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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,
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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
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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.
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281:. At the top of the butte, a statue of the virgin Mary and a panoramic view.
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158:. The sediments deposited in the basin are affected by numerous
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to distinguish it from the others. The name is derived from the
144:, that formed in response to compressional deformation of the
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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
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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
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254:– Celebrated for its romanesque sculptures
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266:French Towns and Lands of Art and History
287:— For its 18th century château with its
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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
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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
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31:
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248:– Romanesque basilica
71:, on the edge of the
40:French pronunciation:
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21:
361: /
271:Usson, Puy-de-DĂ´me
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24:
293:suspension bridge
279:orgues basaltique
264:city, one of the
242:– For its château
104:, or large lake.
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399:Plains of France
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235:Château de Ravel
136:, including the
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217:village with a
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170:intrusion into
140:, known as the
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65:Auvergne region
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44:[limaɲ]
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394:Massif Central
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295:built in 1830.
289:English garden
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95:Grande Limagne
73:Massif Central
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365:46.0°N 3.25°E
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118:normal faults
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231:of St Julien
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138:Rhine Graben
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102:Lacus Magnus
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94:
78:départements
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69:Allier river
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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:(
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