Business and Economics

The Economic Aspect of Geology

Unveiling the Economic Influence of Geological ForcesBy C. K. Leith

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Length19h 33m

About this audiobook

In "The Economic Aspect of Geology," C. K. Leith explores the intricate relationship between geological principles and economic development, synthesizing scientific rigor with practical application. This seminal work employs a clear, analytical literary style conducive to both academic inquiry and lay understanding, placing geology within the broader socio-economic context. Leith's investigation spans mineral resources, energy production, and land use, offering readers insights into the geological foundations that underpin industrial growth and societal advancement, making it a pivotal text for geologists, economists, and policy-makers alike. C. K. Leith, a prominent geologist and educator, was instrumental in advancing the understanding of geology's economic implications during a time of significant industrial expansion. His diverse experiences, including field studies and work with governmental and educational institutions, shaped his perspective on the vital role of geology in resource management. Leith's commitment to connecting scientific disciplines with practical decision-making reflects the pressing needs of his era and leads him to produce works that are still relevant today. This book is highly recommended for readers seeking a deeper comprehension of how geological factors influence economic landscapes. Whether you are a student, academic, or professional in related fields, Leith'Äôs insightful analysis provides essential perspectives that encourage critical thinking about the sustainable use of Earth's resources and the interconnectedness of our economic systems.

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Audiobook details

GenreBusiness and Economics

Length19 hrs 33 mins

Narrated byListen with 1,000+ voices

FormateBook with Audio

Publish dateDec 6, 2019

LanguageEnglish

1CHAPTER I

2INTRODUCTION

3SURVEY OF FIELD

4ECONOMIC APPLICATIONS OF THE SEVERAL BRANCHES OF GEOLOGY AND OF OTHER SCIENCES

5Mineralogy and Petrology

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6Stratigraphy and Paleontology

7Structural Geology

8Physiography

9Rock Alterations or Metamorphism

10Application of Other Sciences

11TREATMENT OF THE SUBJECT IN THIS VOLUME

12CHAPTER II

13THE COMMON ELEMENTS, MINERALS, AND ROCKS OF THE EARTH AND THEIR ORIGINS

14RELATIVE ABUNDANCE OF THE PRINCIPAL ELEMENTS OF THE LITHOSPHERE

15RELATIVE ABUNDANCE OF THE PRINCIPAL MINERALS OF THE LITHOSPHERE

16RELATIVE ABUNDANCE OF THE PRINCIPAL ROCKS OF THE LITHOSPHERE

17Soils and Clays

18Water (Hydrosphere)

19COMPARISON OF LISTS OF MOST ABUNDANT ROCKS AND MINERALS WITH COMMERCIAL ROCKS AND MINERALS

20THE ORIGIN OF COMMON ROCKS AND MINERALS

21Igneous Processes

22Weathering of Igneous Rocks and Veins

23Sedimentary Processes

24Weathering of Sedimentary Rocks

25Consolidation, Cementation, and Other Subsurface Alterations of Rocks.

26THE METAMORPHIC CYCLE AS AN AID IN STUDYING MINERAL DEPOSITS: FOOTNOTES:

27CHAPTER III

28SOME SALIENT FEATURES OF THE GEOLOGY AND CLASSIFICATION OF MINERAL DEPOSITS

29VARIOUS METHODS OF CLASSIFICATION

30NAMES

31MINERAL DEPOSITS AS MAGMATIC SEGREGATIONS IN IGNEOUS ROCKS

32MINERAL DEPOSITS WITHIN AND ADJACENT TO IGNEOUS ROCKS WHICH WERE FORMED IMMEDIATELY AFTER THE COOLING AND CRYSTALLIZATION OF THE MAGMAS THROUGH THE AGENCY OF HOT MAGMATIC SOLUTIONS.

33Evidence of Igneous Source

34Possible Influence of Meteoric Waters in Deposition of Ores of This Class

35Zonal Arrangement of Minerals Related to Igneous Rocks

36The Relation of Contact Metamorphism to Ore Bodies of the Foregoing Class.

37SECONDARY CONCENTRATION IN PLACE OF THE FOREGOING CLASSES OF MINERAL DEPOSITS THROUGH THE AGENCY OF SURFACE SOLUTIONS

38RESIDUAL MINERAL DEPOSITS FORMED BY THE WEATHERING OF IGNEOUS ROCKS IN PLACE

39MINERAL DEPOSITS FORMED DIRECTLY AS PLACERS AND SEDIMENTS

40Mechanically Deposited Minerals

41Chemically and Organically Deposited Minerals

42SEDIMENTARY MINERAL DEPOSITS WHICH HAVE REQUIRED FURTHER CONCENTRATION TO MAKE THEM COMMERCIALLY AVAILABLE

43ANAMORPHISM OF MINERAL DEPOSITS

44CONCLUSION: FOOTNOTES: