Chapter

 1 VI     |       limit of the terrestrial crust, for there the temperature
 2 VI     |        elastic force which the crust of the earth would be unable
 3 VI     |      upheaving the terrestrial crust, would cause periodical
 4 VI     |      suppose that the external crust cooled down first, whilst
 5 VI     |       into the fissures of the crust of the earth, they broke
 6 XV     |   outflow the thickness of the crust of the island increased
 7 XV     |       cooling of the trachytic crust. Therefore a time would
 8 XV     |        distend and lift up the crust, and then burst through
 9 XVIII  |      we had gone deep into the crust of earth, we should have
10 XX     |       coats of the terrestrial crust; the plants, unacquainted
11 XX     |       yet elastic and yielding crust of the earth obeyed the
12 XXII   |   contraction gave rise in its crust to disruptions, distortions,
13 XXII   |        the base of the mineral crust of the earth, and have ascertained
14 XXII   |      and a half of terrestrial crust. The weight of it seemed
15 XXV    |        to the thickness of the crust of the earth.”~“I don’t
16 XXVI   |    windings of the terrestrial crust.~Before starting afresh
17 XXVII  | substance of the earth’s thick crust, a struggling denizen of
18 XXX    |   consisted only of an elastic crust or bark, alternately acted
19 XXX    |       subsidences of the outer crust, when a portion of the sedimentary
20 XXXI   |         under this terrestrial crust, an ocean with ebbing and
21 XXXVIII|      were still disturbing the crust of the earth. The long-continued
22 XXXVIII| through a great fissure in the crust of the earth, down to the
23 XL     |        through the terrestrial crust; and thy fellow-creatures
24 XLII   |   measure the thickness of the crust of the earth that lay between
25 XLIII  |        conviction. The mineral crust of the globe threatened