.
◇ Also called as primary rocks because these were originated first of all the rocks during the formation of upper crust of the earth on cooling, solidification and crystallization of hot and liquid magmas after the origin of the earth.
◇ All the subsequent rocks were formed, whether directly or indirectly, from the igneous rocks in one way or the other. This is why igneous rocks are also called as parent rocks.
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Repost from UPSC GEOGRAPHY
◇ Laccoliths - Laccoliths are formed due to injection (intrusion) of magmas along the bedding planes of horizontally bedded sedimentary rocks. Laccoliths are of mushroom shape having convex summital form.
◇ Phacoliths - are formed due to injection of magma along the anticlines and synclines in the regions of folded mountains.
◇ Lopoliths —The word lopolith has been derived from German word 'lopas' meaning thereby a shallow basin or bowl shape body. When magma is injected and solidified in a concave shallow basin whose central part is sagged downward, the resultant form of solidified magmas is called a lopolith.
◇ Sills - The sills are usually parallel to the bedding planes of sedimentary rocks. In fact, sills are formed due to injection and solidification of magmas between the bedding planes of sedimentary rocks. Thick beds of magmas are called sills whereas thin beds of magma are termed as ‘sheets .
◇ Dykes - represent wall-like formation of solidified magmas. These are mostly perpendicular to the beds of sedimentary rocks.
▪︎JOIN - @upsc_geography_notes
66 562
Repost from UPSC GEOGRAPHY
■ INTRUSIVE LANDFORMS
#Geomorphology #Igneousrocks
◇ The magmas are solidified in different forms depending upon the hollow places such as batholiths, laccoliths, phacoliths, lopoliths, sills, dikes, etc.
◇ Batholiths - are long irregular and undulating forms of solidified intruded magmas. They are usually dome-shaped and their side walls are very steep, almost vertical. The upper portions of batholiths are seen when the super incumbent cover is removed due to continued denudation but their bases are never seen because they are buried deep within the earth.
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◇ Laccoliths - Laccoliths are formed due to injection (intrusion) of magmas along the bedding planes of horizontally bedded sedimentary rocks. Laccoliths are of mushroom shape having convex summital form.
◇ Phacoliths - are formed due to injection of magma along the anticlines and synclines in the regions of folded mountains.
◇ Lopoliths —The word lopolith has been derived from German word 'lopas' meaning thereby a shallow basin or bowl shape body. When magma is injected and solidified in a concave shallow basin whose central part is sagged downward, the resultant form of solidified magmas is called a lopolith.
◇ Sills - The sills are usually parallel to the bedding planes of sedimentary rocks. In fact, sills are formed due to injection and solidification of magmas between the bedding planes of sedimentary rocks. Thick beds of magmas are called sills whereas thin beds of magma are termed as ‘sheets .
◇ Dykes - represent wall-like formation of solidified magmas. These are mostly perpendicular to the beds of sedimentary rocks.
▪︎JOIN - @upsc_geography_notes
66 562
■ INTRUSIVE LANDFORMS
#Geomorphology #Igneousrocks
◇ The magmas are solidified in different forms depending upon the hollow places such as batholiths, laccoliths, phacoliths, lopoliths, sills, dikes, etc.
◇ Batholiths - are long irregular and undulating forms of solidified intruded magmas. They are usually dome-shaped and their side walls are very steep, almost vertical. The upper portions of batholiths are seen when the super incumbent cover is removed due to continued denudation but their bases are never seen because they are buried deep within the earth.
66 562
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66 562
■ INTRUSIVE IGNEOUS ROCKS
#Geomorphology #Rocks
◇ When the rising magmas during a volcanic activity do not reach the earth's surface rather they are cooled and solidified below the surface of the earth, the resultant igneous rocks are called intrusive igneous rocks.
◇ These rocks are further subdivided into two major groups of plutonic intrusive igneous rocks and hypabyssal intrusive igneous rocks.
◇ Plutonic igneous rocks are formed due to cooling of magmas very deep inside the earth. Since the rate of cooling of magmas is exceedingly slow because of high temperature prevailing there and hence there is sufficient time for the full development of large grains.
◇ Hypabyssal igneous rocks are formed due to cooling and solidification of rising magma during volcanic activity in the cracks, pores, crevices, and hollow places just beneath the earth's surface, the resultant rocks are called as hypabyssal igneous rocks.
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66 562
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66 562
Repost from UPSC GEOGRAPHY
■ CLASSIFICATION OF ROCKS
#Geomorphology #Rocks
◇ The crustal rocks are classified on several grounds e.g. mode of formation, physical and chemical properties, locations etc.
◇ On the basis of mode of formation The rocks are divided into three broad categories :-
1. Igneous rocks
2. Sedimentary rocks,
3. Metamorphic rocks.
▪︎JOIN - @upsc_geography_notes
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66 562
■ CLASSIFICATION OF ROCKS
#Geomorphology #Rocks
◇ The crustal rocks are classified on several grounds e.g. mode of formation, physical and chemical properties, locations etc.
◇ On the basis of mode of formation The rocks are divided into three broad categories :-
1. Igneous rocks
2. Sedimentary rocks,
3. Metamorphic rocks.
▪︎JOIN - @upsc_geography_notes
