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It is the technical specialty that deals with soil and rock as supporting materials for structures.
It is the technical specialty that deals with soil and rock as supporting materials for structures.
- Geotechnical Engineering (correct)
- Structural Engineering
- Foundation Engineering
- Geological Engineering
It deals with the application of geologic fundamentals to engineering.
It deals with the application of geologic fundamentals to engineering.
- Engineering Geology (correct)
- Geology
- Geotechnical Engineering
- Soil Science
It is basic science that is concerned with the study of the history of the Earth, the rocks of which it is composed and the changes that it has undergone or is undergoing.
It is basic science that is concerned with the study of the history of the Earth, the rocks of which it is composed and the changes that it has undergone or is undergoing.
- Geotechnical Engineering
- Soil Science
- Engineering Geology
- Geology (correct)
These are formed from rock as it is acted upon by physical, chemical, and biological forces.
These are formed from rock as it is acted upon by physical, chemical, and biological forces.
It is a phenomenon by which the soil on the downstream sides of some hydraulic structures gets lifted up due to excess pressure of water.
It is a phenomenon by which the soil on the downstream sides of some hydraulic structures gets lifted up due to excess pressure of water.
It serves as parent material for natural soil formation.
It serves as parent material for natural soil formation.
Molten solution where igneous rocks came from.
Molten solution where igneous rocks came from.
They form when sediments undergone compaction and cementation.
They form when sediments undergone compaction and cementation.
This is the ability to resist sliding along internal surfaces within a mass.
This is the ability to resist sliding along internal surfaces within a mass.
They form when rocks undergone weathering and erosion.
They form when rocks undergone weathering and erosion.
This is the study of physical properties like density and magnetism of the earth or its parts.
This is the study of physical properties like density and magnetism of the earth or its parts.
It is a general term used when the surface of the earth is worn away by the chemical as well as mechanical actions of physical agents and the lower layers are exposed
It is a general term used when the surface of the earth is worn away by the chemical as well as mechanical actions of physical agents and the lower layers are exposed
It deals with the application of geological knowledge in the field of mining.
It deals with the application of geological knowledge in the field of mining.
It is the study of the ways in which rocks or sediments are arranged and deformed on the earth.
It is the study of the ways in which rocks or sediments are arranged and deformed on the earth.
It is the process of simply removing the loose sand and dust sized particles from as area, by fast moving winds.
It is the process of simply removing the loose sand and dust sized particles from as area, by fast moving winds.
This is a two-dimensional view of rock distribution.
This is a two-dimensional view of rock distribution.
The subject concerned with the study of the response of rock to an applied disturbance caused by natural or engineering processes.
The subject concerned with the study of the response of rock to an applied disturbance caused by natural or engineering processes.
It is a view of a vertical slice of the earth
It is a view of a vertical slice of the earth
This branch is relatively more recent and deals with the occurrence, distribution, abundance, mobility etc, of different elements in the earth crust.
This branch is relatively more recent and deals with the occurrence, distribution, abundance, mobility etc, of different elements in the earth crust.
These are defined as wavy undulations developed in the rocks of the Earth's crust due to horizontal compression resulting from gradual cooling of the Earth's crust, lateral deflection and intrusion of magma in the upper strata
These are defined as wavy undulations developed in the rocks of the Earth's crust due to horizontal compression resulting from gradual cooling of the Earth's crust, lateral deflection and intrusion of magma in the upper strata
The finest particles of dust travelling in suspension with the wind are transported to a considerable distance,
The finest particles of dust travelling in suspension with the wind are transported to a considerable distance,
This is where the continuity of the rock mass breaks
This is where the continuity of the rock mass breaks
These are fractures in crustal strata along which appreciable shear displacement of the adjacent rock blocks have occurred relative to each other, probably due to tectonic activities.
These are fractures in crustal strata along which appreciable shear displacement of the adjacent rock blocks have occurred relative to each other, probably due to tectonic activities.
The fracture along which the shear displacement has taken place
The fracture along which the shear displacement has taken place
It is a branch of mechanics that studies the mechanical properties of various types of soil and its strength at different moisture-content levels.
It is a branch of mechanics that studies the mechanical properties of various types of soil and its strength at different moisture-content levels.
He is the Father of Modern Soil Mechanics.
He is the Father of Modern Soil Mechanics.
These are highly permeable are compressed in a relatively short period of time as compared to cohesive soils which are less permeable
These are highly permeable are compressed in a relatively short period of time as compared to cohesive soils which are less permeable
It involves a gradual compression occurring simultaneously with a flow of water out of the mass and with a gradual transfer of the applied pressure from the pore water to the mineral skeleton
It involves a gradual compression occurring simultaneously with a flow of water out of the mass and with a gradual transfer of the applied pressure from the pore water to the mineral skeleton
It is defined as the ratio of an earthquake based on actual effects produced by the quakes on the earth.
It is defined as the ratio of an earthquake based on actual effects produced by the quakes on the earth.
The process opposite to consolidation
The process opposite to consolidation
The field and laboratory investigations required to obtain the essential information on the subsoil
The field and laboratory investigations required to obtain the essential information on the subsoil
They exist in nature and are formed by natural causes.
They exist in nature and are formed by natural causes.
The point which is diametrically opposite to the epicenter
The point which is diametrically opposite to the epicenter
This is the steepest inclination of the plane to horizontal
This is the steepest inclination of the plane to horizontal
It is the trace of the dipping plane with the horizontal reference plane. It is also the orientation of the horizontal line drawn on the dipping plane
It is the trace of the dipping plane with the horizontal reference plane. It is also the orientation of the horizontal line drawn on the dipping plane
They look like a new moon in plan are of most common occurrence.
They look like a new moon in plan are of most common occurrence.
This is the interface between a superstructure and its supporting soil.
This is the interface between a superstructure and its supporting soil.
This is the inclination of any arbitrary line on the plane to horizontal, which is always less than the true dip
This is the inclination of any arbitrary line on the plane to horizontal, which is always less than the true dip
It is the study of different types of foundation and their proper applications.
It is the study of different types of foundation and their proper applications.
It normally comprises two footings connected by a beam
It normally comprises two footings connected by a beam
It is a long footing supporting two or more columns in one row.
It is a long footing supporting two or more columns in one row.
It is a large footing, usually supporting several columns in two or more rows.
It is a large footing, usually supporting several columns in two or more rows.
It is defined as the process of breaking up of rocks into small pieces by the mechanical agencies of physical agents.
It is defined as the process of breaking up of rocks into small pieces by the mechanical agencies of physical agents.
It is defined as that of applied sciences which deals with the application of geology for a safe, stable land economical design and construction of a civil engineering project.
It is defined as that of applied sciences which deals with the application of geology for a safe, stable land economical design and construction of a civil engineering project.
It deals with different physical features of the earth, such as mountains, plateaus, valleys, rivers, lakes, glaciers, and volcanoes in terms of their origin and development.
It deals with different physical features of the earth, such as mountains, plateaus, valleys, rivers, lakes, glaciers, and volcanoes in terms of their origin and development.
This deals with the study of minerals.
This deals with the study of minerals.
It deals with the study of rocks
It deals with the study of rocks
It deals with occurrence, movement and nature of groundwater in an area.
It deals with occurrence, movement and nature of groundwater in an area.
It is defined as a process of decay, disintegration and decomposition of rocks under the influence of certain physical and chemical agencies.
It is defined as a process of decay, disintegration and decomposition of rocks under the influence of certain physical and chemical agencies.
These are the elongated ridges of sand with their longer axis broadly parallel to the direction of the prevailing wind.
These are the elongated ridges of sand with their longer axis broadly parallel to the direction of the prevailing wind.
It is defined as the process of breaking up of mineral constituents to form new components by the chemical actions of the physical agents.
It is defined as the process of breaking up of mineral constituents to form new components by the chemical actions of the physical agents.
It is the chemical reaction between gases of the atmosphere and minerals of the rocks
It is the chemical reaction between gases of the atmosphere and minerals of the rocks
It occurs when living organisms break up rocks
It occurs when living organisms break up rocks
It is the reaction of oxygen with chemicals in a rock.
It is the reaction of oxygen with chemicals in a rock.
It is a process in which a rock absorbs water into its chemical structure.
It is a process in which a rock absorbs water into its chemical structure.
This is a combination of those two representations and gives a 3-D view of formations and contacts.
This is a combination of those two representations and gives a 3-D view of formations and contacts.
It is caused by carbonic acid in water reacting with and degrading rock.
It is caused by carbonic acid in water reacting with and degrading rock.
This is a fracture where little or no movement has taken place
This is a fracture where little or no movement has taken place
It is caused by sulphur and nitrogen compounds in the air reacting with water to form acids that then fall to the ground.
It is caused by sulphur and nitrogen compounds in the air reacting with water to form acids that then fall to the ground.
These are huge heaps of sand formed by the natural deposition of windblown sand sometimes of characteristics and recognizable shape.
These are huge heaps of sand formed by the natural deposition of windblown sand sometimes of characteristics and recognizable shape.
The interaction between soils and percolating water
The interaction between soils and percolating water
Flashcards
Geotechnical Engineering
Geotechnical Engineering
Deals with soil and rock as supporting materials for structures.
Engineering Geology
Engineering Geology
Applies geologic fundamentals to engineering projects.
Geology
Geology
Concerns the history of the Earth and rocks.
Soil
Soil
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Magma
Magma
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Sedimentary Rocks
Sedimentary Rocks
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Geophysics
Geophysics
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Mining Geology
Mining Geology
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Structural Geology
Structural Geology
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Deflation
Deflation
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Map View
Map View
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Rock Mechanics
Rock Mechanics
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Geochemistry
Geochemistry
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Folds
Folds
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Loess
Loess
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Fracture
Fracture
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Faults
Faults
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Soil Mechanics
Soil Mechanics
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Disintegration
Disintegration
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Decomposition
Decomposition
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Study Notes
- Deals with soil and rock as supporting materials for structures: Geotechnical Engineering
- Applies geologic fundamentals to engineering: Engineering Geology
- Studies Earth's history, rocks, and changes: Geology
- Soil forms from rock due to physical, chemical, and biological forces
- Piping occurs when soil lifts due to excess water pressure
- Mineral serves as parent material for natural soil formation
- Magma is the molten solution for igneous rocks
- Sedimentary rocks form when sediments undergo compaction and cementation
- Shear strength provides resistance to sliding within a mass
- Sediments form when rocks experience undergoing through weathering and erosion
- Study of the Earth's physical properties like density and magnetism: Geophysics
- Weathering is the wearing away of Earth's surface by chemical and mechanical actions
- Application of geological knowledge in mining: Mining Geology
- Study of rock and sediment arrangement and deformation: Geology
- Deflation is removing particles by wind
- A two-dimensional view of rock distribution: Map View
- Study of rock response to disturbance: Rock Mechanics
- A Geologic cross-section is a view of a vertical slice of the earth
- Deals with element occurrence, distribution, and mobility in Earth's crust: Geochemistry
- Wavy undulations in rocks from horizontal compression: Folds
- Loess are fine dust particles carried by the wind over long distances
- Fractures indicate breaks in rock mass continuity
- Faults are fractures with shear displacement due to tectonic activity
- Fault Plane is the fracture along which shear displacement occurs
- Branch of mechanics studying soil properties and strength: Soil Mechanics
- Karl Terzaghi is the Father of Modern Soil Mechanics
- Cohesionless soils are highly permeable and compress quickly
- Consolidation is gradual compression with water flow and pressure transfer
- Magnitude is the ratio of an earthquake based on actual effects
- Swelling is the process opposite to consolidation
- Soil Exploration gets information of the subsoil
- Natural Slopes exist and are formed by natural causes
- The Anticenter point is diametrically opposite to the epicenter
- True Dip is the steepest inclination of a plane to horizontal
- Strike is the trace of a dipping plane with the horizontal reference plane (orientation of horizontal line)
- Barchans are new moon shaped (in plan) and commonly occur
- Interface between a superstructure and its supporting soil: Foundation
- The Apparent Dip is the inclination of any arbitrary line on a plane to horizontal, always less than the true dip
- Different types of foundation and their applications: Geotechnical engineering
- Combined Footing comprises two footings connected by a beam
- A long footing supporting multiple columns in one row: Combined Footing
- A large footing supporting several columns in multiple rows: Mat Foundation
- Disintegration involves breaking rocks into small pieces by mechanical agents
- Engineering Geology is applied geology for safe and economical civil engineering design and construction
- Physical Geology studies Earth's physical features and their development
- Petrology is the study of rocks
- Geohydrology covers groundwater occurrence, movement, and nature
- Weathering involves decay, disintegration, and decomposition of rocks by physical and chemical agencies
- Barchans are elongated ridges of sand parallel to wind direction
- Breaking mineral constituents to form components by chemical actions: Decomposition
- Chemical Weathering the reaction between gases and minerals
- Biological Weathering the act of organisms breaking up rocks
- Reaction of oxygen with rock chemicals: Oxidation
- Hydrolysis is the rock absorbs water into its chemical structure
- Combination giving a 3-D view of formations and contacts: Block Diagram
- Carbonic acid in water reacting with and degrading rock causes Carbonation
- A fracture where little or no movement has taken place is called a Joint
- Acid Rain from air pollutants reacting with water
- Huge heaps of windblown sand with recognizable shape are called Sand Dunes
- Interaction between soils and percolating water called Consolidation
- Rock Engineering applies engineering geology and rock mechanics economically
- Transverse Dunes similar to barchans/curved transverse to wind
- Earthquake Magnitude: the rating based on energy released from rocks rebounding
- Tectonic Earthquakes originate from crystal block movement on faulting
- Non-Tectonic Earthquakes arise from volcanic eruptions or landslides
- An earthquake's origin spot beneath the surface: Focus
- Point where earthquake first reaches the surface (above the focus): Epicenter
- Climatic/geological changes known from investigations: Stratigraphy
- Physical Weathering a breakdown of rock masses under atmospheric agents
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