April 21, 1860, that they had for sale "the best and
finest article of table salt, gathered from the banks of
Salt creek, forty miles directly west of this city. Nature
is the only evaporator used in the manufacture of this
salt." The News of April 28th relates that a sample
of some thirty bushels of the very neatest and best of table
salt had been brought for its inspection, and it had been
"scraped up from the banks of Salt creek with a shovel. The
probability is that the salt, as well as gold, silver, and
coal mines of Nebraska are inexhaustible." The News
of May 25, 1861, notes that a train of three wagons passed
through Nebraska City to engage in the manufacture of salt
at the springs fifty miles west. The same paper says that,
"A gentleman the other day brought in from Salt creek 1800
pounds of as fine salt as we have ever seen. It met with
ready sale. There is a mine of wealth out there." The
News of September 14, 1861, reports that there are
"four salt basins of a thousand acres each -- except one
small one -- filled with small springs that during the night
ooze out their briny waters and cover the plateaus with a
thick scum of salt. They ebb and flow like the tides of the
ocean, during the night time covering the entire surface to
the extent of thousands of acres and to a depth of several
inches. By nine o'clock of an ordinarily dry day, with
sunshine, the waters have sunk away, or rather evaporated,
leaving a crust of salt. There are at present ten furnaces."
The Advertiser reports that a number of persons from
Nemaha county and Atchison county, Missouri, had been out to
the salt springs in Saline and Lancaster counties
manufacturing salt for winter use. "They all returned with
their wagons filled with the very best quality of salt. The
salt manufactured at these springs is precisely the same as
we get in small sacks. called table salt. Hereafter there
will be but little salt brought up the river for this region
of the country." The News of June 28, 1862, in a
description of Salt creek valley, says that along this
valley and near some of its tributaries the saline deposits
and springs are found, the first of them in township 8, and
thence to township 12 they are of frequent occurrence. The
more southerly are not of very great value. In township 10
of ranges 6 and 7 are found the great springs, the water of
which is of sufficient strength and supply to make the
manufacture profitable. The News of June 7, 1862,
notes that the surveyor general of Kansas and Nebraska "is
about to visit and reëxamine the saline lands lying
west of this city in Calhoun county." |
23, 34, and 37." The secretary of the interior had
advised him that the delegate (presumably the delegate to
Congress, Mr. Daily) had informed him that there was "good
reason to believe that large quantities of saline lands have
been reported as ordinary lands by fraudulent collusion
between the surveyors and speculators." On the 12th of
September, 1859, John W. Prey located military land warrants
on 320 acres of these lands, which included the best of the
springs, in sections 21 and 22, township 10 north of range 6
east, and the certificates were issued by Andrew Hopkins,
register of the land office at Nebraska City. Mr. Prey had
obtained these warrants from J. S. Morton, who held them as
agent for eastern owners. As they were worth their face for
land entry but were below par in the market, there might be
mutual advantage in this arrangement. Patents for these
lands were sent to the land office, but before they were
delivered the question whether the lands were open to
private entry arose, and the patents were withheld by the
order of the commissioner of the general land office. In the
following November Prey made warranty deeds of an undivided
third interest in these lands to Andrew Hopkins, Charles A.
Manners, and J. Sterling Morton, respectively, the
consideration recited in each deed being $166. The
commissioner of the land office held that these lands were
reserved as saline lands under the act of July 22, 1854. The
enabling act of 1864 granted to the state of Nebraska, when
it should be admitted into the Union, "all salt springs in
said state not exceeding twelve in number, with six sections
of land adjoining, to be selected by the governor within one
year after the admission of the state." Governor Butler made
a selection of most of the lands under this act in June,
1867. In his message to the legislature which convened
January 7, 1869, Governor Butler made an enthusiastic
statement of his belief in the great commercial value of the
salt basin and said that for the purpose of promoting the
early development of the salt industry he had leased one
section of the salt lands claimed by the state to Anson C.
Tichenor, who in turn assigned a half interest in the lease
to the Nebraska Salt Company of Chicago; but this company
was neglecting or refusing to develop the industry. On the
15th of February, 1869, the legislature declared this lease
void, and on the same date a part of the reserve --the north
half, and the north half of the south half of section 21,
township 10 -- was leased by the governor to Anson C.
Tichenor and Jesse T. Green for a term of twenty years. For
the purpose of testing the legal rights of the purchasers of
the lands under Prey's entry, as against the state and its
lessees, on the 24th of December, 1870, J. Sterling Morton,
with several assistants, including Edward P. Roggen, since
well known as a politician and secretary of the state of
Nebraska, took possession of a building upon the leased
lands which had been erected by the lessees for their use
while carrying on the work of salt production; but the
premises were not occupied at this time. Thereupon, under
the direction of James E. Philpott, attorney for the
lessees, Morton and Roggen were arrested on the charge of
stealing firewood which was piled up at the building they
had appropriated to their use. The alleged trespassers were
brought before John H. Ames, then justice of the peace,
since then a commissioner of the supreme court of Nebraska,
and Seth Robinson, attorney-general of the state, appeared
to prosecute them. On Morton's agreement to desist from any
further attempt to obtain possession of the disputed lands
until the question of title should be legally settled, the
criminal proceedings were stopped at this stage. |
while Justice Oliver I. Mason dissented in a long and
vigorous opinion, in which he held that the reservation act
of 1854 did not apply to the lands in question. The
plaintiffs then carried the case to the Supreme Court of the
United States, where it was contested on their part by such
eminent counsel as Jeremiah S. Black, Montgomery Blair, J.
H. Hopkins and Eleazer Wakeley; and by E. Rockwood Hoar for
the defendants. Judge Wakeley had been Mr. Morton's attorney
from the inception of the case. The Supreme Court also
decided against the plaintiffs, Judge David Davis writing
the opinion, in which he held that the lands in question had
been reserved as saline lands by the act of Congress, and
that the patents -- or right to them -- on which the
plaintiffs relied for their title were void from the
beginning. The opinion recites that, "It appears by the
record that on the survey of the Nebraska country the
salines in question were noted on the field books but those
notes were not transmitted to the register's general plats,
and it is argued that the failure to do this gave a right of
entry." But the court held that the language of the statute
was sweeping. "The executive officers had no authority to
issue a patent for the lands in controversy, because they
were not subject to entry having been previously reserved."
It appears that before Prey located these lands with his
military warrants the President of the United States had
offered them for sale, and there being no bidders they were
thus, so far as this record appeared, left open to private
filing or entry. |
for sinking a well to the depth of 2,000 feet for a
consideration of $10,125. The plant was set by April 7,
1886, and actual work was begun on the 3d of May and
continued to the last of August, 1887. At a depth of 600
feet flowing water was reached, as in the Cahn and Evans
well. "This water is some different from that obtained at
the government square. Both flows were found in limestone,
the one at the square at 560 feet." The work under the first
contract ceased at 2,008 feet. "No brine of sufficient
strength to warrant the manufacture of salt" having been
found, a supplementary contract was made to go down 400 feet
further. The work stopped at a depth of 2,463 feet, "without
finding any brine or indications of salt." The strongest
brine was found in a stratum of sand and gravel between
depths of 195 feet and 205 feet, and it tested thirty-five
degrees. It was the opinion of B. P. Russell, the geologist
in charge of the work, that the salt springs upon the basin
were caused by the gradual rising of this water to the
surface. At 205 feet the first hard rock was found, and the
use of the diamond drill began. A pipe or casing, nine
inches in diameter, was sunk in the first forty-nine feet of
the boring, and then a seven-inch pipe was inserted in this
and sunk below it down to the hard rock at 205 feet. From
this point to a depth of 365 feet a bit cutting a core four
inches in diameter was used; then a bit cutting a two-inch
core was substituted and used to a depth of 1,025 feet,
where a soft straturn compelled the reaming of this smaller
section and the sinking of a four-inch casing through the
soft material until hard rock was again reached at 1,113
feet. The artesian stratum of water at 600 feet was a weak
brine of twelve to fourteen degrees, another flowing stratum
at 828 feet tested from twenty degrees to twenty-two
degrees. |
remarks that hunting these animals is exciting sport,
their speed and endurance being such that it requires a good
horse to overtake them or break them down in a fair race,
and the skill and practice of a good hunter to place the
ball in fatal parts. He had known a buffalo to be perforated
with twenty balls and yet be able to maintain a distance
between himself and his pursuer. "Experienced hunters aim to
shoot them in the lungs or the spine. From the skull the
ball rebounds, flattened as from a rock or a surface of iron
and has usually no other effect on the animal than to
increase his speed. A wound in the spine brings them to the
ground instantly, and after a wound in the lungs their
career is soon suspended from difficulty of breathing. They
usually sink, rather than fall, upon their knees and
haunches, and in that position remain until they are dead,
rarely rolling upon their backs." Mr. Bryant remarks that
the flesh of the bull is coarse, dry, and tough, but that
from a young fat heifer or cow -- and many of them were very
fat -- "is superior to our best beef." "The choice pieces of
a fat cow are a strip of flesh along each side of the spine
from the shoulders to the rump; the tender-loin; the liver;
the heart; the tongue; the hump-ribs; and an intestinal
vessel or organ, commonly called by hunters the 'marrow-gut'
which anatomically speaking, is the chylo-poetic duct."
Major Long, on his expedition in 1819,
also found buffalos in large numbers above the confluence of
the forks of the Platte, and at one time, "it would be no
exaggeration to say that at least ten thousand here burst on
our sight in an instant." Major Long also found these
animals in vast numbers, on his return trip, in the
neighborhood of the great bend on the Arkansas. In the upper
Platte country he observes that, "We have frequently
remarked broad, shallow excavations in the soil of the
diameter of from five to eight feet, and greatest depth from
six to eighteen inches. These are of rare occurrence near
the Missouri as far as Engineer Cantonment and in other
districts where the bison is seldom seen at the present
day." He observes that these "wallows" become more and more
numerous as he goes west, "offering a considerable
impediment to the traveler who winds his way amongst them,
and are entirely destitute of grass, being covered with a
deep dust." Major Long was convinced from observation that
these wallows were made by the bulls dusting themselves by
means of their fore feet, and that they also served as
places for rolling and wallowing. Stansbury also found large
herds of buffalos west of the forks of the Platte. Kelly
found these animals in immense numbers in the same region.
They were so numerous that he was driven to confess that the
stories he had heard about them in this respect had not been
exaggerated. |
In 1851 Father De Smet found that "the
whole space between the Missouri and the Yellowstone was
covered [with buffalos] as far as the eye could
reach." He observed that a young Indian lured the cows
within easy gun-shot by imitating the cries of a calf, and
he called back the simple creatures to their death at
pleasure by repeating these cries after he had killed part
of them. After leaving the valley of the Platte, "a very
sensible change is perceptible in the productions of the
soil; instead of the former robust and vigorous vegetation
the plains are overgrown with a short, crisp grass; however
it is very nourishing and eagerly sought by the herds of
buffalo and countless wild animals that graze on them." |
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