As worth a certain price in praise, but take them all
And use them all, with simple, heartfelt pleasure.
For when we gladly eat our daily bread, we bless
The hand that feeds us;
And when we walk along life’s way in cheerfulness,
Our very heart-beats praise the Love that leads us.
(1294)
Gratuities—See [Ridicule, Apt].
GRAVITATION AND ICEBERGS
The hundreds of thousands of icebergs that every spring and summer terrify our ocean steamers are simply detachments from the glaciers that perpetually cover the face of northern lands. As far as can be learned, the interior of Greenland has a surface of tall hills and deep gulches, with an elevated range rather on the eastern side, running from north to south. Hence, if the climate of the interior of Greenland were mild, this extended range would serve as a watershed diverting streams to the sea on both sides. But the temperature some distance inland is nearly always below the freezing point, so that the almost constant snowfall and the brief midsummer rains remain on the surface, accumulating year after year, till there are formed thousands of square miles of blue compact ice, some of it over 1,500 feet thick. This enormous body of ice, like water, is subject to the laws of gravitation, and is eternally on the march to the sea. But its rate of travel is so slow as to be in most places imperceptible to the eye. So deep is this mass of inland ice that after a couple of days’ march from the sea there are no longer any hills visible, the entire landscape being white and naked. The ice from the higher ground is being constantly forced into the valleys and most of these valleys terminate toward the sea in very deep fjords. These fjords are in reality the launchways for most of the ice-floes and a great many of the bergs. You might lie for hours in your boat by most of the glaciers where they enter the sea, and not be aware that they were moving; but each one pushes constantly, and at a regular rate of speed, outward and outward into the sea, till the buoyancy of the water under it causes it to break at the shore, and sets it free to rove the ocean for thousands of miles, till it melts in Southern latitudes.—Edmund Collins, Harper’s Weekly.