The Pacific tourist:

124 the red-colored rocks disappearinglark gray taking their place. How these columns were formed will ever be a question of interest to those who are permitted to see them. One of the Witches especially looks as though she was afflicted with the "Greciau bend"' of modern fashion, a fact which does not at all comport with the dignity or character of a witch. Worn iini fantastic shapes by the storms of ages, and capped with gray, they stand as if "mocking the changes and the chance of time." Four miles below Echo, we lound a rocky point, nearly opposite to which lies the little Mormoni Village of Heinsiferville, on the left side of Weber River, wi th it s bishop's palace-the largest brick building in sight —and school-house, also of brick, niestled under the mountains which lift up rugged peaks in the background. The valley now narrows to a gorge, and we approach IVeber Canon proper. It has high bluffs on the left, with a rocky castle towering up oin the right. If Echo Canon was a wonderful place in the mind of the traveler, wonders, if possible more lrugged and grand, will be revealed to his gaze here. High up oni the face of a bluff to the left, as you pass through the gorge, see the little holes or caves worn by the winds, in which the eagles build their nests. This bluff is called "Eagle?test Roclk." Every year the proud monarch of the air finds here a safe habitation in which to raise his young. It is beyond the reach of men, and accessible onlv to the birds which fly in the air. Passing this home of'; Fr-eedorai's Bird," before we have time to read these lines hardly, we are at the I'lg,oirsaitd Mile Tree, Devil's Stlide, atc., -on the left side of the track. There it stands, spreading its arms of green, from one of which halnigs the sign which marks the distance traveled since leaving Omaha. It is passed in a moment, and other objects of interest claim your attention. High upon rocks to the right, as you peer ahead, see how the winds have made holes in projecting poinlts through which the light and sky beyond can be observed; now looking back see another similar formation oni the opposite side — oile to be seen looking ahead, the other looking back. Now we come to Slate Cut —wheire photograph rocks without number are found. The rocks are so called from the pictures of ferns, branches of trees, shrubs, etc., which are seen traced ill them. They remind one of mossa,ates, only they are a great deal larger-magnified a thousand times, and are not in clear groundwork like the agates. Lost Creek Canon now puts in from the right, and around the curve you call see the houses of the little Mormon Town, Croyden. It is only seven miles from Echo. This canon runs palrallel with Echo Canon for quite a distance, and is said to be rzich ill the scener y characteristic of this region, with a narrow valley of great fertility whelk cul on the south side of the tr ain, will have a pretty little gl impse of th e uppe r portion of Weber River, with its green banks and tree verdure-a charming relief to t he b are, dry plains, s o cora stant and even tiresome. A curious feature of this little Weber Valley, are the terraces. Nlear Echo City is a low, narrow bottom, near the river; then an abr upt asce nt o f 30 feet; then a level plai n or bottom of 200 to 400 yards; then a gend tle ascent to the rock bluffs. The Weber River is exceedingly crooked in its course, -origina lly o ccupy in g the entire width of the littl e space ill the Canon-and ill construct i ng the railroa d at various points, the llr oad-bled here has been built directly into the river, to m ake room for the track. The average angle of elevation of the heights of Weber Canon is 70 to 80 degrees, —and the, height of the suminmnits above the river is 1,500 to 2,000 feet. In this canon i s found a thick bed of hard, red sandstone, of great value for building stone tlvicle can be wrought into fin e form s for cul ve rts, fronts of buildings, caps, sills, etc. Emerging froiin the mouth of Wteber Canon- iand turning to the right, every vestige of rugged canoll mscenery vanishes, and the scene i s changed into onie of peace and quietnes s of v alley life. I/ere the Weber River has a strong, powerful current-wi thi heavy and constanit f all ov er beds of water-worn stolr es, and fallen rocks of imlinense size. In the spring and summer months, it is swollen bytruowf the melting of sow from the mouptaiks, and is of great depth, -th ough usually it aveuages bult four t o six feet in depth and its width, at the mouth of the canon, is usually 120 feet. aThe r e mainder of it s course to the Great Salt Lake, is tohurogh a large open bottom of increasig breadth, a long w hich gather little villages, grain fields, mea dows, brilliant with flowers of which the Ind i an Pink, with its deep scarlet clusters, is most luxuriant. The hills are smooth i outlin o ine, and as we appr oach Ogden, the grand suLmit of the Waahsatch Mountains, with snowy peaks, arise behind, in front, and nor thward, around u s bold and impressive. This is the range of mountain s which b o rder the east s ide of the Salt Lake Valley, and will accompany us, as we go southward to Salt Lake City. Ilochl; s of theber Canoi.-Rettaring to tile road; after leaving Echo you will soon notice, o n the north side of the track, two ctrious formations. The first is a group of reddish-colored cones of different sizes and varying some, in shape, but on the whole remarkably uniform in their appearance. These are known as Battlement Rocks. They are about one mile, perhaps not that, below Echo. Next come the wierd forms of " The W~it~ches " —looking as thoughl they werse talking with each other. These ale gray, andi about) this place it seems that the formnation changes — I I TRE raclprc TOURIST.

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Title
The Pacific tourist:
Author
Williams, Henry T.
Canvas
Page 124
Publication
New York,: H. T. Williams,
1876.
Subject terms
West (U.S.) -- Description and travel
Central Pacific Railroad Company.
Union Pacific Railroad Company.

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"The Pacific tourist:." In the digital collection Making of America Books. https://name.umdl.umich.edu/afk1140.0001.001. University of Michigan Library Digital Collections. Accessed June 13, 2025.
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