A Study of Recent Earthquakes

A Study of Recent Earthquakes
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"A Study of Recent Earthquakes" by Charles Davison. Published by Good Press. Good Press publishes a wide range of titles that encompasses every genre. From well-known classics & literary fiction and non-fiction to forgotten−or yet undiscovered gems−of world literature, we issue the books that need to be read. Each Good Press edition has been meticulously edited and formatted to boost readability for all e-readers and devices. Our goal is to produce eBooks that are user-friendly and accessible to everyone in a high-quality digital format.

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Charles Davison. A Study of Recent Earthquakes

A Study of Recent Earthquakes

Table of Contents

PREFACE

A STUDY OF. RECENT EARTHQUAKES

CHAPTER I

INTRODUCTION

TERMS AND DEFINITIONS

ORIGIN OF EARTHQUAKES

FOOTNOTES:

CHAPTER II.ToC

THE NEAPOLITAN EARTHQUAKE OF DECEMBER 16TH, 1857

ISOSEISMAL LINES AND DISTURBED AREA

DAMAGE CAUSED BY THE EARTHQUAKE

GENERAL OBJECTS OF INVESTIGATION

POSITION OF THE EPICENTRE

DEPTH OF THE SEISMIC FOCUS

NATURE OF THE SHOCK

ELEMENTS OF THE WAVE-MOTION

SOUND-PHENOMENA

VELOCITY OF THE EARTH-WAVES

MINOR SHOCKS

ORIGIN OF THE EARTHQUAKE

FOOTNOTES:

CHAPTER III.ToC

THE ISCHIAN EARTHQUAKES OF MARCH 4TH, 1881, AND JULY 28TH, 1883

VOLCANIC HISTORY OF ISCHIA

EARTHQUAKE OF MARCH 4TH, 1881

ISOSEISMAL LINES AND DISTURBED AREA

POSITION OF THE EPICENTRE

DEPTH OF THE SEISMIC FOCUS

NATURE OF THE SHOCK

AFTER-SHOCKS

EARTHQUAKE OF JULY 28TH, 1883

PREPARATORY SIGNS

ISOSEISMAL LINES AND DISTURBED AREA

POSITION OF THE EPICENTRE

DEPTH OF THE SEISMIC FOCUS

NATURE OF THE SHOCK

LANDSLIPS

AFTER-SHOCKS

CHARACTERISTICS OF ISCHIAN EARTHQUAKES

ORIGIN OF THE ISCHIAN EARTHQUAKES

FOOTNOTES:

CHAPTER IV.ToC

THE ANDALUSIAN EARTHQUAKE OF DECEMBER 25TH, 1884

DAMAGE CAUSED BY THE EARTHQUAKE

ISOSEISMAL LINES AND DISTURBED AREA

THE UNFELT EARTHQUAKE

POSITION OF THE EPICENTRE

DEPTH OF THE SEISMIC FOCUS

NATURE OF THE SHOCK

SOUND-PHENOMENA

VELOCITY OF THE EARTH-WAVES

MISCELLANEOUS PHENOMENA

AFTER-SHOCKS

GEOLOGY OF THE MEIZOSEISMAL AREA AND ORIGIN OF THE EARTHQUAKES

REFERENCES

FOOTNOTES:

CHAPTER V.ToC

THE CHARLESTON EARTHQUAKE OF AUGUST 31ST, 1886

DAMAGE CAUSED BY THE EARTHQUAKE

ISOSEISMAL LINES AND DISTURBED AREA

PREPARATION FOR THE EARTHQUAKE

NATURE OF THE SHOCK

THE DOUBLE EPICENTRE

ORIGIN OF THE DOUBLE SHOCK

DEPTH OF THE SEISMIC FOCI

VELOCITY OF THE EARTH-WAVES

MISCELLANEOUS PHENOMENA

AFTER-SHOCKS

ORIGIN OF THE EARTHQUAKE

REFERENCES

FOOTNOTES:

CHAPTER VI.ToC

THE RIVIERA EARTHQUAKE OF FEBRUARY 23RD, 1887

DAMAGE CAUSED BY THE EARTHQUAKES

PREPARATION FOR THE EARTHQUAKES

ISOSEISMAL LINES AND DISTURBED AREA

POSITION OF THE EPICENTRES

DEPTH OF THE PRINCIPAL FOCUS

NATURE OF THE SHOCK

SOUND-PHENOMENA

THE UNFELT EARTHQUAKE

EFFECTS OF THE EARTHQUAKE AT SEA

MISCELLANEOUS PHENOMENA

AFTER-SHOCKS

ORIGIN OF THE EARTHQUAKES

REFERENCES

FOOTNOTES:

CHAPTER VII.ToC

THE JAPANESE EARTHQUAKE OF OCTOBER 28TH, 1891

THE MEIZOSEISMAL AREA

DAMAGE CAUSED BY THE EARTHQUAKE

ISOSEISMAL LINES AND DISTURBED AREA

NATURE OF THE SHOCK

PRINCIPAL MEASUREMENTS OBTAINED FROM SEISMOGRAPHIC RECORDS

VELOCITY OF THE EARTH-WAVES

THE GREAT FAULT-SCARP

MINOR SHOCKS

EFFECT OF THE EARTHQUAKE ON THE SEISMIC ACTIVITY OF THE ADJOINING DISTRICTS

ORIGIN OF THE EARTHQUAKE

REFERENCES

FOOTNOTES:

CHAPTER VIII.ToC

THE HEREFORD EARTHQUAKE OF DECEMBER 17TH, 1896, AND THE INVERNESS EARTHQUAKE OF SEPTEMBER 18TH, 1901

THE HEREFORD EARTHQUAKE OF DECEMBER 17TH, 1896

ISOSEISMAL LINES AND DISTURBED AREA

NATURE OF THE SHOCK

DIRECTION OF THE SHOCK

COSEISMAL LINES AND VELOCITY OF EARTH-WAVES

SOUND-PHENOMENA

MINOR EARTHQUAKES

ORIGIN OF THE EARTHQUAKES

THE INVERNESS EARTHQUAKE OF SEPTEMBER 18TH, 1901

PREPARATORY SHOCKS

EFFECTS OF THE SHOCK

ISOSEISMAL LINES AND DISTURBED AREA

NATURE OF THE SHOCK

SOUND-PHENOMENA

ORIGIN OF THE EARTHQUAKE

THE AFTER-SHOCKS AND THEIR ORIGIN

SYMPATHETIC EARTHQUAKES

CONCLUSION

REFERENCES

FOOTNOTES:

CHAPTER IX.ToC

THE INDIAN EARTHQUAKE OF JUNE 12TH, 1897

ISOSEISMAL LINES AND DISTURBED AREA

NATURE OF THE SHOCK

ELEMENTS OF THE WAVE-MOTION

SOUND-PHENOMENA

VELOCITY OF THE EARTH-WAVES

THE UNFELT EARTHQUAKE

EARTH-FISSURES, SAND-VENTS, ETC

LANDSLIPS

ROTATION OF PILLARS, ETC

AFTER-SHOCKS

STRUCTURAL CHANGES IN THE EPICENTRAL AREA

ORIGIN OF THE EARTHQUAKE

REFERENCES

FOOTNOTES:

CHAPTER X.ToC

CONCLUSION

FORE-SHOCKS

DISTURBED AREA

POSITION OF THE EPICENTRE

DEPTH OF THE SEISMIC FOCUS

NATURE OF THE SHOCK

SOUND-PHENOMENA

VELOCITY OF THE EARTH-WAVES

STRUCTURAL CHANGES IN THE EPICENTRAL AREA

AFTER-SHOCKS

ORIGIN OF EARTHQUAKES

FOOTNOTES:

INDEX.ToC

Отрывок из книги

Charles Davison

Published by Good Press, 2019

.....

The existence of the Montemurro focus must, however, complicate any relation that may connect these two quantities.

Maximum Velocity.—The means at Mallet's disposal for determining the maximum velocity were more numerous than those available for the amplitude. From the dimensions of a fallen column of regular form we should be able, he remarks, to find an inferior limit to the value of the maximum velocity; while a superior limit at the same place may be obtained from some other regular solid which escaped being overthrown. If a loose body is projected by the shock at a place where the angle of emergence is known, the horizontal and vertical distances traversed by the centre of gravity will give the velocity of projection. Or, if two such bodies are projected at one place, the same measures for each will as a rule give both the angle of emergence and the velocity of projection. A third method depends on the fissuring of walls, supposing that we know the force per unit surface which, when suddenly applied, is just sufficient to produce fracture. Sometimes more than one method must be applied to the same object. The two gate-pillars near Saponara (illustrated in Fig. 6) for example required a horizontal velocity of 5.48 feet per second to fracture them, and an additional velocity of 5.14 feet per second to overthrow them.

.....

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