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The Exploring Expedition to the Rocky Mountains, Oregon and California - To which is Added a Description of the Physical Geography of California, with Recent Notices of the Gold Region from the Latest and Most Authentic Sources by Brevet Col. J.C. Fremont
page 119 of 555 (21%)
23d.--Yesterday evening we reached our encampment at Rock Independence,
where I took some astronomical observations. Here, not unmindful of the
custom of early travelers and explorers in our country, I engraved on this
rock of the Far West a symbol of the Christian faith. Among the thickly
inscribed names, I made on the hard granite the impression of a large
cross, which I covered with a black preparation of India-rubber, well
calculated to resist the influence of wind and rain. It stands amidst the
names of many who have long since found their way to the grave, and for
whom the huge rock is a giant gravestone.

One George Weymouth was sent out to Maine by the Earl of Southampton, Lord
Arundel, and others; and in the narrative of their discoveries, he says:
"The next day we ascended in our pinnace that part of the river which lies
more to the westward, carrying with us a cross--a thing never omitted by
any Christian traveler--which we erected at the ultimate end of our
route." This was in the year 1605; and in 1842 I obeyed the feeling of
early travelers, and left the impression of the cross deeply engraved on
the vast rock one thousand miles beyond the Mississippi, to which
discoverers have given the national name of _Rock Independence_.

In obedience to my instructions to survey the river Platte, if possible, I
had determined to make an attempt at this place. The India-rubber boat was
filled with air, placed in the water, and loaded with what was necessary
for our operations; and I embarked with Mr. Preuss and a party of men.
When we had dragged our boat a mile or two over the sands, I abandoned the
impossible undertaking, and waited for the arrival of the party, when we
packed up our boat and equipage, and at nine o'clock were again moving
along on our land journey. We continued along the valley on the right bank
of the Sweet Water, where the formation, as already described, consists of
a grayish micaceous sandstone, and fine-grained conglomerate, and marl. We
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