class="tdr">
Probably the rings had to arrive at a certain stage of density before contracting circumferentially |
139 |
Possible average temperature of the sun at the present day. |
|
Central heat probably very much greater |
140 |
Churning of matter going on in the interior of the sun, caused by unequal |
|
rotation between the equator and the poles |
140 |
CHAPTER VIII. |
|
Inquiry into the Interior Construction of the Earth. |
|
What is really known of the exterior or surface |
142 |
What is known of the interior |
143 |
Little to be learned from Geology, which reaches very few miles down |
144 |
Various notions of the interior |
145 |
What is learnt from earthquake and volcanoes. Igno-aqueous fusion, liquid magma. |
146 |
Generally believed that the earth consists of solid matter to the centre. |
|
Mean density. Surface density |
147 |
More detailed estimate of densities near the surface |
148 |
Causes of increased surface density after the crust was formed |
148 |
Calculations of densities for 9 miles deep, and from there to the centre forming Table IV. |
150 |
Reflections on the results of the calculations |
151 |
Notion that the centre is composed of the heaviest metals. |
|
"Sorting-out" theory absurd |
151 |
Considerations as to how solid matter got to the centre |
152 |
Gravitation might carry it there, but attraction could not |
153 |
How the earth could be made out of cosmic matter, meteorites or meteors |
154 |
CHAPTER IX. |
|
Inquiry into the Interior Construction of the Earth—continued |
165 |
The earth gasiform at one period. Density including the moon may have been 1/10,000th |
|
that of air. Must have been a hollow body. Proofs given |
166 |
Division of the mass of the earth alone into two parts |
169 |
Division of the two masses at 817 miles from surface |
171 |
Reasons why the earth cannot be solid to the centre |
172 |
Gasiform matter condensing in a cone leaves apex empty |
172 |
Proportions of the matter in a cone |
173 |
Calculations of the densities of the outer half of the hollow |
|
shell of the earth. Remarks upon the condensation |
174 |
Calculations of inner half of the hollow shell |
175 |
Remarks upon position of inner surface of the shell |
177 |
Calculations of the same |
179 |
CHAPTER X. |
|
Inquiry into the interior construction of the Earth—continued |
184 |
Density of 8·8 times that of water still too high for the |
|
possible compression of the component matter of the earth as known to us |
185 |
Reasons for this conclusion drawn from crushing strains of materials |
186 |
A limit to density shown thereby |
187 |
The greatest density need not exceed 6·24 of water |
188 |
Gases shut up in the hollow centre. Their weight must so |
|
far diminish the conceded maximum of 6·24 |
189 |
Density of inner half of earth at 3000 miles diameter. |
|
Greatest density may be less than 5·833 of water |
190 |
Supposed pressure of inclosed gases very moderate |
191 |
Meaning of heat limit to density. Temperature of interior |
|
half of shell and inclosed gases must be equal |
193 |
State of the hollow interior |
194 |
Results of the whole inquiry |
195 |
CHAPTER XI. |
|
The Earth. The idea entertained by some celebrated men, and others |
197 |
Difficulties of forming a sphere out of a lens-shaped nebula |
199 |
Various studies of the earth's interior made for specialy purposes. Difficulty some |
|
people find in conceiving how the average density of little over 5·66 can be |
|
possible, the earth being a hollow sphere |
200 |
What is gained by its being a hollow shell |
201 |
Geological theories of the interior discussed. |
|
Volcanoes and earthquakes in relation to the interior |
202 |
Liquid matter on the interior surface of the shell, and gases in the hollow, |
|
better means for eruptions than magma layers |
206 |
Focal depths of earthquakes within reach of water, but not of lavas |
207 |
Minute vesicles in granite filled with gases, oxygen and hydrogen, but not water |
209 |
The Moon. A small edition of the earth |
211 |
Rotation stopped. Convulsions and cataclysms caused thereby. Air, water, |
|
vapour driven off thereby to far-off hemisphere. Liquid matter in hollow |
|
interior would gravitate to the inside of the nearest hemisphere |
212 |
Form and dimensions during rotation. Altered form after it stopped |
213 |
Agreeing very closely with Hansen's "curious theory" |
|