Buffalo Land: Authentic Account of the Discoveries, Adventures, and Mishaps of a Scientific and Sporting Party in the Wild WestWebb, W. E. (William Edward)
History
Buffalo Land: Authentic Account of the Discoveries, Adventures, and Mishaps of a Scientific and Sporting Party in the Wild West
Webb, W. E. (William Edward)
Hunting -- West (U.S.); Paleontology -- Kansas; West (U.S.) -- Description and travel
"At Fort Riley about sixty-nine per cent, of the annual precipitation is
in spring and summer; at Fort Kearney, eighty-one; and at Fort Laramie,
seventy-two per cent. From observations at Forts Harker, Hays, and
Wallace, on the line of this road, the same rule seems to hold good.
Records have not been long enough continued at these three posts to give
a long average, but the mean appears to be between seventeen and
nineteen inches at Hays and Wallace, and possibly rather more at Harker.
The actual average for 1868 and 1869 at Hays is 18.76 inches, and for
the first six months of 1870 the record is 10.68 inches. At Wallace the
record for 1869 was over seventeen inches, and in 1870, up to October 1,
about the same amount had fallen.
"Without records there can be only conjecture; and I can only remark
that there does not seem to be much diminution in the annual rain-fall
until we get as far west as the one hundred and third meridian. Thence
to the base of the mountains (except perhaps in the timbered portions of
the great divide south of the line of this railway) the annual average
may be possibly two or three inches less than in the midst of the
plains--a peculiarity explained, hypothetically, by the fact that the
region 'lies to the westward of the general course of the moisture
currents of air flowing northward from the Gulf of Mexico, and is so
near the mountains as to lose much of the precipitation that localities
in the plains east and north-east are favored with. The mountains seem
to exercise an influence--electrical and magnetical--in attracting
moisture, which is condensed in the cooler regions of their summits,
while the plains at their feet may be parched and heated to excess.'
This explanation may be fanciful, but the fact remains that near the
mountains the rains seem to decrease north of the great divide;
fortunately, however, this occurs in a region where irrigation may be
applied extensively and where there is sufficient moisture to nourish
bountiful crops of grass.
"The vegetation of the plains along wagon tracks and rail road
embankments shows a capability of production scarcely suggested by the
surface where undisturbed: wherever the earth is broken up, the wild
sunflower (_Helianthus_), and others of the taller-growing plants,
though previously unknown in the vicinity, at once spring up.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account