Part,  Chapter

 1      I,  XVI  |      which was convex towards the current, consisted of a collection
 2      I,  XVIII|          of a pure and refreshing current of air.~The Lieutenant and
 3      I,  XVIII|         trembled as if swept by a current of air.~No description could
 4     II,  I    |          under the influence of a current about which nothing was
 5     II,  I    |         certain resistance to the current, and on its northern shores
 6     II,  II   |        there is no return.~Or the current would take it to the south,
 7     II,  II   |          is called the Kamtchatka Current. It takes its rise in the
 8     II,  II   |        the warm season.~The other current, called Behring Current,
 9     II,  II   |           current, called Behring Current, flows just the other way.
10     II,  II   |        speak, with the Kamtchatka Current at the opening of the strait,
11     II,  II   |      either follow the Kamtchatka Current to the deserted regions
12     II,  II   |       float down with the Behring Current to be swallowed up by the
13     II,  II   |         moment; for I see but one current from the offing of Cape
14     II,  II   |          the dangerous Kamtchatka Current. Are you not afraid that
15     II,  II   |        Because it is a very rapid current, madam; and if we had been
16     II,  II   |     likely between the Kamtchatka Current and the coast, perhaps in
17     II,  II   |          that there is some other current, not marked on our map.
18     II,  II   |          Pole. “With a favourable current might they not reach that
19     II,  II   |       direction, borne along by a current unmarked on the chart, and
20     II,  II   |        been moving along with the current parallel with the coast
21     II,  IV   |          the warmer waters of the current and exposed to all the fury
22     II,  IV   |     exactly the same speed as the current which is bearing it away.
23     II,  V    |           coast. The speed of the current seemed to be less here than
24     II,  V    |         only the 24th July, and a current of average speed would carry
25     II,  VI   |          soon meet the Kamtchatka current, and be carried by it to
26     II,  VI   |        north-west wind out of the current, had approached the continent.
27     II,  VII  |           to have remained in the current which was dragging us to
28     II,  VIII |          the dangerous Kamtchatka Current, which, if it once seized
29     II,  IX   |    towards the west by a powerful current, which could take firmer
30     II,  IX   |        hours, and assisted by the current from the coast.~There was
31     II,  IX   |     island by keeping in the same current which was drifting it away.~
32     II,  IX   |        she knew that the wind and current had driven them into the
33     II,  X    |        CHAPTER X.~ THE KAMTCHATKA CURRENT.~We can readily imagine
34     II,  X    |      driven the island out of the current. The ice-field had approached
35     II,  X    |         grasp of the irresistible current, and was being carried along
36     II,  X    |           grasp of the Kamtchatka Current, and was drifting towards
37     II,  X    |     course made by the Kamtchatka Current, and would quickly pass
38     II,  X    |       along again by the powerful current.~The distance from the northern
39     II,  XII  |           the coast by an unknown current, how the hurricane had driven
40     II,  XII  |          seized by the Kamtchatka Current, concluding his narrative
41     II,  XII  |           the coast by an unknown current, how the hurricane had driven
42     II,  XII  |          seized by the Kamtchatka Current, concluding his narrative
43     II,  XV   |        that it was the Kamtchatka Current which brought us where we
44     II,  XV   |           although the Kamtchatka Current runs the other way, the
45     II,  XV   |      always goes down the Behring Current. Other reasons there are
46     II,  XV   |           still doubtful to which current it would be subject after
47     II,  XV   |           but that the Kamtchatka Current might sweep the island to
48     II,  XV   |          influence of the Behring Current.~“But,” Kalumah repeated
49     II,  XV   | northwards.~Was it the Kamtchatka Current which produced this motion?
50     II,  XV   |          influence of the Behring Current. To make herself more easily
51     II,  XV   |       traced the direction of the current on the sand with a little
52     II,  XV   |          the grasp of the Behring Current, was drifting towards the
53     II,  XVII |         farther by the Kamtchatka Current, which, as is well known,
54     II,  XVIII|           the grasp of a powerful current, and was driving the island
55     II,  XIX  |           of a powerful submarine current, hastening onwards on to
56     II,  XIX  |         of that is at an end; the current is carrying us with great
57     II,  XIX  |          continent, might not the current drive us on to one of the
58     II,  XX   |          deviation of the Behring current, it is bearing in a south-westerly
59     II,  XX   |         Lieutenant was right, the current seemed likely to drag the
60     II,  XX   |         impelled by the submarine current, whilst Victoria Island,
61     II,  XX   |        under the influence of the current, would be left floating
62     II,  XX   |      drawn along by the submarine current, drifted rapidly to the
63     II,  XXI  |         that all the force of the current was deep down below the
64     II,  XXIII|        under the influence of the current, as it gave no hold to the
65     II,  XXIII|           they thought. If only a current, the direction of which