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Sidobre

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The Sidobre is an important zone of quarrying, representing half of the granite production in France, with about 1,200 employees and 100 companies. Because of competition from China, there has been a steady decrease in the number of quarries since the 1950s, with barely fifteen nowadays, though these
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This stunning site, with its dozens of huge strange-shaped rocks, is unique in Europe (other sites exist in France, but in a much smaller scale), and has inspired many legends and tales.
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have grown bigger. The granite is used for many purposes: pavements, airport runways, funerary art...
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Originally composed by one single piece of rock, the Sidobre was cracked by the
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The site and its environment have been placed under the protection of the
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The Sidobre, while just adjacent to it, is totally independent from the
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resulting from a Hercynian intrusion dated back (using the
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Le Roc de l'Oie (« The Rock of the Goose Â»)
247: 242: 227: 188: 170: 156: 148: 143: 135: 130: 120: 112: 107: 88: 475:While mass tourism is still uncommon in the area, 266:is a mountainous area located in the south of the 43:but its sources remain unclear because it lacks 406:Le Peyro Clabado, on the commune of Lacrouzette 341:metamorphic rocks. In the central part of the 101:Location of Sidobre within the Massif Central 8: 296:department, at the South-Western end of the 479:also contributes to the Sidobre's economy. 85: 74:Learn how and when to remove this message 396: 7: 368:, thus becoming more exposed to the 484:Haut-Languedoc Regional Nature Park 274:. It consists of a plateau made of 14: 304:East : the Mounts of Lacaune 447: 435: 423: 411: 399: 325:The granite of the Sidobre is a 95: 20: 139:88 km (34 sq mi) 528:Geography of Tarn (department) 1: 387:and the channel of the river 379:. They are separated by the 345:, the granite is a slightly 454:Trembling rock in Sept-Faux 544: 126:707 m (2,320 ft) 442:Waterfall in the Sidobre 331:Rubidium-Strontium method 313:West : territory of 93: 29:This article includes a 183:Saint-Salvy-de-la-Balme 58:more precise citations. 468: 467: 292:It is located in the 284:“Le Patau” (707 m). 508:Sidobre-information 208: /  469: 108:Highest point 31:list of references 381:sedimentary basin 307:South : the 260: 259: 190:Range coordinates 84: 83: 76: 535: 451: 439: 427: 418:Le Peyro Clabado 415: 403: 366:Pyrenean orogeny 232:Monts de Lacaune 223: 222: 220: 219: 218: 213: 212:43.633°N 2.400°E 209: 206: 205: 204: 201: 99: 86: 79: 72: 68: 65: 59: 54:this article by 45:inline citations 24: 23: 16: 543: 542: 538: 537: 536: 534: 533: 532: 513: 512: 504: 496:Tourism in Tarn 492: 462: 455: 452: 443: 440: 431: 428: 419: 416: 407: 404: 362: 323: 290: 216: 214: 210: 207: 202: 199: 197: 195: 194: 103: 102: 80: 69: 63: 60: 49: 35:related reading 25: 21: 12: 11: 5: 541: 539: 531: 530: 525: 523:Massif Central 515: 514: 511: 510: 503: 502:External links 500: 499: 498: 491: 488: 461: 458: 457: 456: 453: 446: 444: 441: 434: 432: 429: 422: 420: 417: 410: 408: 405: 398: 377:Montagne Noire 361: 358: 322: 319: 318: 317: 311: 309:Montagne Noire 305: 298:Massif central 289: 286: 268:Massif central 258: 257: 251: 245: 244: 240: 239: 236:Montagne Noire 229: 225: 224: 192: 186: 185: 172: 168: 167: 158: 154: 153: 150: 146: 145: 141: 140: 137: 133: 132: 128: 127: 124: 118: 117: 114: 110: 109: 105: 104: 100: 94: 91: 90: 82: 81: 39:external links 28: 26: 19: 13: 10: 9: 6: 4: 3: 2: 540: 529: 526: 524: 521: 520: 518: 509: 506: 505: 501: 497: 494: 493: 489: 487: 485: 480: 478: 477:local tourism 473: 466: 459: 450: 445: 438: 433: 426: 421: 414: 409: 402: 397: 395: 392: 390: 386: 382: 378: 373: 371: 367: 359: 357: 355: 351: 348: 344: 340: 336: 333:) to 304 ± 8 332: 328: 327:plutonic rock 320: 316: 312: 310: 306: 303: 302: 301: 299: 295: 287: 285: 283: 282: 277: 273: 270:, in central 269: 265: 255: 252: 250: 246: 241: 237: 233: 230: 226: 221: 217:43.633; 2.400 193: 191: 187: 184: 180: 176: 173: 169: 166: 165:Midi-PyrĂ©nĂ©es 162: 159: 155: 151: 147: 142: 138: 134: 129: 125: 123: 119: 115: 111: 106: 98: 92: 87: 78: 75: 67: 57: 53: 47: 46: 40: 36: 32: 27: 18: 17: 481: 474: 470: 393: 374: 363: 350:granodiorite 342: 324: 291: 279: 263: 261: 249:Type of rock 238:and Castrais 70: 61: 50:Please help 42: 215: / 175:Lacrouzette 171:Settlements 56:introducing 517:Categories 370:rhexistasy 228:Borders on 131:Dimensions 354:monzonite 347:porphyric 179:Ferrières 144:Geography 122:Elevation 64:June 2024 490:See also 339:Cambrian 288:Location 281:lieu-dit 116:Le Patau 460:Economy 385:Castres 321:Geology 315:Castres 276:granite 264:Sidobre 254:granite 243:Geology 200:43°38′N 149:Country 89:Sidobre 52:improve 343:massif 272:France 203:2°24′E 157:Region 152:France 389:ThorĂ© 360:Sites 37:, or 294:Tarn 262:The 256:rock 181:and 161:Tarn 136:Area 113:Peak 391:”. 383:of 519:: 486:. 356:. 335:Ma 234:, 177:, 163:, 41:, 33:, 77:) 71:( 66:) 62:( 48:.

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Elevation
Tarn
Midi-Pyrénées
Lacrouzette
Ferrières
Saint-Salvy-de-la-Balme
Range coordinates
43°38′N 2°24′E / 43.633°N 2.400°E / 43.633; 2.400
Monts de Lacaune
Montagne Noire
Type of rock
granite
Massif central
France
granite
lieu-dit
Tarn
Massif central
Montagne Noire
Castres
plutonic rock
Rubidium-Strontium method

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