Fundamentals of Geology
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The presentation aiding the lecture Fundamentals of Geology for the course CE 8392 Engineering Geology handled by Prof. Rathnavel Pon for Akshaya College of Engineering and Technology, Coimbatore
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Grades of metamorphism
This document summarizes the different grades of metamorphism: very low-grade, low-grade, medium-grade, and high-grade. Each grade is defined by the typical temperature and pressure conditions and indicator minerals present. Very low-grade occurs below 200°C and involves minerals like lawsonite. Low-grade occurs from 200-300°C and involves hydrous minerals. Medium-grade occurs from 400-550°C and involves minerals like staurolite and cordierite. High-grade occurs above 600°C and involves breakdown of minerals like muscovite. Isogrades are lines that indicate boundaries of metamorphic grade based on the appearance of indicator minerals.
Classification of igneous rocks
This document classifies igneous rocks based on their visible crystal size, composition, and mineralogy. It divides rocks into phaneritic, aphanitic, porphyritic, fragmental, pegmatitic, and glassy categories based on crystal size. It further classifies rocks as felsic, intermediate, mafic, or ultramafic based on their silica and iron/magnesium content. Diagrams show classifications of specific rock types like plutonic rocks, volcanic rocks, gabbroic rocks, and ultramafic rocks based on their mineralogy and compositions.
STRATIGRAPHIC CORRELATION
Historical geology Is the branch which deals with the history of the rocks of the earth’s crust with special emphasis on their approximate time of formation and the climate changes they have undergone since their formation.
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Geological criteria in exploration
The document discusses the various geological criteria used in mineral exploration, including stratigraphic, structural, lithological, magmatogenic, metamorphogenic, geomorphological, paleogeographical, paleoclimatic, and historical criteria. Geological criteria are an indirect method of locating ore deposits to save time and money during exploration. Some examples of deposits associated with different criteria include stratigraphically-controlled coal and uranium, structurally-controlled porphyry copper deposits related to subduction zones, and lithologically-controlled tin deposits associated with granitic rocks.
Geological mapping
Geological mapping involves systematically observing and recording rock exposures and structural features in the field to produce maps that show the spatial distribution and relationships of rock units. The document discusses different types of geological maps including reconnaissance, regional, detailed, and specialized maps. It also describes common mapping techniques such as traversing, exposure mapping, drilling, underground mapping, and photo-geology. Field equipment used in mapping includes hammers, chisels, compasses, clinometers, tapes, and notebooks.
Geochemical methods in mineral exploration
This document discusses geochemical methods for mineral exploration. It covers general principles of geochemistry as they relate to mineral deposits. It also discusses optimizing exploration through proper planning, selection of areas and methods, and organization of field, lab, and supervisory operations. Geochemistry is described as an essential component of modern integrated exploration programs due to the low-grade, large-tonnage nature of most economic deposits and its effectiveness in weathered tropical environments.
Fluvial depositional landform geomorphology
This document summarizes fluvial depositional landforms. It begins with an introduction to stream deposition and fluvial landforms. It then discusses reasons for sediment deposition including changes in slope, flow obstructions, and sediment supply. Major landforms are classified and explained, including alluvial fans/cones, braided streams, meandering belts, point bars, backswamps, floodplains, natural levees, and river deltas. Specific features of each landform like bar formation and channel abandonment are described. The document concludes by noting the geological significance of these landforms and their use for cultivation.
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Grades of metamorphism
This document summarizes the different grades of metamorphism: very low-grade, low-grade, medium-grade, and high-grade. Each grade is defined by the typical temperature and pressure conditions and indicator minerals present. Very low-grade occurs below 200°C and involves minerals like lawsonite. Low-grade occurs from 200-300°C and involves hydrous minerals. Medium-grade occurs from 400-550°C and involves minerals like staurolite and cordierite. High-grade occurs above 600°C and involves breakdown of minerals like muscovite. Isogrades are lines that indicate boundaries of metamorphic grade based on the appearance of indicator minerals.
Classification of igneous rocks
This document classifies igneous rocks based on their visible crystal size, composition, and mineralogy. It divides rocks into phaneritic, aphanitic, porphyritic, fragmental, pegmatitic, and glassy categories based on crystal size. It further classifies rocks as felsic, intermediate, mafic, or ultramafic based on their silica and iron/magnesium content. Diagrams show classifications of specific rock types like plutonic rocks, volcanic rocks, gabbroic rocks, and ultramafic rocks based on their mineralogy and compositions.
STRATIGRAPHIC CORRELATION
Historical geology Is the branch which deals with the history of the rocks of the earth’s crust with special emphasis on their approximate time of formation and the climate changes they have undergone since their formation.
ELEMENTS OF CORRELATION, STRUCTURAL FEATURES, METHOD OF STRATIGRAPHIC CORRELATION ,
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Geological criteria in exploration
The document discusses the various geological criteria used in mineral exploration, including stratigraphic, structural, lithological, magmatogenic, metamorphogenic, geomorphological, paleogeographical, paleoclimatic, and historical criteria. Geological criteria are an indirect method of locating ore deposits to save time and money during exploration. Some examples of deposits associated with different criteria include stratigraphically-controlled coal and uranium, structurally-controlled porphyry copper deposits related to subduction zones, and lithologically-controlled tin deposits associated with granitic rocks.
Geological mapping
Geological mapping involves systematically observing and recording rock exposures and structural features in the field to produce maps that show the spatial distribution and relationships of rock units. The document discusses different types of geological maps including reconnaissance, regional, detailed, and specialized maps. It also describes common mapping techniques such as traversing, exposure mapping, drilling, underground mapping, and photo-geology. Field equipment used in mapping includes hammers, chisels, compasses, clinometers, tapes, and notebooks.
Geochemical methods in mineral exploration
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Fluvial depositional landform geomorphology
This document summarizes fluvial depositional landforms. It begins with an introduction to stream deposition and fluvial landforms. It then discusses reasons for sediment deposition including changes in slope, flow obstructions, and sediment supply. Major landforms are classified and explained, including alluvial fans/cones, braided streams, meandering belts, point bars, backswamps, floodplains, natural levees, and river deltas. Specific features of each landform like bar formation and channel abandonment are described. The document concludes by noting the geological significance of these landforms and their use for cultivation.
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Introduction to engineering geology
Engineering geology is a branch of applied geology that deals with the application of geological knowledge and principles to civil engineering projects. It provides essential information for safe, stable, and economical design and construction of structures like buildings, dams, roads, and tunnels. Engineering geological studies are conducted during planning, design, construction, and post-construction phases of projects. The studies help understand site conditions, availability of construction materials, and how to mitigate geological hazards. Knowledge of geology is crucial for heavy construction projects and excavation works to plan realistically and design sound foundations.
Open pit mining
Open pit mining, also called surface mining, involves excavating minerals or rock that are close to the surface. There are two main types of mining methods: underground mining, which excavates deeper deposits; and surface mining, where the deposits are closer to the surface. Open pit mining involves digging a pit on the surface to extract near-surface mineral deposits through horizontal benches. It is best suited for deposits that are no deeper than 300 meters and have a low ratio of overburden rock to ore. The process involves site preparation, drilling and blasting of overburden rock, removing overburden with heavy machinery, excavating and transporting ore, and reclaiming the land after mining is complete.
An Introduction to physical geology
The presentation contains basic terms of Physical Geology which is related to Geology. It is a gross presentation including images and animated gif's for better understanding.
Mechanical characters of rock
This document summarizes the key mechanical properties of rocks, including density, specific gravity, strength, strain, stress, porosity, and permeability. It defines each property, provides examples for common rock types, and notes that mechanics refers to how materials respond to applied loads. The conclusion restates that the document covered the mechanical characteristics of rocks according to these seven properties.
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joints and its classification and its recognition
Joints are fractures in rock without displacement. They form due to tension, shear, or compressive stresses. Joints can be classified based on their orientation relative to bedding, their geometry, genesis, and dip. Systematic joints are parallel while nonsystematic joints have irregular distributions. Joints influence groundwater flow, construction, and are important in mining and resource exploration. They provide pathways for fluid migration and impact slope stability.
Geological fieldwork report
The geological fieldwork conducted in Chobhar, Nepal aimed to provide practical geological knowledge to crisis management students. Key activities included observing landforms, structures, and rock types; gaining information from topographical maps; measuring geological orientations; and locating one's position on a map. The fieldwork helped students understand geological processes of the past that influenced landform development and how this knowledge can inform crisis management and planning.
Presentation on geophysical methods
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150 branches of geology
Geology is the scientific study of the all constituents of planets, their internal and external forms and processes. More precisely, it is the study of nature, structure and history of the planet. Earth is the home to all life, well known to the humankind. Geology, itself, is a major part of The Earth and atmospheric sciences, which were born as twins . The subject of geology encompasses all aspects including the composition, structure, physical properties, and history of a planets'( like Earth's) inter-related components and the processes that are shaping the features on the surface. Geologists are the scientists who study the origin, occurrence, distribution and utilities of all materials(metallic, non-metallic, inorganic, etc), minerals, rocks, sediments, soils, water, oil and all other inorganic natural resources. It is a very vast subject covering a wide spectrum of scientific principles and holding hundred and fifty plus scientific branches. This report enumerates and highlights most of them, in a nutshell, for all those who intends to know for planning their career path.
Stress and strain ellipsoid
This document discusses stress and strain ellipsoids in structural geology. It defines stress as a force applied over an area that causes rock deformation. Stress can be tensional, compressional, or shear. Strain is the response of rock to stress and describes the change in shape of an object under stress. Stress and strain are represented geometrically using ellipsoids. The relationship between stress and strain ellipsoids is that the greatest and least axes are opposite. The orientation of stress and strain ellipsoids provides information about the deformative forces acting on rocks.
PROCESSES OF FORMATION OF ORE DEPOSIT
The document summarizes the various processes of formation of ore deposits, which are grouped into three main types: magmatic, sedimentary, and metamorphic. Magmatic processes include magmatic concentration, hydrothermal processes, and sublimation. Sedimentary processes include sedimentary deposits, oxidation and supergene enrichment, residual and mechanical concentration, volcanogenic deposits, evaporation, and bacteriogenic processes. The key magmatic and sedimentary processes are described in further detail.
Isostasy
1. The document discusses concepts in geophysics including isostasy, density, susceptibility, and resistivity of rocks. Isostasy refers to equilibrium between the earth's lithosphere and asthenosphere. Density is a measure of how tightly packed molecules are in a material. Susceptibility measures a material's magnetization in response to an external magnetic field. Resistivity quantifies a material's opposition to electric current flow.
2. Igneous rocks generally have higher density, susceptibility, and resistivity compared to metamorphic and sedimentary rocks. This is because igneous rocks contain more mafic minerals and have undergone less alteration from their original state than other rock types. Factors like pore space,
Introduction marine geology
Marine geology is the study of the Earth below the oceans and seas. It examines the character and history of ocean floors and coastal areas. Major developments in marine geology include the HMS Challenger expedition in the 1870s which made the first systematic survey of ocean basins, and the Lamont-Doherty Geological Observatory founded in 1948 which advanced techniques like precision depth recording and piston coring. Deep-sea drilling projects from the 1960s-1980s using vessels like the Glomar Challenger confirmed theories of seafloor spreading and plate tectonics through ocean floor sampling and drilling.
UNCONFORMITY BY DHARMESH
This document defines and describes different types of unconformities in geology. It begins by defining an unconformity as a break or gap in the geological record representing a period of erosion or non-deposition. It then describes the major types of unconformities, including angular, disconformity, non-conformity, and local unconformities. Finally, it outlines several ways that unconformities provide significance, such as indicating time intervals missing from the geological record, structural discordances between rock layers, evidence of past topography, and signs of weathering at the contact surface.
Folds
This lecture includes the fold terminology and classification of folds based of different criteria.
Classification of folds based on:
Direction of closing
Attitude of axial surface
Size of interlimb angle
Profile
Ramsay Classification of folds
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Economic Geology, Engineering Geology, Mining Geology
Geo physics, Geo Hydrology, Geo Chemistry, Scope of Geology
Importance of Geology in Civil Engineering, General Geology
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Core, Tectonic Plates, Types of Plate Boundaries, Plates collide = convergent boundary, Plates separate = divergent boundary
Plates slide past one another = transform boundary.
Metamorphic textures
This document discusses metamorphic textures, which refer to the physical appearance or arrangement of minerals in metamorphic rocks at the microscopic level. There are several types of textures that can form during metamorphism due to factors like heat, pressure, and chemically active fluids. Typomorphic textures are characteristic of metamorphism and include porphyroblastic, mortar, and granoblastic textures. Relict textures are inherited from the original rock, such as ophitic or porphyritic textures. Reaction textures involve chemical reactions between minerals, forming textures like coronas or reaction rims. The document provides examples of different textures and concludes that textures provide information about the metamorphic conditions and original rock type.
Sedimentary structure
This document discusses sedimentary structures, which are macroscopic features formed during sediment deposition. It classifies sedimentary structures based on their morphology and formation processes. The key types discussed are physical structures like bedding, cross-bedding, and ripple marks formed directly by sedimentation. Chemical structures like nodules and concretions are formed by precipitation. Biogenic structures such as stromatolites and trace fossils provide evidence of ancient life. Studying sedimentary structures can provide insight into depositional environments, paleocurrents, and stratigraphic relationships.
Principle of Stratigraphic
This document summarizes key concepts in stratigraphy and sequence stratigraphy. It discusses the principles of stratigraphy including superposition, original horizontality, and lateral continuity. It also describes unconformities and how they represent gaps in the stratigraphic record. Sequence stratigraphy divides rock sequences into systems tracts based on bounding surfaces and stacking patterns. Sequences are bounded by unconformities and composed of parasequence sets, which are made up of genetically related beds bounded by flooding surfaces.
1.1 geology & its branches
This document provides an introduction to geology and its importance from a civil engineering perspective. It discusses the definitions and branches of geology, including mineralogy, petrology, geophysics, stratigraphy, physical geology, hydrogeology, and structural geology. The branches study minerals, rocks, the structure and evolution of the Earth, rock layers and ages, geological processes and landforms, groundwater, and rock structures. The document emphasizes the importance of geology for civil engineers for site selection, understanding construction materials and ground conditions, planning projects, and treating geological features like faults or joints that could impact stability. A foundation in the introduction to geology and key branches is important for civil engineers.
What is geology and scope of geology
Geology is the study of the Earth, including its composition, structure, physical properties, history and the processes that shape it. The document outlines several key branches of geology, including economic geology, mining geology, petroleum geology, engineering geology, environmental geology, geochemistry, geomorphology, geophysics, historical geology, hydrogeology, mineralogy, paleontology, petrology, structural geology, sedimentology, stratigraphy and volcanology. Each branch deals with different aspects of the Earth and geological processes. Engineering geology specifically applies geological knowledge to civil engineering projects regarding construction materials, site selection, and safe design and construction.
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The document outlines the key stages of mining exploration and prospecting. Prospecting uses direct methods like visual examination of rock exposures and indirect geophysical/geochemical techniques to locate potential mineral deposits. Exploration utilizes more advanced tools like drilling and geochemical analysis to determine the size and grade of identified deposits. Samples are analyzed and feasibility studies conducted to assess mining viability based on factors like reserves, costs, environment, and demand. If viable, projects then progress to the development and exploitation stages of mining.
Introduction to engineering geology
Engineering geology is a branch of applied geology that deals with the application of geological knowledge and principles to civil engineering projects. It provides essential information for safe, stable, and economical design and construction of structures like buildings, dams, roads, and tunnels. Engineering geological studies are conducted during planning, design, construction, and post-construction phases of projects. The studies help understand site conditions, availability of construction materials, and how to mitigate geological hazards. Knowledge of geology is crucial for heavy construction projects and excavation works to plan realistically and design sound foundations.
Open pit mining
Open pit mining, also called surface mining, involves excavating minerals or rock that are close to the surface. There are two main types of mining methods: underground mining, which excavates deeper deposits; and surface mining, where the deposits are closer to the surface. Open pit mining involves digging a pit on the surface to extract near-surface mineral deposits through horizontal benches. It is best suited for deposits that are no deeper than 300 meters and have a low ratio of overburden rock to ore. The process involves site preparation, drilling and blasting of overburden rock, removing overburden with heavy machinery, excavating and transporting ore, and reclaiming the land after mining is complete.
An Introduction to physical geology
The presentation contains basic terms of Physical Geology which is related to Geology. It is a gross presentation including images and animated gif's for better understanding.
Mechanical characters of rock
This document summarizes the key mechanical properties of rocks, including density, specific gravity, strength, strain, stress, porosity, and permeability. It defines each property, provides examples for common rock types, and notes that mechanics refers to how materials respond to applied loads. The conclusion restates that the document covered the mechanical characteristics of rocks according to these seven properties.
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joints and its classification and its recognition
Joints are fractures in rock without displacement. They form due to tension, shear, or compressive stresses. Joints can be classified based on their orientation relative to bedding, their geometry, genesis, and dip. Systematic joints are parallel while nonsystematic joints have irregular distributions. Joints influence groundwater flow, construction, and are important in mining and resource exploration. They provide pathways for fluid migration and impact slope stability.
Geological fieldwork report
The geological fieldwork conducted in Chobhar, Nepal aimed to provide practical geological knowledge to crisis management students. Key activities included observing landforms, structures, and rock types; gaining information from topographical maps; measuring geological orientations; and locating one's position on a map. The fieldwork helped students understand geological processes of the past that influenced landform development and how this knowledge can inform crisis management and planning.
Presentation on geophysical methods
This document provides an overview of geophysical methods used for site investigation and laboratory measurements. It discusses various methods including electrical resistivity, seismic methods, electromagnetic conductivity, gravity geophysical methods, and geothermal methods. For each method, it describes how the technique works and how tests are conducted to collect subsurface data on properties like density, conductivity, and elastic moduli. The document aims to explain different geophysical techniques that can be employed to characterize subsurface conditions.
150 branches of geology
Geology is the scientific study of the all constituents of planets, their internal and external forms and processes. More precisely, it is the study of nature, structure and history of the planet. Earth is the home to all life, well known to the humankind. Geology, itself, is a major part of The Earth and atmospheric sciences, which were born as twins . The subject of geology encompasses all aspects including the composition, structure, physical properties, and history of a planets'( like Earth's) inter-related components and the processes that are shaping the features on the surface. Geologists are the scientists who study the origin, occurrence, distribution and utilities of all materials(metallic, non-metallic, inorganic, etc), minerals, rocks, sediments, soils, water, oil and all other inorganic natural resources. It is a very vast subject covering a wide spectrum of scientific principles and holding hundred and fifty plus scientific branches. This report enumerates and highlights most of them, in a nutshell, for all those who intends to know for planning their career path.
Stress and strain ellipsoid
This document discusses stress and strain ellipsoids in structural geology. It defines stress as a force applied over an area that causes rock deformation. Stress can be tensional, compressional, or shear. Strain is the response of rock to stress and describes the change in shape of an object under stress. Stress and strain are represented geometrically using ellipsoids. The relationship between stress and strain ellipsoids is that the greatest and least axes are opposite. The orientation of stress and strain ellipsoids provides information about the deformative forces acting on rocks.
PROCESSES OF FORMATION OF ORE DEPOSIT
The document summarizes the various processes of formation of ore deposits, which are grouped into three main types: magmatic, sedimentary, and metamorphic. Magmatic processes include magmatic concentration, hydrothermal processes, and sublimation. Sedimentary processes include sedimentary deposits, oxidation and supergene enrichment, residual and mechanical concentration, volcanogenic deposits, evaporation, and bacteriogenic processes. The key magmatic and sedimentary processes are described in further detail.
Isostasy
1. The document discusses concepts in geophysics including isostasy, density, susceptibility, and resistivity of rocks. Isostasy refers to equilibrium between the earth's lithosphere and asthenosphere. Density is a measure of how tightly packed molecules are in a material. Susceptibility measures a material's magnetization in response to an external magnetic field. Resistivity quantifies a material's opposition to electric current flow.
2. Igneous rocks generally have higher density, susceptibility, and resistivity compared to metamorphic and sedimentary rocks. This is because igneous rocks contain more mafic minerals and have undergone less alteration from their original state than other rock types. Factors like pore space,
Introduction marine geology
Marine geology is the study of the Earth below the oceans and seas. It examines the character and history of ocean floors and coastal areas. Major developments in marine geology include the HMS Challenger expedition in the 1870s which made the first systematic survey of ocean basins, and the Lamont-Doherty Geological Observatory founded in 1948 which advanced techniques like precision depth recording and piston coring. Deep-sea drilling projects from the 1960s-1980s using vessels like the Glomar Challenger confirmed theories of seafloor spreading and plate tectonics through ocean floor sampling and drilling.
UNCONFORMITY BY DHARMESH
This document defines and describes different types of unconformities in geology. It begins by defining an unconformity as a break or gap in the geological record representing a period of erosion or non-deposition. It then describes the major types of unconformities, including angular, disconformity, non-conformity, and local unconformities. Finally, it outlines several ways that unconformities provide significance, such as indicating time intervals missing from the geological record, structural discordances between rock layers, evidence of past topography, and signs of weathering at the contact surface.
Folds
This lecture includes the fold terminology and classification of folds based of different criteria.
Classification of folds based on:
Direction of closing
Attitude of axial surface
Size of interlimb angle
Profile
Ramsay Classification of folds
Introduction of Engineering Geology
UNIT -1
INTRODUCTION, WHY GEOLOGY ???, GEOLOGY, Main and Allied Branch of Geology, Physical Geology, Mineralogy, Petrology, Structural Geology, Historical Geology, Palaeontology
Economic Geology, Engineering Geology, Mining Geology
Geo physics, Geo Hydrology, Geo Chemistry, Scope of Geology
Importance of Geology in Civil Engineering, General Geology
Geological Agents, Exogenous Geological Agents, Endogenous Geological Agents, Weathering of Rocks, Mechanical, Weathering, Chemical weathering, Biological Weathering, Earth Structure, Atmosphere, Troposphere, Stratosphere, Mesosphere, Thermosphere, Exosphere, Earth Interior Structure, Lithosphere, Crust, Mantle
Core, Tectonic Plates, Types of Plate Boundaries, Plates collide = convergent boundary, Plates separate = divergent boundary
Plates slide past one another = transform boundary.
Metamorphic textures
This document discusses metamorphic textures, which refer to the physical appearance or arrangement of minerals in metamorphic rocks at the microscopic level. There are several types of textures that can form during metamorphism due to factors like heat, pressure, and chemically active fluids. Typomorphic textures are characteristic of metamorphism and include porphyroblastic, mortar, and granoblastic textures. Relict textures are inherited from the original rock, such as ophitic or porphyritic textures. Reaction textures involve chemical reactions between minerals, forming textures like coronas or reaction rims. The document provides examples of different textures and concludes that textures provide information about the metamorphic conditions and original rock type.
Sedimentary structure
This document discusses sedimentary structures, which are macroscopic features formed during sediment deposition. It classifies sedimentary structures based on their morphology and formation processes. The key types discussed are physical structures like bedding, cross-bedding, and ripple marks formed directly by sedimentation. Chemical structures like nodules and concretions are formed by precipitation. Biogenic structures such as stromatolites and trace fossils provide evidence of ancient life. Studying sedimentary structures can provide insight into depositional environments, paleocurrents, and stratigraphic relationships.
Principle of Stratigraphic
This document summarizes key concepts in stratigraphy and sequence stratigraphy. It discusses the principles of stratigraphy including superposition, original horizontality, and lateral continuity. It also describes unconformities and how they represent gaps in the stratigraphic record. Sequence stratigraphy divides rock sequences into systems tracts based on bounding surfaces and stacking patterns. Sequences are bounded by unconformities and composed of parasequence sets, which are made up of genetically related beds bounded by flooding surfaces.
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This document provides an introduction to geology and its importance from a civil engineering perspective. It discusses the definitions and branches of geology, including mineralogy, petrology, geophysics, stratigraphy, physical geology, hydrogeology, and structural geology. The branches study minerals, rocks, the structure and evolution of the Earth, rock layers and ages, geological processes and landforms, groundwater, and rock structures. The document emphasizes the importance of geology for civil engineers for site selection, understanding construction materials and ground conditions, planning projects, and treating geological features like faults or joints that could impact stability. A foundation in the introduction to geology and key branches is important for civil engineers.
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Geology is the study of the Earth, including its composition, structure, physical properties, and history. It plays an important role in civil engineering by providing knowledge about soil and rock properties, which is necessary for foundation design, construction of highways, tunnels, and dams. The main branches of geology include physical geology, mineralogy, petrology, geomorphology, historical geology, economic geology, and others. Geology provides critical information for planning, designing, and constructing engineering projects and for mining activities.
1.pptx
This document provides an overview of an engineering geology course at Alzaiem Alazhari University. The course covers topics like the definition and importance of engineering geology, physical properties of soil and rocks, geological factors that affect engineering structures, and methods used in geological investigations and applications. Students will learn to understand engineering geology objectives, identify engineering problems with soil and rocks, use geological maps, and prepare reports using various geological methods. The course content includes introductions to physical geology, mineralogy, petrology, structural geology, and applications of geological investigations in areas like mining, landslides, and coastal protection. Students will be assessed through written exams, quizzes, tutorials, and assignments.
Introduction.ppt
Geology is the study of the Earth, its composition, structure and processes. It is important for civil engineering as it provides information about construction materials and site conditions. Geology helps in planning, design and construction of projects. It is also useful for mining engineering and groundwater resource development. Geology can be divided into physical geology and historical geology. The main branches of geology include mineralogy, petrology, structural geology, geomorphology, economic geology, stratigraphy, paleontology and paleogeography.
Engineering Geology Unit 1.pdf
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Geochemistry branches of geolchemistry.pptx
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WU_Engineering geology_lecture note_Elias.pdf
This document provides information about an Engineering Geology course at Wollo University in Ethiopia. It includes:
1. Basic details about the course such as the title, code, credit hours, instructors contact information.
2. The course aims to increase students' knowledge of applying geology principles to civil engineering projects.
3. Upon completing the course students will be able to conduct site investigations, prepare engineering geological maps, evaluate suitable sites for structures, identify construction materials, and assess/mitigate geological hazards for engineering structures.
4. The course outline covers topics such as site investigation, hazardous earth processes, subsurface water, dams, tunnels, river engineering, foundations, and geological mapping.
WU_Engineering geology_lecture note_Elias.pdf
This document provides information about an Engineering Geology course at Wollo University in Ethiopia. It includes:
1. Basic details about the course such as the title, code, credit hours, instructors contact information.
2. The course aims to increase students' knowledge of applying geology principles to civil engineering projects.
3. Upon completing the course students will be able to conduct site investigations, prepare engineering geological maps, evaluate suitable sites for structures, identify construction materials, and assess/mitigate geological hazards for engineering structures.
4. The course outline covers topics such as site investigation, hazardous earth processes, subsurface water, dams, tunnels, river engineering, foundations, and geological mapping.
Geography form 1 notes, kenya syllabus
Geography is the study of the Earth. There are two main branches: physical geography, which examines landforms and climate, and human geography, which studies human activities and settlements. Geography relates to other subjects like chemistry, physics, agriculture, biology and history.
The solar system consists of the Sun and objects that orbit it, like planets, asteroids, comets and moons. The Earth originated from a cloud of gas and dust about 4.6 billion years ago. It rotates on its axis and revolves around the Sun, causing day/night and seasons. Internally, it has a core, mantle and crust. Geography involves understanding our planet and its relationship to other celestial bodies.
1 introduction
This document provides information about the Engineering Geology and Seismology course CE-312 at UET Peshawar. It includes the instructor's contact information, course objectives to understand geologic factors that influence civil engineering projects and earthquakes, an overview of the engineering geology and seismology topics covered, recommended textbooks, grading criteria which includes exams, assignments, and a group project, and examples of what can happen when geology is ignored in civil projects or how geology can also be interesting to study.
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This document provides an overview of an introductory earth science course. It outlines course logistics, objectives, and topics including what geology is, practical applications, and the differences between physical and historical geology. It also briefly describes the origin of the universe, solar system, and Earth as well as plate tectonics theory and how it explains Earth's internal processes and dynamics.
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This document discusses engineering geological mapping and provides details on:
1) The purpose of engineering geological maps is to provide basic information for land use planning, engineering works planning/design/construction/maintenance, and environmental planning.
2) Engineering geological maps represent characteristics of rocks/soils, hydrogeological conditions, geomorphological conditions, and active geodynamic phenomena.
3) Classification of rocks and soils on maps is based on properties indicating physical/engineering characteristics, such as mineralogy, texture, structure, and weathering state.
Geological Survey Civil Engineering 3rd PDF
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INTRODUCTION TO GEOLOGY
This document provides an overview of the different branches of geology. It discusses the definition of geology as the study of the Earth, including its origin, structure, composition and history. Some of the key branches mentioned include physical geology, mineralogy, crystallography, petrology, structural geology, geophysics, stratigraphy, geochemistry, paleontology, historical geology, economic geology, mining geology, hydrogeology, geology of Pakistan, resources engineering, photo geology, remote sensing, engineering geology, and field geology. Each branch is studied to better understand different aspects of the Earth and its materials.
1 Unit-I Scope of Geology in Engineering
Geology is the study of the Earth, including its composition, structure, physical properties, history and the processes that shape it. It involves studying topics like the origin and age of the Earth, its internal structure, various surface features and how they evolve and change over time. Geology has many branches that study different aspects like physical geology, geomorphology, mineralogy, petrology, economic geology, geochemistry, geophysics, hydrogeology, mining geology, engineering geology and more. Civil engineers and geologists work closely together in areas like planning, designing and constructing major civil engineering projects to ensure their safety, stability and cost-effectiveness by understanding the geological conditions and properties of the construction site and materials.
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Introduction to Earth
Earth is composed of four main layers - crust, mantle, outer core, and inner core. The crust is the outermost layer and is made up of either continental or oceanic crust. Below the crust is the mantle, which is divided into lithosphere, asthenosphere, upper mantle, and lower mantle. The outer core is a liquid layer made of nickel and iron that generates Earth's magnetic field. The inner core is made of solid iron deep within Earth. Overall, Earth's composition is approximately 34.6% iron, 29.5% oxygen, and 15.2% silicon.
5.earthquake xi
The document discusses earthquakes, including their causes, measurement, effects, and zones of risk. Some key points:
- Earthquakes are caused by movement of tectonic plates and faults in rocks. Their magnitude is measured on the Richter Scale and their intensity by the Mercalli scale.
- Seismic waves transmit earthquake energy and are used to locate epicenters. The major earthquake zones are the Pacific Ring of Fire, Alpide Belt, and Mid-Atlantic Ridge.
- India has five seismic zones of risk. Zone V including Kashmir and Northeast India faces the highest risk, while Zone I including parts of central India faces the lowest risk.
4.faults
Faults are cracks or fractures in the Earth's crust caused by stresses that induce brittle deformation of rocks. There are three main types of faults: dip-slip faults which involve vertical motion, strike-slip faults with horizontal motion, and oblique-slip faults with an oblique motion. Normal faults occur during extension while reverse faults are caused by compression. The elastic rebound theory explains that tectonic plates accumulate energy during periods of stress until a sudden slip occurs along the fault, releasing energy in the form of seismic waves and causing earthquakes.
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providing crucial environmental data for scientific, resource management, policy purposes, and
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9
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Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
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Fundamentals of Geology
- 1. FUNDAMENTALS OF GEOLOGY A PON.RATHNAVEL PRESENTATION
- 2. WARM UP A WORD FORYOUR LETTER A pple K nowledge S kill H appy A ward Y outh A lways 2 8/31/2020 Add a footer
- 3. Objective • To understand the meaning of geology • To comprehend the different branches of geology • To take cognizance of applications of geology in civil engineering 3 8/31/2020 Add a footer
- 4. GEOLOGY • Geography vs Geology • Geology Geo (earth) + logy (scientific study) Geology = scientific study of the earth • Geology is defined as a scientific study of the earth as a planet which includes the study of origin, composition, structure, physical features, materials, interactions and physico – chemical processes operating within the earth. (OC SP MI PC) 4 8/31/2020 Add a footer
- 5. BRANCHES OF GEOLOGY 5 8/31/2020 Add a footer S. No. Branch Significance 1 Physical Geology Study of Structure of Earth and its various surface features 2 Historical Geology Study of origin of earth and changes in geology from past to present 3 Economic Geology Study of materials of earth that can be used for economic benefit of man 4 Petrology Study of rocks 5 Mineralogy Study of minerals 6 Geomorphology Part of Physical Geology - Study of land surface features 7 Geohydrology Part of Physical Geology - Study of water surface features 8 Meteorology Part of Physical Geology - Study of atmospheric features 9 Geochemistry Study of Chemical Composition of Earth, interaction of components and application of chemistry 10 Geophysics Study of application of physics to solve geology related issues 11 Engineering Geology Study of interaction between geology and engineering (mostly civil engineering)
- 6. APPLICATIONS IN CIVIL ENGINEERING 6 8/31/2020 Add a footer • BUILDINGS Foundation,Tall Buildings, Massive Buildings • INFRASTRUCTURE Water Resources – Dams, Canals • TRANSPORTATION Bridges,Tunnels, Railways, Airports, Docks, Harbours • ENVIRONMENT Environment Impact Assessment
- 7. THANKYOU