Book,  Chapter

 1        I,  III  |            the upper strata of the atmosphere were suffused with a rosy
 2        I,  V    |           The decompression of the atmosphere made the specific gravity
 3        I,  VI   |  diminution in the pressure of the atmosphere had precisely the same effect
 4        I,  VII  |  diminution in the pressure of the atmosphere. He felt that his judgment
 5        I,  VII  |  diminution in the pressure of the atmosphere. Water boiling at a temperature
 6        I,  VIII |             that the planet had an atmosphere of her own; and certain
 7        I,  IX   |         and that the weight of the atmosphere was so much diminished?
 8        I,  XII  |          in its formation that the atmosphere had had no opportunity of
 9        I,  XIII |   anticipations. The weight of the atmosphere was so reduced that there
10        I,  XV   |            envelope of the earth’s atmosphere, and that it is now traveling
11        I,  XVI  |         vapors accumulating in the atmosphere; and nothing more than a
12        I,  XVII |           chilled condition of the atmosphere prevented the formation
13        I,  XVII |         portion of the old earth’s atmosphere, why should it not likewise
14        I,  XX   |      either the oxygen of Gallia’s atmosphere had been brought into contact
15        I,  XXI  |          dryness and purity of the atmosphere caused to re-echo like a
16        I,  XXII |          as it were, congealed the atmosphere so that there was not a
17        I,  XXIII|    reappear.~On the 26th, under an atmosphere perfectly clear and dry,
18       II,  IV   |          complete stillness of the atmosphere; the very air seemed to
19       II,  IV   | thermometer continued to fall; the atmosphere remained clear as heretofore.
20       II,  V    |          that had fallen while the atmosphere was still to some extent
21       II,  XII  |           with a proportion of the atmosphere of the earth, and beneath
22       II,  XII  |         the earth had possessed no atmosphere, and that consequently no
23       II,  XIII |       still bitterly cold, but the atmosphere had lost nothing of its
24       II,  XV   |            be a derangement in the atmosphere of Gallia, which would result
25       II,  XVI  |           a portion of the earth’s atmosphere and substance, and so she
26       II,  XVI  |    suffocated, for all our comet’s atmosphere would be assimilated with
27       II,  XVI  |   assimilated with the terrestrial atmosphere, and we, supposing we were
28       II,  XVI  |           beforehand into Gallia’s atmosphere, I believe it will transpire
29       II,  XVI  |           will transpire that this atmosphere will amalgamate with that
30       II,  XVI  |       would glide into the mingled atmosphere and remain suspended in
31       II,  XVI  |       breezes to which the Gallian atmosphere had long been unaccustomed.
32       II,  XVI  |            making the transit from atmosphere to atmosphere.~The necessity
33       II,  XVI  |         transit from atmosphere to atmosphere.~The necessity was becoming
34       II,  XVII |     carried with it any portion of atmosphere, whether it possessed any
35       II,  XVII |         possible to glide from one atmosphere to another, so that they
36       II,  XVII |            be high in the air. The atmosphere was less buoyant than that
37       II,  XVIII|           pervaded the terrestrial atmosphere.~But as the aeronauts were
38       II,  XVIII|    suddenness of transfer from one atmosphere to the other.~The next question
39       II,  XVIII|            altitude in the comet’s atmosphere much inferior to the balloon.~
40       II,  XVIII|          receive the comet and its atmosphere, balloon and all, into its
41       II,  XVIII|     vibration quivered through the atmosphere. The montgolfier, elongated