This note deals with the application
of geological and related principles to the solution of various types of crimes.
Topics covered includes: The Case of the Sandy Body, Characterizing Sand,
Characterizing Minerals, Characterizing Rocks, Using Pigments to Identify Art
Fraud, Demise of the Ice Man, Radioactive Isotopes, Stable Isotopes.
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
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.
This book
relates fractals and chaos to a variety of geological and geophysical
applications. This book contains eight chapters showing the recent
applications of the fractal or mutifractal analysis in geosciences. Two chapters
are devoted to applications of the fractal analysis in climatology, two of them
to data of cosmic and solar geomagnetic data from observatories. Four chapters
of the book contain some applications of the (multi-) fractal analysis in
exploration geophysics.
New Theory of the Earth, is a book written by Don L. Anderson. This
is an interdisciplinary advanced textbook on all aspects of the interior of the
Earth and its origin, composition, and evolution: geophysics, geochemistry,
dynamics, convection, mineralogy, volcanism, energetics and thermal history.
This is the only book on the whole landscape of deep Earth processes that ties
together all the strands of the subdisciplines.
This book explains about the earth and its
evolution.Also describes planetary formation theories and builds a model of what
early earth could of looked like, subtley using the scientific method and asking
and answering questions every step of the way.
IN these days of specializing in "
watertight compartments," the bearing of geology in relation to almost every
branch of engineer-ing is very frequently neglected or ignored. A knowledge of
geology is, however, of the first importance to the practical engineer, but it
is difficult for him to study the application of this
science to his requirements without having recourse to a large number of
different textbooks and other works. References to geology which are often of
the greatest practical importance are often almost hidden away or treated in an
obscure fashion, where- as the engineer requires the needful information to be
put before him in a clear and concise manner. To meet this want I have endeavoured to compile the requisite information in one volume, in the hope that
it may serve as a handy book of reference. GEOLOGY is the science which
investigates the history of the earth. It treats of the nature and formation of
the rocks which form the solid framework of the globe ; of the agents which
produce changes in these rocks ; and of the history of the past life, whose
remains (fossils) are buried in them.