Search Nevada County Historical Archive
Enter a name, company, place or keywords to search across this item. Then click "Search" (or hit Enter).
To search for an exact phrase, use "double quotes", but only after trying without quotes. To exclude results with a specific word, add dash before the word. Example: -Word.

Collection: Books and Periodicals > Mining & Scientific Press

Volume 28 (1874) (430 pages)

Go to the Archive Home
Go to Thumbnail View of this Item
Go to Single Page View of this Item
Download the Page Image
Copy the Page Text to the Clipboard
Don't highlight the search terms on the Image
Show the Page Image
Show the Image Page Text
Share this Page - Copy to the Clipboard
Reset View and Center Image
Zoom Out
Zoom In
Rotate Left
Rotate Right
Toggle Full Page View
Flip Image Horizontally
More Information About this Image
Get a Citation for Page or Image - Copy to the Clipboard
Go to the Previous Page (or Left Arrow key)
Go to the Next Page (or Right Arrow key)
Page: of 430  
Loading...
An illustrated Journal of Mining, Popular Science and Progressive Industry. BY DEWLY & CO., = Patent Solicitore. “ SAN FRANCISCO, SATURDAY, JANUARY 3, 1874, ! VOLUME XXVIII Number 1. Snow-Shoeing in the Sierras. {Written for tho Pares by 0. W. Hervey.) Near the snmmit of the Slerra ’ Nevada Monntains, on the’ borders, of the ‘conntics of Sierra and Plumas, are the towns of La Porte, Howland Fiat, St. Louis, noted during the “flush times” of California for their enormous yield of gold dust, and still retaining . fixed characteristics The-climate is very salubrious; most deaths oconr from greatintemperance, éxposnre, accidents and violence, “The spring, gumimer and. autnmn months. will compare, favorably with the climate of ‘northern! Italy. . The excessive heat prevailing jn‘ the valleys lasts for ‘a few days, and ‘only for a few honrs during each, afternoon, The winter months are often very severs, but even duting the prevalence of the; great, storms, thes cold ‘is::not,.so severe.as in. the Eastern States in the same latitnde at a less altitnde, while the snow falls to a great of the typical ‘honést, depth in these high altitndes. It falls as mnoh as 60 to 125 feet during. onc season In some places; thongh generally there is bnt little in the lower valleys. When the snow attainsa considerable depth in the Sierras, locomotion can only be accomplished by means of the celebrated ‘‘Norwegian snow-shoes,”’ or ‘“‘Norway skates,’’ withont which travel would be nearly imprao= _——— SS » SNOW-SHOB RACING ticable, sincs it becomes.almost impossible ‘to break roads or trails,"where the snow often covers buildings evsn two stories high, so that people can only make their -exit ,from their, honses throngh the upper windows.'; It sometimes-happeéns that a resident had to climb ont throngh his chimney, after pnnohing a hole. throngh the. snow above iti: 6 ii 14 L ' ~ Bnow-shogs’ for-'traveling are from 8 to ‘1 feet long, 34 to 4 inches, wide, ahd'134 inches} thick in the center.; They .ars tapered at tha ‘top from “hear the middle to one-fourth of an inch in thickness at the toes, and nearly flat. The toes are turned np like sleigh rnnners, . feet im length, from 3% to 434 inches in width, They are nearly of nniform width from end to end—as little wider, if any, on the front—and a spring is worked in, so that withont welghts they rest on the heels and points; bnt when the rider stands on them, the weight is somewhat evenly distributed, and'a concave groove is made at the bottom, beginning near the toes and running to the heels, similar to the bottom: of the skates. The bottoms are highly polished, MOUNTAINS OF CALIFORNIA. and tar is barned and robbed in natil a full, mahogony-like finish is obtained, which hardens the wood, makes a smooth surface, and at. itracts heat when exposed to the snn—the latter being a desideratum in pntting on the’ “dope” when traveling. § . % “Shoes made for racing are from 10% to 138%) wider on'the front part than‘on the back. ‘Where the turn commences to, the heel, or back end of the shoe, there is a ,finted or; concave groove abont % of an inch deep at the heel and taperingin depth from the tnrn at the point. This groove is abont 1% inch wide, narrower at back end ‘than in front. On top of the shoes, 4 littleback'from the oenter, there is ahout 18 inches of wood left flat, and toward the front they are shaved and planed, tapering snfficiently to leave the point springy. Thsre is coneiderable wood left behind from the ' center to the snd, which makes the proper balance~little or no spring being reqnired on the baok part—the most essential being the front. The t S oa T ‘object of thigis, that in running ovsr rongh ‘places, there will be'nosndden jerk endangerng the equilibrium of the rider, who often attains a speed of 60 to 80 miles an honr on these shoes. They have a tendency to “‘bnek’* when going over nneven snow, and the rider loften finds that they are as uncertain as. all other things are here below. So great have heen the imptovements made in racing shoes, during the past faw years, from. the original style, first introdnced 20 years ago, that they now appear to Have redched perfection. The rider stands a little back of the center, [Continued on Page 9.]