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of the middle and upper
Triassic. These dolomites are separated into a lower and upper dolomite by a ten-metre-thick band of slightly metamorphosed
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Although this layer is thin, it produces a clear morphological division. At the bottom of the
Mesozoic sediments is a sequence of
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that still exists today. The external appearance of the Kalkkögel resembles the
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deposits, the most important of which were quarried south of the
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In this layer, which is at most a few tens of metres thick, are
505:(in German) (13th ed.), Munich: Bergverlag Rudolf Rother,
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of the upper
Triassic, which lie on its crystalline bedrock.
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For the most part, however, these sediments consist of
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432:South flank of the Kalkkögel, seen from Kreuzjoch
304:and was the basis of the tool industry in the
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213:. The highest point of the Kalkkögel is the
410:North flank of the Kalkkögel seen from the
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201:are a mountain chain that is part of the
30:The Kalkkögel from the northwest, by the
557:Mountain ranges of Tyrol (federal state)
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61:2,804 m above sea level (AA)
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347:Steingrubenwand und Schlicker Zinnen
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316:Individual peaks in the Kalkkögel
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451:Ötztaler und Stubaier Alpen
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217:which reaches a height of
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527:Geology of the Kalkkögel
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495:Walter Klier (2006),
472:Die Mineralien Tirols
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530:at senderswind.at
498:Alpenvereinsführer
392:Niederer Burgstall
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40:Highest point
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414:(Senderstal)
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280:Raibler beds
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185:Type of rock
155:Parent range
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552:Stubai Alps
532:(in German)
412:Kemater Alm
377:Widdersberg
327:Ampferstein
226:Ampferstein
221:m (AA)
219:2,804
203:Stubai Alps
173:Age of rock
140: /
541:Categories
489:Literature
438:References
367:Riepenwand
291:sandstones
253:Tribulaune
128:11°16′00″E
125:47°09′00″N
310:Dolomites
306:Stubaital
302:Burgstall
272:dolomites
241:sediments
199:Kalkkögel
67:Geography
56:Elevation
19:Kalkkögel
298:iron ore
261:Triassic
238:Mesozoic
190:dolomite
178:Triassic
263:to the
257:Permian
245:Wipptal
232:Geology
211:Austria
167:Geology
108:Austria
509:
478:
457:
276:slates
265:Norian
249:Serles
502:alpin
322:Saile
207:Tyrol
104:Tyrol
100:State
507:ISBN
476:ISBN
455:ISBN
289:and
197:The
45:Peak
293:.
282:.
205:in
543::
209:,
106:,
259:-
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