The application of geology for a safe, stable and economic design and construction of a civil engineering project
Branches of Geology
Physical Geology
Crystallography
Mineralogy
Petrology
Physical Geology
Deals with the various agents that modify the face of the Earth
Includes the study of Erosion, Transportation and Deposition (ETD)
Plays a vital role in collecting a suitable basis for different types of foundations and in the study of the effects of the earth's processes on civil engineering structures
Crystallography
Deals with the study of crystals
Not much important to civil engineering, but necessary to recognize the minerals
Mineralogy
Deals with the study of minerals
Most important for a civil engineering student to identify the rocks
Important in industries such as cement, iron and steel, fertilizers, glass industry and in the production of atomic energy
Petrology
Deals with the study of rocks
Most important for a civil engineer in the selection of suitable rocks for building stones, road metals, etc.
Structural Geology
A branch of geology that deals with the study of structures found in rocks. Also known as tectonic geology or tectonics.
Structural Geology
It plays an important role in civil engineering in the selection of suitable sites for all types of projects such as dams, tunnels, multistoried buildings, etc.
Mining Geology
A branch of geology that deals with the application of geology to mining engineering in such a way that the selection of stable sites for quarrying and mines can be determined.
Civil Engineering Geology
A branch of geology that deals with all the geological problems that arise in the field of civil engineering along with suitable treatment. It includes the construction of dams, tunnels, mountain roads, building stones and road metals.
The average distance from the Earth to the Sun is 92,956,050 miles (149,598,262 km)
The length of a solar day (single rotation on Earth's axis) is 23.934 hours
The Earth is about 4.54 billion years old
Biosphere
The part of Earth that supports life (biota-animals, plants and microorganisms) includes water, rock and soil of the earth's crust, and the atmosphere.
Lithosphere
The rocky material of the Earth's outer shell from the surface to about 100 km deep
Layers of Lithosphere
Crust
Mantle
Core
Hydrosphere
The body of liquid on or near the surface of the Earth
Atmosphere
The gaseous blanket where important gases circulate
Chemical Composition of the Atmosphere (Dry Air)
Nitrogen (78.084%)
Oxygen (20.546%)
Argon (0.934%)
Carbon Dioxide (0.0407%)
Others (Neon, Helium, etc.)
Layers of Atmosphere
Troposphere
Stratosphere
Mesosphere
Thermosphere
Exosphere
Troposphere
The lowest major atmospheric layer, located from Earth's surface up to the bottom of the stratosphere. It extends upward to about 10km (6.2 miles or about 33,000 feet) above sea level. Humans live in this layer.
Stratosphere
The layer where the ozone layer is found. It absorbs high-energy ultraviolet from the sun. Commercialpassengerjets fly in this layer.
ContinentalDrift
The large-scale horizontal movements of continents relative to one another and to the ocean basins during one or more episodes of geologic time. This concept was an important precursor to the development of the theory of plate tectonics.
The 7 Continents
North America
South America
Antarctica
Europe
Asia
Africa
Australia
Plate Tectonics
The theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle.
The 9 Major Plates
North American Plate
Pacific Plate
Eurasian Plate
African Plate
Indo-Australian Plate
Indian Plate
South American Plate
Australian Plate
Antarctic Plate
Earth's Processes
InternalProcesses
SurfaceProcesses
Internal Processes
Processes that originate deep in the Earth's interior, such as earthquakes and volcanism.
Surface Processes
Processes that affect the Earth's surface, mostly driven by water, wind, and gravity.
Uniformitarianism
The theory that Earth's features are mostly accounted for by gradual, small-scale processes that occurred over long periods of time.
Catastrophism
The theory that Earth's features are mostly accounted for by violent, large-scale events that occurred in a relatively short amount of time.
Earthquake
Sudden shaking or trembling of the ground caused by the sudden breakage or slippage of large rock masses below or at the surface of the earth
Violent earthquakes release energy which is about 10,000 times of an atomic bomb
Foreshocks
Tremors that occur before the main earthquake
Aftershocks
Tremors that occur after the main earthquake, may happen for a few days or few weeks
Types of earthquake
Tectonicearthquake - caused by movements in the earth's crust
Volcanicearthquake - movement of molten material or by gas pressure under a volcano
Focus
Location where the earthquake begins
Epicenter
Point on the earth's surface located directly above the focus of an earthquake
Plate tectonics
Theory that the earth's crust and the upper mantle, which together form the lithosphere, is broken into large and smaller plates
These plates are moving around, and their movements cause changes in the earth's crust