Historical Geology is the study of analyzing Earth's past by investigating rocks and the information found in them
Understand the concept of geology
Engineering geology deals with the study of the structure of the earth in relation to civil engineering for the execution of safe and cost-effective design for construction projects
Structure of Earth and Composition - Composition of Mantle
Conduction – heat transfer that occurs through rapid collision of atoms. It happens if the material is solid
Convection – material that can move and flow may develop convection energy
Upper Mantle - Primarily composed of silicate minerals, including olivine and pyroxene
Transition zone - A region in the mantle where high-pressure conditions lead to changes in mineral structures
Lower Mantle - Composed of silicate minerals in a solid state due to high pressures, even though temperatures are elevated
Know the relation of geology to civil engineering
Our planet’s structure is composed of a variety of elements and compounds
Why Is Geology so Important to Civil Engineers?
1. Collect preliminary information from already existing data about the site
2. Completing a geological survey of the site
3. Compiling all data from the survey about geology underneath the surface to form hypotheses
4. Conduct drilling and boring projects to authenticate geological hypotheses
5. Conducting tests on soils and rocks from the proposed site to examine where the land is suitable for the project
Structure of Earth and Composition
Crust
Outer Core
Mantle
Inner Core
Physical Geology is the study of the solid Earth and the processes that change the physical landscape of the planet
Geology is a very broad field that can be divided into many more specific branches
Structure of Earth and Composition - Mantle
Mantle is made of solid rocks
Mantle is hot
Surveying requires civil engineers to determine the relative positions of points that are at, above, and below the surface of the earth
Structure of Earth and Composition - Crust
Continental Crust – mainly composed of granite
Oceanic Crust - primarily composed of basalt
Contents of the Presentation
Geology in Civil Engineering
Branches of Geology
Earth Structure and Composition
Elementary Knowledge on Continental Drift and Plate Tectonics
Earth Processes
Weathering
Work of Rivers, Wind and Sea and Engineering Importance
Origin and Occurrence of Earthquake
Mode of Occurrence of Earthquake
Earthquake Prospecting
Ground Water
Why Is Geology so Important to Civil Engineers?
Environmental Geology is the study of the interaction between humans and the geological environment
Structure of Earth and Composition - Oceanic Crust vs. Continental Crust
Composed mainly of dark-colored and mafic rocks
Composition: Predominantly composed of light-colored and felsic rocks
Thickness: Oceanic Crust - Typically around 7 km (4 miles), Continental Crust - Ranges from about 20 to 70 km (12 to 43 miles)
Density: Oceanic Crust - 3.00 grams per cubic meter, Continental Crust - 2.7 grams per cubic meter
Branches of Geology
Physical Geology
Historical Geology
Environmental Geology
Researchers discovered that earthquakes tended to occur in specific places rather than equally all over Earth using a seismometer
According to Alfred Wegener's theory, Pangaea was once a supercontinent that included all landmasses, and the current continents moved to their current locations through continental drift
Lower Mantle is composed of silicate minerals in a solid state due to high pressures, even though temperatures are elevated
Geologists expanded their understanding of the Earth throughout the 20th century by making observations in the ocean basins and utilizing new tools and methods
Transition zone is a region in the mantle where high-pressure conditions lead to changes in mineral structures
Strain results from stress, causing a change in shape of an object
Alfred Wegener was a German explorer and climatologist who proposed the theory of continental drift
Landforms are formed on the Earth’s surface after natural occurrences, making up terrains such as mountains, valleys, plains, plateau, ocean basins, and mid-ocean ridges
Chemical weathering is a geological process that alters the composition of rocks and minerals through chemical reactions
Deposition is the laying down of sediment carried by wind, flowing water, the sea, or ice
Stress is the force applied on an object, resulting in compressive stress, tensile stress, or shearing stress
Mechanical weathering is a natural process that breaks down rocks into smaller fragments without changing their chemical composition
Silicate minerals
olivine
pyroxene
Erosion involves the movement of fragments, distinguishing it from weathering, which focuses on in situ decay
Plate Tectonics is the study of large-scale movement and deformation of the outer layers of the Earth
Outer Core
Primarily composed of liquid iron and nickel
The movement of molten metal in the outer core generates the Earth’s magnetic field through a process called the GEODYNAMO
The asthenosphere and lithosphere convect, causing the plates to move apart at varying speeds of two to fifteen centimeters per year
Wegener found three main pieces of evidence for continental drift
Geologic
Fossil
Climate
A magnetometer helped find evidence of surprising magnetic variations near undersea ridges, showing alternating stripes of rock recording a flip-flopping of Earth’s magnetic field