be spared. 'Balance those of summer against those of winter by
partially straightening the axis; reduce the inclination from
twenty-three degrees, thirty minutes, to about fifteen degrees,
but let us stop there,' many said. Before we had gone far,
however, we found it would be best to make the work complete.
This will reclaim and make productive the vast areas of Siberia
and the northern part of this continent, and will do much for the
antarctic regions; but there will still be change in temperature;
a wind blowing towards the equator will always be colder than one
blowing from it, while the slight eccentricity of the orbit will
supply enough change to awaken recollections of seasons in our
eternal spring.

"The way to accomplish this is to increase the weight of the pole
leaving the sun, by increasing the amount of material there for
the sun to attract, and to lighten the pole approaching or
turning towards the sun, by removing some heavy substance from
it, and putting it preferably at the opposite pole. This
shifting of ballast is most easily accomplished, as you will
readily perceive, by confining and removing water, which is
easily moved and has a considerable weight. How we purpose to
apply these aqueous brakes to check the wabbling of the earth, by
means of the attraction of the sun, you will now see.

"From Commander Fillmore, of the Arctic Shade and the Committee
on Bulkheads and Dams, I have just received the following by
cable telephone: 'The Arctic Ocean is now in condition to be
pumped out in summer and to have its average depth increased one
hundred feet by the dams in winter. We have already fifty
million square yards of windmill turbine surface in position and