Knowledge (XXG)

Limagne

Source đź“ť

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de Goer de Herve, A. 2008. Chapter 5, Peperites from the Limagne Trench (Auvergne, French Massif Central), a distinctive feature of phreatomagmatic pyroclastics. History of semantic drift. In: Leyrit, H. & Montenat, C. (Eds.) Volcaniclastic rocks, from magmas to sediments, Taylor & Francis,
50: 93:. The term is sometimes used to include this, and three other less extensive plains, that lie along the valley of the Allier, in which case the first is known as 403: 265: 388: 349: 337: 141: 120:
that border the western edge of the plain. It contains about 2 km of sediments, and the amount of stretching of the
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Allen, P.A. & Allen, J.R. 1990. Basin analysis; Principles and applications, WileyBlackwell, 451pp.
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The Limagne is a very fertile plain and is mainly an area of cereal production, with some tobacco and
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are found along the borders of the plain on the edge of the Massif Central, particularly at
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Ziegler, P.A. 1990. Geological Atlas of Western Europe, Geological Society London, 256pp.
148: 145: 82: 72: 68: 382: 198: 284: 261: 214: 155: 90: 186: 364: 351: 281:. At the top of the butte, a statue of the virgin Mary and a panoramic view. 174: 129: 228: 190: 163: 64: 26: 18: 245: 224: 274: 239: 194: 167: 125: 113: 86: 210: 98: 257: 171: 158:. The sediments deposited in the basin are affected by numerous 133: 97:
to distinguish it from the others. The name is derived from the
144:, that formed in response to compressional deformation of the 22:
Location of the Limagne plain on a map of the Massif Central
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Volcanism accompanied the rifting and continued into the
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and the main phase of subsidence continued into the Late
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is estimated as 1.2–1.3. The rifting started in the Late
132:. The Limagne Graben forms part of a system of linked 30:
The village of Usson on the edge of the Limagne plain
116:, downthrown from the Massif Central by a series of 273:– Ruined fortress walls and the columnar jointed 8: 254:– Celebrated for its romanesque sculptures 322: 320: 266:French Towns and Lands of Art and History 287:— For its 18th century château with its 25: 17: 305: 42: 7: 14: 404:Landforms of Auvergne-RhĂ´ne-Alpes 162:. The area was the first where 67:of France in the valley of the 1: 142:European Cenozoic Rift System 75:. It mainly lies within the 420: 63:) is a large plain in the 389:Landforms of Puy-de-DĂ´me 166:were described, from a 112:The Limagne plain is a 205:Main sites of interest 60: 31: 23: 248:– Romanesque basilica 71:, on the edge of the 40:French pronunciation: 29: 21: 361: /  271:Usson, Puy-de-DĂ´me 32: 24: 293:suspension bridge 279:orgues basaltique 264:city, one of the 242:– For its château 104:, or large lake. 411: 399:Plains of France 376: 375: 373: 372: 371: 366: 362: 359: 358: 357: 354: 341: 335: 329: 324: 315: 310: 235:Château de Ravel 136:, including the 54: 53: 52: 46: 41: 419: 418: 414: 413: 412: 410: 409: 408: 379: 378: 369: 367: 363: 360: 355: 352: 350: 348: 347: 345: 344: 336: 332: 325: 318: 311: 307: 302: 217:village with a 207: 183: 170:intrusion into 140:, known as the 110: 65:Auvergne region 49: 48: 47: 44:[limaɲ] 39: 12: 11: 5: 417: 415: 407: 406: 401: 396: 394:Massif Central 391: 381: 380: 343: 342: 330: 316: 304: 303: 301: 298: 297: 296: 295:built in 1830. 289:English garden 282: 268: 255: 249: 243: 237: 232: 222: 206: 203: 182: 179: 109: 106: 95:Grande Limagne 73:Massif Central 13: 10: 9: 6: 4: 3: 2: 416: 405: 402: 400: 397: 395: 392: 390: 387: 386: 384: 377: 374: 365:46.0°N 3.25°E 340: 334: 331: 328: 323: 321: 317: 314: 309: 306: 299: 294: 290: 286: 283: 280: 276: 272: 269: 267: 263: 259: 256: 253: 250: 247: 244: 241: 238: 236: 233: 230: 226: 223: 220: 216: 212: 209: 208: 204: 202: 200: 196: 192: 188: 180: 178: 176: 173: 169: 165: 161: 157: 152: 150: 147: 143: 139: 135: 131: 127: 123: 119: 118:normal faults 115: 107: 105: 103: 100: 96: 92: 88: 84: 80: 79: 74: 70: 66: 62: 58: 51: 45: 37: 28: 20: 16: 346: 333: 308: 278: 231:of St Julien 184: 153: 138:Rhine Graben 111: 102:Lacus Magnus 101: 94: 78:dĂ©partements 76: 69:Allier river 35: 33: 15: 368: / 285:Parentignat 262:Renaissance 252:Mozac Abbey 156:Pleistocene 91:Haute-Loire 83:Puy-de-DĂ´me 383:Categories 370:46.0; 3.25 300:References 291:, and the 219:romanesque 199:Châteaugay 187:sugar beet 172:lacustrine 160:intrusions 191:Vineyards 175:limestone 164:peperites 130:Oligocene 229:basilica 215:Medieval 168:basaltic 149:foreland 353:46°00′N 246:Issoire 225:Brioude 181:Economy 108:Geology 61:Limanha 57:Occitan 36:Limagne 356:3°15′E 339:270pp. 275:basalt 240:Effiat 227:– The 221:church 195:Corent 146:Alpine 126:Eocene 114:graben 87:Allier 211:Auzon 134:rifts 122:crust 99:Latin 258:Riom 197:and 89:and 34:The 81:of 385:: 319:^ 277:, 260:– 213:– 201:. 189:. 177:. 151:. 85:, 59:: 55:; 38:(

Index



[limaɲ]

Occitan
Auvergne region
Allier river
Massif Central
départements
Puy-de-DĂ´me
Allier
Haute-Loire
Latin
graben
normal faults
crust
Eocene
Oligocene
rifts
Rhine Graben
European Cenozoic Rift System
Alpine
foreland
Pleistocene
intrusions
peperites
basaltic
lacustrine
limestone
sugar beet

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