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Издание 9
Автор(ы):Petersen M.S., Ritter S.M.
Издание:Waveland Press, 2023 г., 313 стр., ISBN: 978-1-4786-4897-0
Язык(и)Русский
Interpreting Earth history. A manual in historical geology / Интерпретация Земной истории. Руководство по исторической геологии

The discovery of “deep time” is one of geology’s greatest contributions to human understanding. The conceptual foundations laid by eighteenth- and nineteenth-century geologists working in relatively small geographic areas paved the way for development of the modern high-resolution geological timescale (figure 1.1), which spans 4.6 billion years of Earth history and applies to geological features anywhere on Earth.

Издание 3
Автор(ы):Hazelton P., Murphy B.
Издание:CSIRO, 2016 г., 200 стр., ISBN: 978-1486303960
Язык(и)Английский
Interpreting soil test results. What do all the numbers mean? / Интерпретация результатов анализа почвы. Что означают все эти цифры?

Soils are a valuable resource and a critical component in many of the environmental and economic issues facing society today. Understanding soil properties and soil behaviour and interpreting soil data are especially relevant for many environmental and land management issues facing the community. These issues include urban development, control of salinity, clearing of native vegetation, prevention of land degradation, control of water and wind erosion, irrigation development, the management of effluent disposal, contamination and the management of acid sulfate soils.

Автор(ы):Ray D.K.
Издание:Москва, 1979 г., 38 стр.
Язык(и)Английский
Interregional seminar on the development potential o precambrian mineral deposits / Межрегиональный семинар, посвященный потенциалу освоения докембрийских месторождений полезных ископаемых

The Precambrians of India are the principal sources of iron and manganese, base metal, gold and alloy metal ore deposits and a host of non-metallic substances of industrial use. A spectacular limeament divides the Indian peninsular shield into two contrasted segments. The southern segment is girdled by an Archean granulite belt. Inwards, gneissess and two distinct Greenstone-banded iron sequences span the Lower Proterozoic time and perhaps the Middle Proterozoic too. Upper Proterozoic platform cover rests unconformably on them in separate basins. In the northern segment the greenstone belts are not so distinct, and the Middle Proterozoic has a better development. Upper Proterozoic platform cover is more widespread. <...>

Автор(ы):Eisma D.
Издание:CRC Press, 1997 г., 541 стр., ISBN: 0-8493-8049-9
Язык(и)Английский
Intertidal deposits. River mouths, tidal flats and coastal lagoons / Приливно-отливные отложения. Устья рек, приливные отмели и прибрежные лагуны

This book is the outcome of experience, first with the Wadden Sea and later with other intertidal areas in the world visited by the author and co-authors, partly to do research, partly because of more personal interest and fascination. Intertidal areas can be important for many reasons besides scientific or economic ones, as the many activities testify that aim to keep intertidal areas in a (more or less) natural state.

Автор(ы):Scott J.
Издание:Paraninfo, Madrid, 1975 г., 120 стр., ISBN: 84-283-0709-1
Язык(и)Испанский (перевод с английского)
Introducción a la paleontologia / Введение в палеонтологию

La Paleontología es una ciencia notablemente compleja, que abarca todos los problemas relacionados con los seres vivos, referidos a épocas pasadas, en su sentido más amplio y, al mismo tiempo, sus implicaciones geológicas, toda vez que los fósiles asociados a las rocas sedimentarias, constituyen el elemento básico para determinar su edad geológica <...>

Автор(ы):Sanders I.
Издание:Dunedin, London, 2018 г., 160 стр., ISBN: 9781780460642
Язык(и)Русский
Introducing Metamorphism / Введение в метаморфические процессы

Metamorphism (from the Greek words meta = change and morphos = form) is a geological process that changes pre-existing igneous and sedimentary rocks into new rocks – metamorphic rocks – that look quite different from the rocks they started out as. Metamorphism can even change pre-existing metamorphic rocks into new, and different looking, metamorphic rocks. When rocks are changed like this they are said to become metamorphosed, but one should note that the related word metamorphosis has no place in geology. It applies to other kinds of change, such as from a tadpole to a frog, and is not a synonym for metamorphism.

Издание 6
Автор(ы):Strahler A.
Издание:Wiley, 2013 г.
Язык(и)Английский
Introducing Physical Geography / Введение в физическую географию

This easy-to-use website features animations, videos, and interactive exercises, making it possible to quickly reinforce and illustrate key concepts from the text. Students can use these resources for tutorials, as well as a self-quizzing device to complement the textbook and enhance their understanding of geography. Easy integration of this content into course management systems and homework assignments enables instructors to conveniently integrate multimedia with their syllabi and more traditional reading and writing assignments. <...>

Автор(ы):Park G.
Издание:Dunedin Academic Press Ltd, 2012 г., 148 стр., ISBN: 978-1906716264
Язык(и)Английский
Introducing tectonics, rock structures and mountain belts / Знакомство с тектоникой, горными структурами и горными поясами

Meaning and scope of the terms ‘tectonic’ and ‘structure’ The adjective ‘tectonic’ merely means ‘structural’, i.e. applying to a structure. However, in geological usage it has come to be applied particularly to large-scale structures – thus ‘tectonic plate’. In order to explain rock structures, it is necessary to understand the forces operating within and on the crust that are responsible for creating them, and to do this, we need to investigate the Earth-scale processes known collectively as plate tectonics. The term ‘structure’ in everyday usage refers normally to a building or other artificial construction, but in geological terms it has come to mean a body of rock whose shape can be defined geometrically and which has originated by a geological process.

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