It providesknowledge about materialsusedforconstruction
Its knowledgeishelpfulforconstructingDams
GeotechnicalEngineers needs knowledge about this subject for excavation
Its knowledge is required for foundationfaults
For design of highway and roads
Construction of Tunnels
Soil Testing
RiverControl and ShippingWork
Geology
The study of earth. It deals with the study of origin, age, interior structure, history of earth
Geology also
Tells us the evolution and modification of various surface features like rivers, mountains, and lakes
Branches of Geology
Physical Geology
Mineralogy
Petrology
Structural Geology
Historical Geology
Paleontology
Economic Geology
Physical Geology
Also called as Dynamic Geology or Geomorphology
Deals with the different Physical feature of the earth such as Mountains, Rivers, Lakes, Glaciers, and Volcanoes
It also deals with different changes occurs on earth surface like marine, formation or disappearance of rivers, spring, and lakes
Mineralogy
Deals with the study of Minerals
Also deals with the detailed mode of formation, composition, occurrence, types, association properties used and etc.
Mineral
A naturally occurring substance with distinctive chemical and physical properties, composition, and atomic structure
Rock
Generally made up of two or more minerals, mixed up through geological processes
Petrology
Deals with the study of Rocks
The earth crust which is also called Lithosphere, is made up of different types types of rocks
Deals with the formation, structure, texture, composition, occurrence, and types etc.
Structural Geology
Rocks which forms the earth's crust undergoes various deformation, dislocations and disturbances under the influence of tectonic plates forces
Study of rock's deformation
Historical Geology
Kind of study of earth's history through sedimentary rocks
Sedimentary rocks are one of three main types of rocks, along with igneous and metamorphic. They are formed on or near the Earth's surface from the compression of ocean sediments or other processes
Paleontology
The study of ancient life, from dinosaurs to prehistoric plants, mammals, fish, insects, fungi, and even microbes
Fossil evidence reveals how organisms changed over time and what our planet was like long ago
Economic Geology
The scientific study of mineral resources and the application of such knowledge in mineral exploration and mining
Historical geology
Discipline that uses the principles and methods of geology to reconstruct the geological history of Earth
Historical geology
Studies the idea of geologic time, the evolution of plant and animal evidence found in the rock record, and the historical development of the rock units that comprise the Earth's crust
Includes study of stratigraphy and paleontology
Our planet was formed from the solar nebula, a cloud of gas and dust
Determining the age of the Earth
1. Relative dating methods such as stratigraphy
2. Radiometric dating using radioactive elements
Scientists have estimated the age of the Earth to be 4.5 billion years
Biblical Estimates
In medieval Europe, the Bible, particularly the book of Genesis, served as the foundation for understanding the Earth's age, with a timeframe of approximately 6,000 years
Bernard Palissy observed that erosion caused by rain and winds could not have resulted in rapid geological changes, suggesting the Earth was much older than 6,000 years
James Hutton observed that Hadrian's Wall had not eroded significantly despite being in place for over 1600 years, corresponding with Palissy's views
Evolution
The process by which different kinds of living organisms are thought to have developed and diversified from earlier forms during the history of the earth
Darwinism
The theory of the evolution of species by natural selection advanced by Charles Darwin
Natural Selection
A mechanism of evolution that ensures only the traits that help a species survive and reproduce get passed on to future generations
Nicolas Steno
Danish scientist, pioneer in both anatomy and geology, first to observe and propose a number of basic principles of historical geology, including the law of superposition, the principle of original horizontality, and the principle of lateral continuity
Law of superposition
Layers of sediments are originally deposited horizontally under the action of gravity
Principle of original horizontality
Layers of sediment are initially deposited horizontally
Principle of lateral continuity
Layers of sediment initially extend laterally in all directions
William Smith
Father of English Geology, established the first Geological map of England
James Hutton
Scottish geologist, often referred to as the "Father of Modern Geology", proposed the theory of uniformitarianism
Uniformitarianism
The Earth was formed by the same natural phenomena that are at work today, the product of slow and continuous geological changes
Charles Lyell
Scottish geologist who expanded upon Hutton's concept of uniformitarianism
Plate Tectonics
The scientific theory that Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since about 3.4 billion years ago
Methods used to tell the sequence of geological events
Stratigraphy
Structural geology
Paleontology
Sedimentology
Stratigraphy
Branch of geology concerned with the study of rock layers (strata) and layering (stratification), primarily used in the study of sedimentary and layered volcanic rocks
Stratigraphy
Combines the Latin word Stratum with the Greek word Graphia
Deals with the arrangement and succession of strata, as well as the origin, composition and distribution of these geological strata through time and space
Subfields of Stratigraphy
Lithostratigraphy
Biostratigraphy
Chronostratigraphy
Magnetostratigraphy
Allostratigraphy
Geochronology
Seismic Stratigraphy
Lithostratigraphy
The study of strata or rock layers based on their physical and petrographic characteristics
Biostratigraphy
Focuses on correlating and assigning relative ages of rock strata by using the fossils assemblages contained within them
Chronostratigraphy
Studies the ages of rock strata in relation to time, involves comparing which rocks originated globally at the same time