This note
explains the follolwing topics: Parameters of Structural Geology,
Mathematics of Structural Geology, Deformation Mapping, Deform. and
Displacement Gradients, Examples of Geological Deformation, The Displacement
Gradient, Rotational vs. Irrotational Strain, Strain Markers and Rock Strain,
Properties of Tensors, Introduction to Stress , The Force-Balance Problem, The
Mohr Circle and Earth Stress, Coulomb Failure Criterion, Microcracks and Shear
Fracturing,Stress Concentration, Crack Propagation and Jointing, Effective
Stress, Joint Patterns, Friction, Fault Rocks, Paleozoic Geology of the
Cordiller, Alpine Geology.
This page provides PDF links that covers the following topics
related to Geology : Introduction, history of the earth and geological time,
Minerals, The rock cycle and igneous rocks, Volcanism and volcanic rocks,
Sedimentary and metamorphic rocks , Glaciation and surficial deposits, History
of Plate Tectonics, Plate tectonics, Earthquakes.
This note explains the following topics:
Origins - Universe, Solar System and Earth, Earth Structure and Composition,
Continental Drift, Plate Tectonics, Minerals, Rocks and the Rock Cycle, Igneous
Rocks, Sedimentary Rocks, Metamorphic Rocks, The Hydrologic Cycle,Soils and Mass
Wasting/Mass Movement, Streams, Groundwater , Glaciers and Glaciation,
Volcanoes, Earthquakes, Mountains and Structures, Geologic Time, Fossils, Energy
Resourses.
This
course note introduces students to the basics of geology. It will addresses
topics ranging from mineral and rock identification to the origin of the
continents, from geologic mapping to plate tectonics, and from erosion by rivers
and glaciers to the history of life.
Author(s): Prof. Taylor Perron and Prof. Oliver Jagoutz
This note
explains the follolwing topics: Parameters of Structural Geology,
Mathematics of Structural Geology, Deformation Mapping, Deform. and
Displacement Gradients, Examples of Geological Deformation, The Displacement
Gradient, Rotational vs. Irrotational Strain, Strain Markers and Rock Strain,
Properties of Tensors, Introduction to Stress , The Force-Balance Problem, The
Mohr Circle and Earth Stress, Coulomb Failure Criterion, Microcracks and Shear
Fracturing,Stress Concentration, Crack Propagation and Jointing, Effective
Stress, Joint Patterns, Friction, Fault Rocks, Paleozoic Geology of the
Cordiller, Alpine Geology.
The aim of this note is to
provide a basic introduction to the geological and geophysical processes that
form and shape the ocean basins and their margins. Topics covered includes:
Seafloor Mapping, Understanding Conductive Cooling, Cooling of the Ocean Plates,
Evidence for Plate Tectonics from Magnetics, Global Seismology, Mantle Melting
and Phase Diagrams, Mid-Ocean Ridge Segmentation, Subduction Zones, Seismic
Hazards in the Pacific Northwest, Passive Margins and Sediment Transport,
Sequence Stratigraphy and Eustacy, Deep Sea Sedimentation and Paleoceanography.
This
book, like the others in the Series, is written in simple English the language
most widely used in science and technology. It provides an introduction to the
study of Earth science, but `Earth science' is interpreted differently in
different countries. In some regions of the Earth, such as on the Pacific
margins, it usually covers all the science relating to the Earth, including
geology, meteorology, oceanography, geomorphology and soil science. It therefore
covers much of physical geography in these regions, where geography is often not
a strong school subject. In other countries `Earth science' has a rather
narrower definition, largely covering only geology, whilst other aspects of
`Earth science' are covered in geography. Nevertheless, wherever on Earth this
book is being read, if you want to study `Earth science' in Higher Education, at
College or University, you will study mainly geology. So this book has been
written as an introductory guide to geology, to interest you in the subject and
to enthuse you to study geology at higher levels.
This is a book by the
Scottish geologist Charles Lyell. Lyell used geology throughout as a basis to
strengthen his argument for Uniformitarianism.This book explains the geological
state of the modern Earth by considering the long-term effects of observable
natural phenomena.
A sufficient number of leading facts has been introduced to enable
the learner to feel that every important principle is a conclusion to which he
has himself arrived; and yet, for the purpose of compression, that fullness of
detail has been avoided with which more extended works abound. In furtherance
of the same object, authorities are seldom cited.