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Updated: October 7, 2025
The system of great fissures by which they are broken extends north and south, and the long, narrow, tilted crust blocks intercepted between the fissures give rise to the numerous north-south ranges of the region.
The United States continues to believe that progress can best be made when nations focus on such specific problems, rather than on procedural and institutional questions. It will continue to work to move the North-South dialogue into a more constructive phase. The War on Hunger must be a continuous urgent priority.
After the gape of the Ancobra River the foreshore gradually bends for a few miles from a west-east to a north-south rhumb, and forms a bay within a bay.
"Not much fun for the King here!" he thought, "it's devilish monotonous ... can't see anything, and nothing to hear ... hold on, I can distinguish three separate noises, the plash of the water from the fountains, the rumble of carriages, and that heavy sound can only be the passage of trains from the North-South in the tunnel, which if I mistake not is right under my prison ... and these Singing Fountains ... they are accounted for by the King howling when he got drunk ... but what about the night Susy d'Orsel was killed?... The King wasn't here then, and yet they were heard singing?"
Austria retorted to the steps being taken by the Russo-French group by obtaining from the Sultan permission to build a railway from Uvatz, on the Bosnian frontier, to Mitrovitza, which would link up Serajevo with Salonika. The Balkan railway question had been rankling for years. The Slav wanted an east-and-west line to connect with the Adriatic. The Teuton a north-south one to reach the Aegean.
HOW SHORE DRIFT MIGRATES. It is under the action of waves and currents that shore drift migrates slowly along a coast. Where waves strike a coast obliquely they drive the waste before them little by little along the shore. Thus on a north-south coast, where the predominant storms are from the northeast, there will be a migration of shore drift southwards.
For a moment, when the weather improved for a short time, we saw high mountains directly to the east. During the heavy snow squall on November 28th we passed two peculiarly shaped mountains lying in a north-south direction; they were the only ones that we could see on our right hand. These "Helland-Hansen Mountains" were entirely covered by snow and had an altitude of 9,200 feet.
There are evil reports about the origin of the Frenchman's fatal illness after disregarding this and similar warnings. The deep and steep-banked depression runs north-south, and is apparently the head of the Bujiá stream.
The characteristics of the coast of Maine are due chiefly to the fact that a mountainous region of hard rocks, once worn to a peneplain, and after a subsequent elevation deeply dissected by north-south valleys, has subsided, the depression amounting on its southern margin to as much as six hundred feet below sea level.
I was dumbfounded. I did not know of any fence in these parts, of none where I thought I should be. And how had we got into it? I had not passed through any gate. There was, of course, no use in conjecturing. If the wind had not veered around completely, one of the fences must run north-south, the other one east-west, and we were in the southeast corner of some farm.
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