Hostname: page-component-78c5997874-j824f Total loading time: 0 Render date: 2024-11-14T22:29:45.477Z Has data issue: false hasContentIssue false

I.—A Cruise among the Volcanos of the Kurile Islands

Published online by Cambridge University Press:  01 May 2009

John Milne
Affiliation:
Imperial College of Engineering, Yedo, Japan.

Extract

The following notes upon the Kuriles were collected during an excursion which I made to these islands in the summer of 1878. Owing to a continuance of foggy weather, which I do not think would find its equal even in Newfoundland, the want of harbours, and the strong currents, although I was almost a month steaming. amongst these islands, it was seldom that we could effect a landing. In consequence of this the bulk of the material embodied in the following notes was written from what I saw from the deck of our vessel. However, as I had good opportunities for seeing nearly every island in the group, and many of these from several points of view, the following notes may not be altogether without value. One advantage which was gained by viewing these island from a distance was, that I was thereby better able to judge of the number, and the general from of the mountains they contained, and to roughly make comparisons of their relative heights, than I could have done had I been actually on the island themselves.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1879

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 347 note 1 The soundings made by the Challenger gave for one of the depths to the east of the Kuriles 27,930 feet—the deepest sounding in the Pacific.

page 348 note 1 Geikie still retains the name Old Bed Sandstone; but as he has proved a complete discordance between the Upper and Lower, he has come to the same conclusion as myself, and the names by which the two groups are called does not materially signify.