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The Elements of economic geology

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fullscreen: The Elements of economic geology

Monograph

Identifikator:
1773832379
URN:
urn:nbn:de:zbw-retromon-172798
Document type:
Monograph
Author:
Gregory, John W. http://d-nb.info/gnd/11683014X
Title:
The Elements of economic geology
Place of publication:
London
Publisher:
Methuen
Year of publication:
1928
Scope:
XIV, 312 S.
graph. Darst.
Digitisation:
2021
Collection:
Economics Books
Usage license:
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Chapter

Document type:
Monograph
Structure type:
Chapter
Title:
Part IV. Engineering geology
Collection:
Economics Books

Contents

Table of contents

  • The Elements of economic geology
  • Title page
  • Contents
  • Part I. Introduction
  • Part II. Ore deposits
  • Part III. Earthy minerals
  • Part IV. Engineering geology
  • Part V. Mineral fuels
  • Index of authors
  • Index of localities
  • Subject index

Full text

236 ECONOMIC GEOLOGY 
wave traversing a plateau causes the particles to oscillate 
about their original position; but at the end of the plateau 
the ground is flung forward, just as a tap on one end of a 
row of billiard balls sends a wave through them but only 
moves the last, which is jerked forward. 
Structures should be light to reduce both inertia and 
momentum ; for on a sudden shock inertia tends to jerk 
the lower part from under the slower upper part; while 
momentum causes the upper part to continue the forward 
swing after the base has begun to move back. Hence factory 
chimneys are built with a broad strong base, which tapers 
upward, and the upper part is composed of sheet iron, to 
reduce the weight. A chimney built as a uniform cylinder 
would be fractured at the base. The danger of top-heavy 
chimneys was shown at the Warnambool earthquakes in 
Victoria of 1903; they are built of a dune limestone which 
is used in thick slabs and the weight of those at the cap 
rendered the chimneys as unstable as an inverted pendulum 
and many were overthrown. 
The strength of a wall is reduced by the doors and windows, 
for they serve like the perforations in a sheet of stamps, and 
the cracks run from one to the next. A medium angle of 
emergence is accompanied by cracks that radiate from the 
window corners, while a horizontal emergence is marked by 
vertical cracks. Vertical rows of windows are weaker than 
a diagonal or quincuncial arrangement. 
The arch is a dangerous structure in earthquake areas 
unless embedded underground ; for during horizontal move- 
ments the two sides may move in opposite directions at the 
same time, and the arch be torn asunder. The Kiso Sawa 
railway bridge in Japan rested on piers of masonry 26 feet 
long by 10 feet thick, each supported by two circular drum 
curbs, 12 feet in diameter. The bridge was destroyed by an 
earthquake, as the differential movement of the two drums 
tore each pier in twain; they were replaced by single drums 
30 feet by 12 feet. 
The reduction of the stresses due to momentum and inertia 
specially concerns the design of roofs. When a building is 
jerked forward the roof tends to remain behind, and the side 
left unsupported may fall into the room. In Japanese 
temples the roof timbers were knit together by many joints
	        

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The Elements of Economic Geology. Methuen, 1928.
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