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in the Czech
Republic, and therefore vines are cultivated here. Because of this climate some plant species that do not occur anywhere else in the country grow here. The colourful mosaic of arid rock grass,
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on the Děvín slopes, which originated partly due to the influence of grazing, is called karst forest steppe. The Děvín forest plateaus are dominated by sparse loess oakwoods together with a species-rich
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in landscape, originally created by animals and later overtaken by humans. The area around base of the mountain is permanently settled longer than last 30,000 years. Since
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226:. With an elevation of 550 metres (1,800 ft), it is the highest mountain of the Pavlov Hills within the
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from that period indicate that limestone may have been already denuded at that time. At 15
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426:. During the following 9 Ma, up to 3 km thick layers of maritime and lacustrine
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330:. Sedimentation of Ernstbrunn limestone was preceded by the sedimentation of
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and quite small areas of alluvial meadows have been preserved in the Dyje
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357:(South moravian carpathians). The flysch beds consist of strongly folded
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of Děvín has the remains of a huge Iron Age hill fort, while the ancient
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layers. All the Pavlov Hills are situated at the margin of the
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The body of the Děvín is strongly modulated, with outcrops and
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is situated on the top. The lower platform is used as an
422:BP (before present) a strong subsidence formed the
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195:Landscape silhouette of the Děvín Massif from west
237:It is located right on trace where runs line of
478:dominates the north-facing slopes and valleys.
272:runs neighbors of the mountains base, and all
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600:Outlook from Děvín summit to Pavlov village
303:The entire Děvín massif consists mainly by
693:Mountain ranges of the Western Carpathians
494:in the vicinity of Křivé lake. Remains of
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688:Mountains and hills of the Czech Republic
410:were surrounded by a warm sea. Pieces of
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442:lies in the northwest promontory of the
307:, i.e. series of rocks generated during
280:hunters, ower Celtic tribes settlement,
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653:Pavlov Hills Botanical excursion guide
564:Vineyeards under Kotel and Děvín hills
260:Aerial view of Děvín Hill in light fog
248:and Thaya/Morava meso-level drainage.
438:Děvín as a whole eastern part of the
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576:Old oak beaten and formed by wind
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66:49.3 km (30.6 mi)
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673:Pálava Protected Landscape Area
631:Pálava Hills in: SummitPost.org
232:Pálava Protected Landscape Area
642:Lower Morava Biosphere Reserve
612:Klentnice as viewed from Děvín
430:were deposited on its bottom.
148:Location in the Czech Republic
1:
532:. It was built in 1979–1980.
406:period (Upper Tertiary), the
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341:and clay limestone, called
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46:550 m (1,800 ft)
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414:present in the littoral
372:. During the periods of
320:hard and white limestone
351:Northern Limestone Alps
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668:Small-scale hikersmap
588:Old route in the rock
505:Summit is covered by
496:halophytic vegetation
474:, while Panonian oak-
391:were torn from their
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220:South Moravian Region
194:
101:48.86944°N 16.64972°E
30:Summit limestone rock
334:Děvín-Kotel massif.
328:Ernstbrunn limestone
316:cliffs (klippe/crag)
218:municipality in the
488:narrow-leaved ashes
374:orogenetic activity
355:Western Carpathians
97: /
380:, large blocks of
305:Jurassic limestone
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106:48.86944; 16.64972
36:Highest point
530:observation tower
440:Mikulov Highlands
228:Mikulov Highlands
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484:pedunculate oaks
480:Riparian forests
472:herbaceous layer
386:Early Cretaceous
214:mountain in the
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397:younger flysch
359:Lower Tertiary
324:Later Jurassic
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282:Roman fortress
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551:Dolní Kounice
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455:communities,
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408:Pavlov Hills
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370:conglomerate
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295:and Děvín).
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180:Pavlov Hills
174:Parent range
453:fringe tree
347:flysch zone
270:Amber Route
212:double peak
208:Mayden Berg
104: /
79:Coordinates
682:Categories
618:References
549:View from
516:and rock.
492:floodplain
293:Strachotín
92:16°38′59″E
89:48°52′10″N
52:Prominence
448:arid area
428:sediments
366:sandstone
362:claystone
343:Klentnice
339:claystone
318:of pure,
289:hillforts
278:Cromagnos
241:of Upper
117:Geography
62:Isolation
42:Elevation
514:pinewood
476:hornbeam
467:oakwoods
382:Jurassic
378:Tertiary
246:drainage
158:Location
536:Gallery
500:Moravia
402:In the
376:in the
349:of the
299:Geology
252:History
222:of the
210:) is a
510:meadow
507:steppe
460:bushes
416:gravel
399:beds.
337:Děvín
266:summit
216:Pavlov
204:German
162:Pavlov
482:with
434:Flora
389:rocks
243:Thaya
200:Děvín
142:Děvín
56:300 m
19:Děvín
486:and
462:and
384:and
368:and
353:and
264:The
520:Top
322:of
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420:Ma
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291:(
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