Basic Geology Course

Wednesday, March 2, 2011

Mood of Formation of Igneous Rock

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Igneous rocks are formed by the cooling of hot magma.The grain size of magma depends on the following factors. 1.Rate of cooling: If magma...
Monday, February 28, 2011

Factors affecting erosion and transportation

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Nature of rock: Soft rocks show higher erosion and hard rocks show lower erosion. Attitude of rock:How rocks are placed affect erosion.Incli...
Sunday, February 27, 2011

Metamorphism

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Metamorphism is the phenomenon in which heat, pressure and chemically formed liquid bring about textural,structural and mineralogical change...

Types of Sedimentary Rocks

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Sedimentary rocks are of following types: 1.Clastic Sedimentary rocks:These are sedimentary rocks formed by sedimentation and consolidation ...
Saturday, February 26, 2011

Magmatic Differentiation

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The process of separation of different mineral constituents from magmatic melt is called magmatic differentiation. Types of magmatic differe...
Friday, February 25, 2011

Importance of Geology in Civil Engeneering

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1. To make foundation for dams,airports,bridges and buildings 2. For tunnel construction 3. For excavation,fills and retaining walls and har...
Friday, February 11, 2011

Earthquake

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Earthquake is the sudden and temporary vibration of earth surface ranging from a fair tremor to a wild motion due to sudden release of energ...
Monday, February 7, 2011

Unconformities

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Definition Unconformities are defined as surface of erosion of rock separating the underlying older formation from overlying younger formati...
Sunday, February 6, 2011

Salient Charecteristics of Youth,Mature andOld Stages of River

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Youth Stage 1.In this stage rivers flows through hilly region. 2.Gradient of river is high. 3.Velocity of water is high. 4.Deepening is high...

Weathering

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The term weathering is used for disintegration and decomposition of rocks without any significant transportation of resulting product. ...
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Kyleyx
Student of Chittagong University of Engineering and Technology, Bangladesh
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