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and usually divided from north to south into three segments (or blocks). Basement rocks are in the northern portion dominated by crystalline schists (mostly diaphthorites,
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crystalline basement composed of granitoids and gneisses, covered by the
Mesozoic deposits and two superimposed cover nappes (lower Fatric unit and upper Hronic unit).
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311:[Lithostratigraphy and sedimentogenesis of the Upper Paleozoic Formations in the northern part of the Považský Inovec Mts. (Western Carpathians, Slovakia)]
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View of the northern portion of the Považskský Inovec Mts. from the Trenčianske
Stankovece. The highest mountain in the center is Inovec (1042 m).
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river. It is 48 km (30 mi) long and 15–25 km (9-16 mi) wide mountain range. It is situated from the city of
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309:"Litostratigrafia a sedimentogenéza vrchnopaleozoických súvrství v severnej časti Považského Inovca"
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There are many monuments in or near the mountain range, including
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Geologická stavba československých Karpát: Paleoalpínske jednotky
58:, where is also the highest hill of the entire mountain range,
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288:(in Slovak). Vol. 1. Bratislava: Veda. pp. 310–329.
62:(1042 m). The mountain range separates basins of the Váh and
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have yielded relics of multiple human habitation from the
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191:rocks form the Bojná and the Zlatníky massifs. The
235:are found on the western slopes of the mountains.
119:emerging from the Neogene sedimentary fill of the
115:Považský Inovec Mts. is considered as asymmetric
365:Slovakia and the Slovaks: A Concise Encyclopedia
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211:rocks. Both cover nappes are composed of the
203:nappe is preserved in outlayers, e.g. in the
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490:Mountain ranges of the Western Carpathians
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363:Strhan, Milan; Daniel, David P. (1994).
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131:rivers. The horst is bordered by steep
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259:culture (associated primarily with
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233:Inner-Carpathian Paleogene Basin
159:volcanosedimentary succession (
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183:which is typical composed of
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195:nappe is represented by the
107:lies under Považský Inovec.
485:Mountain ranges of Slovakia
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352:. Kubko-Goral. p. 18.
348:Pšenková, Vlasta (1994).
307:Olšlavský, Mário (2008).
103:. The famous spa city of
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350:Pozoruhodnosti Slovenska
323:: 1–16. Archived from
284:Maheľ, Michal (1986).
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54:where it borders the
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398:48.667°N 18.000°E
317:Mineralia Slovaca
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332:. Retrieved
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261:Neanderthals
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239:Paleontology
149:amphibolites
123:between the
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247:caves near
245:Čertova pec
177:Belice unit
175:sediments (
141:micaschists
137:phyllonites
34:in western
479:Categories
334:2012-08-13
271:References
257:Mousterian
225:marlstones
221:limestones
153:migmatites
139:, biotite
432:geography
294:750488266
267:culture.
265:Szeletian
253:Stone Age
229:dolomites
189:Granitoid
74:hill fort
249:Radošina
213:Triassic
145:gneisses
105:Piešťany
77:Kostolec
66:rivers.
44:Hlohovec
36:Slovakia
389:18°00′E
386:48°40′N
205:Tematín
111:Geology
52:Trenčín
429:Slovak
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201:Hronic
199:. The
193:Fatric
185:Tatric
169:Hrádok
93:Beckov
81:Ducové
60:Inovec
427:This
328:(PDF)
313:(PDF)
165:Selec
129:Nitra
117:horst
91:near
79:near
64:Nitra
30:is a
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290:OCLC
243:The
227:and
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127:and
99:and
215:to
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125:Váh
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