Part,  Chapter

 1      I,  X    |      dry herbage, were wide and level, so that the long train
 2      I,  XIII |    better situation than on the level ground behind Cape Bathurst,
 3      I,  XV   |      but a few inches above the level of the sea, and the tides
 4      I,  XV   |         feet above the ordinary level. How then was it to be explained
 5      I,  XV   | scarcely ten feet above the sea level at low tide?”~“That is just
 6      I,  XV   |         long strip of perfectly level coast-line stretching away
 7      I,  XXII |         caused a sinking of the level of the coast on which the
 8      I,  XXII |       results of this change of level would unfortunately be,
 9      I,  XXII |       liquids to maintain their level, would inundate a portion
10      I,  XXII |      had foreseen, however, the level of the lake was affected
11     II,  I    |     hundred feet more above the level of the ocean, they would
12     II,  IV   |         him to step down to the level of the sea, and from there
13     II,  IV   |        passing, and the general level of the island would sink
14     II,  V    |        of the ice below the sea level was estimated at five feet;
15     II,  VIII |        the waves washed along a level beach when the perpendicular
16     II,  VIII |       island were now only on a level with the ocean.~“O Madge!”
17     II,  VIII |          It is evident that the level of the whole island is gradually
18     II,  X    |         that in some places the level of the coast appeared to
19     II,  XII  |         hours, would suffice to level the entire surface!”~“Yes,
20     II,  XII  |         hours, would suffice to level the entire surface!”~“Yes,
21     II,  XIII |     four hundred feet above the level of the ice-field, and were
22     II,  XV   |         feet at least above the level of the sea, and it was so
23     II,  XVII |    winter, and that the general level of the island did not appear
24     II,  XVIII|        apparent lowering of the level had taken place all along
25     II,  XVIII|         have nearly reached the level of the sea, and Mac Nab
26     II,  XX   |        seven feet below the sea level for every one above—they
27     II,  XXII |        evident that the general level of the islet was being lowered
28     II,  XXIII|       or six feet above the sea level, and its base was probably
29     II,  XXIII|       mean height above the sea level had sensibly diminished.