Chapter

 1 VI   |          known that the internal temperature rises one degree for every
 2 VI   |         leagues, there must be a temperature of 360,032 degrees at the
 3 VI   |     solid or liquid under such a temperature. I have therefore good reason
 4 VI   | terrestrial crust, for there the temperature will be more than 2372 degrees.”~“
 5 VI   |  believed until Fourier that the temperature of the interplanetary spaces
 6 VI   |     confute.”~[1] The degrees of temperature are given by Jules Verne
 7 XI   |        not enough to measure the temperature of springs or any matter
 8 XI   |    hazarded as to their quality, temperature, and even absence, remained
 9 XIII |        sun does not set.~But the temperature was much lower. I was cold
10 XVIII|          no sensible increase of temperature. This justified Davy’s theory,
11 XVIII|    observations, the increase of temperature in the interior of the globe
12 XVIII|      Wuttembourg in Bohemia.~The temperature, which ought to have been
13 XX   |         conclusion that the high temperature then existing was due to
14 XX   |   geological contemplations. The temperature remained what it had been
15 XXI  |         sight of it. I found the temperature and the air stifling. Fatigue
16 XXV  |         to the law of increasing temperature, there ought to be a heat
17 XXX  |     clear whiteness, and its low temperature, showed that it must be
18 XXXIV|         E., unsteady and fitful. Temperature high. Rate three and a half
19 XXXIV|         favourable conditions of temperature. But it seems manifest to
20 XLII |       anxiety, and certainly the temperature was at this moment at the
21 XLII |      some slight increase in the temperature, nothing new had happened.~“
22 XLII |      supply its place.~Still the temperature kept rising, and I felt
23 XLIII|         matter of all kinds. The temperature was becoming unbearable.