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Ozokerite

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27: 200:(738 ft), respectively, electrical power is employed for hauling, pumping and ventilating. In these mines there are the usual main shafts and galleries, the ozokerite being reached by levels driven along the strike of the deposit. The wax, as it reaches the surface, varies in purity, and, in new workings especially, only hand-picking is needed to separate the pure material. In other cases much earthy matter is mixed with the material, and then the rock or shale having been eliminated by hand-picking, the "wax-stone" is boiled with water in large coppers, when the pure wax rises to the surface. This is again melted without water, and the impurities are skimmed off, the material being then run into slightly conical cylindrical 309: 20: 199:
The mining of ozokerite began in Galicia in the 1880s, and was formerly carried on by means of hand-labor, but in the ozokerite mines owned by the Boryslaw Actien Gesellschaft and the Galizische Kreditbank, the workings of which extend to a depth of 200 metres (660 ft), and 225 metres
231:-making material resembling the paraffin obtained from petroleum and shale-oil but of higher melting-point, and therefore of greater value if the candles made from it are to be used in hot climates. There are also obtained in the distillation light oils and a product resembling 216:
or cerasin of commerce is obtained. The refined ozokerite or ceresine, which usually has a melting-point of 61 to 78 °C (142 to 172 °F), is largely used as an
247:. From the residue a form of the material known as heel-ball, used to impart a polished surface to the heels and soles of boots, was also manufactured. 26: 147:
in the fissures and crevices previously occupied by the liquid. As found native, ozokerite varies from a very soft wax to a black mass as hard as
258:. It has a higher melting point than most petroleum waxes, and is favored for some applications, such as electrical insulators and candles. 324: 333: 116:
in the United States, deserve mention, though the latter have been largely worked out. The sole sources of commercial supply are in
96:, as well as from about thirty different countries. Of these occurrences the ozokerite of the island (now peninsula) of 183:
and others. Galician ozokerite varies in color from light yellow to dark brown, and frequently appears green owing to
350: 163:
ranges from 0.85 to 0.95, and its melting point from 58 to 100 °C (136 to 212 °F). It is soluble in
56:
found in many localities. Lacking a definite composition and crystalline structure, it is not considered a
187:. It usually melts at 62 °C (144 °F). Chemically, ozokerite consists of a mixture of various 204:, and thus made into blocks for the market. The crude ozokerite is refined by treatment first with 117: 320: 235:. The residue in the stills consists of a hard, black, waxy substance, which in admixture with 371: 244: 129: 101: 31: 8: 97: 346: 201: 180: 160: 224:, and is frequently colored artificially to resemble that product in appearance. 366: 144: 136: 89: 65: 360: 328: 315: 205: 164: 267: 251: 236: 135:
Ozokerite deposits are believed to have originated in much the same way as
53: 188: 337:. Vol. 20 (11th ed.). Cambridge University Press. p. 430. 217: 176: 172: 128:, though the mineraloid is found at other points on both flanks of the 61: 227:
On distillation in a current of superheated steam, ozokerite yields a
255: 184: 140: 105: 345:(Harvard Historical Studies). Harvard University Press. p. 98. 232: 213: 209: 125: 121: 85: 314:
This article incorporates text from a publication now in the
250:
Mining of ozokerite diminished after 1940 due to competition from
240: 221: 168: 57: 19: 228: 191:, containing 85–87% by weight of carbon and 14.3% of hydrogen. 148: 109: 93: 113: 52:, is a naturally occurring odoriferous mineral wax or 343:
Oil Empire: Visions of Prosperity in Austrian Galicia
291: 289: 287: 285: 283: 280: 358: 139:, the slow evaporation and oxidation of 25: 18: 319: 295: 359: 145:deposition of its dissolved paraffin 13: 84:Specimens have been obtained from 14: 383: 307: 239:was employed under the name of 1: 273: 154: 44:, archaically referred to as 341:Frank, Alison Fleig (2005). 7: 261: 64:. The name was coined from 10: 388: 79: 194: 208:, and subsequently with 334:Encyclopædia Britannica 143:having resulted in the 72:, to stink, and κηρός 34: 23: 29: 22: 245:electrical insulator 112:and the deposits of 32:Wasatch County, Utah 254:manufactured from 35: 24: 321:Redwood, Boverton 379: 338: 313: 311: 310: 299: 293: 181:carbon disulfide 161:specific gravity 124:, Dzwiniacz and 387: 386: 382: 381: 380: 378: 377: 376: 357: 356: 308: 306: 303: 302: 294: 281: 276: 264: 197: 157: 104:, parts of the 102:Türkmenbaşy Bay 82: 17: 12: 11: 5: 385: 375: 374: 369: 355: 354: 339: 329:Chisholm, Hugh 301: 300: 278: 277: 275: 272: 271: 270: 263: 260: 196: 193: 156: 153: 90:Northumberland 81: 78: 15: 9: 6: 4: 3: 2: 384: 373: 370: 368: 365: 364: 362: 352: 351:0-674-01887-7 348: 344: 340: 336: 335: 330: 326: 322: 317: 316:public domain 305: 304: 297: 292: 290: 288: 286: 284: 279: 269: 266: 265: 259: 257: 253: 248: 246: 242: 238: 234: 230: 225: 223: 219: 215: 211: 207: 206:sulfuric acid 203: 192: 190: 186: 182: 178: 174: 170: 167:, petroleum, 166: 162: 152: 150: 146: 142: 138: 137:mineral veins 133: 131: 127: 123: 119: 115: 111: 107: 103: 99: 95: 91: 87: 77: 75: 71: 68:elements Όζω 67: 63: 59: 55: 51: 47: 43: 39: 33: 28: 21: 372:Hydrocarbons 342: 332: 296:Redwood 1911 268:Zietrisikite 249: 237:India-rubber 226: 198: 189:hydrocarbons 158: 134: 83: 73: 69: 49: 45: 41: 37: 36: 212:, when the 130:Carpathians 60:but only a 30:Ozokerite, 16:Mineral wax 361:Categories 274:References 218:adulterant 177:chloroform 173:turpentine 155:Properties 62:mineraloid 325:Ozokerite 323:(1911). " 256:petroleum 252:paraffins 185:dichroism 141:petroleum 106:Himalayas 50:earth wax 42:ozocerite 38:Ozokerite 262:See also 233:vaseline 214:ceresine 210:charcoal 126:Starunia 122:Boryslav 98:Cheleken 86:Scotland 54:paraffin 46:earthwax 331:(ed.). 318::  241:okonite 222:beeswax 169:benzene 118:Galicia 100:, near 80:Sources 76:, wax. 58:mineral 349:  327:". In 312:  243:as an 229:candle 202:moulds 195:Mining 149:gypsum 367:Waxes 165:ether 120:, at 110:India 94:Wales 74:keros 66:Greek 347:ISBN 159:Its 114:Utah 220:of 108:in 70:ozο 48:or 40:or 363:: 282:^ 179:, 175:, 171:, 151:. 132:. 92:, 88:, 353:. 298:.

Index



Wasatch County, Utah
paraffin
mineral
mineraloid
Greek
Scotland
Northumberland
Wales
Cheleken
Türkmenbaşy Bay
Himalayas
India
Utah
Galicia
Boryslav
Starunia
Carpathians
mineral veins
petroleum
deposition of its dissolved paraffin
gypsum
specific gravity
ether
benzene
turpentine
chloroform
carbon disulfide
dichroism

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