172:
117:
110:
26:
595:. Northern branches of Pannonian Basin were penetrating the Tatra-Fatra Area and formed inter-mountain basins. Simultaneously with the immersion of the horsts, ongoing and intense erosion is denuding the mountains and supplies the basin with clastic sediments. Among all of the rocks, the most erosion resistant were the crystalline schists and granites of the Tatric. Similar fold and thrust model of origin is known from the other areas of alpine system. In the
836:
447:
153:, Choč Mountains, Greater Fatra, Horehronské podolie, Hornád Basin, Kozie chrbty, Lesser Fatra, Little Carpathians, Low Tatras, Považský Inovec, Staré Hory Mountains, Strážov Mountains, Sub-Tatra Basin, Súľov Mountains, Tatras, Tríbeč, Turiec Basin, Upper Nitra Basin, Žilina Basin and Žiar
563:
units. Fatric had the same basement as the
Veporic unit and is considered as former northern part of Veporic, but later during the thrusting its substratum was consumed and subducted. Surface occurrences of Fatric basement remained only as a remnants in the northern part of Veporic
568:
and few other areas. Choč Nappe, was thrust from the southern area, but its roots were probably consumed entirely, so its paleogeographic position is not exactly known. Choč Nappe is considered as rootless nappe.
672:
581:
460:
1059:
565:
1079:
1064:
479:
432:
1110:
540:
279:
287:
516:
470:
310:
504:
255:
904:
223:
667:
548:
707:
456:
66:
291:
555:). Krížňa Nappe is dominantly composed of rock, that were formed in the Zliechov basin. It was situated in the Fatric area between the
560:
835:
556:
552:
544:
500:
488:
349:
318:
314:
298:
588:
present day mountain ranges. In the
Neogene, further orogene movement in the external part of Carpathian arc caused formation of
815:
811:
511:, that caused movement of large masses of rocks to the North and Northeast. To the South of the Tatric area a 2 superficial
1105:
109:
572:
After the end of main Eo-Alpine orogenic movement, the area of
Western Carpathians was still not so mountainous. In the
700:
1043:
951:
914:
941:
760:
693:
871:
685:
961:
792:
716:
59:
876:
797:
894:
802:
787:
886:
853:
779:
769:
737:
283:
188:
150:
974:
946:
208:
755:
604:
263:
235:
420:
171:
1084:
1033:
866:
306:
1069:
928:
745:
720:
600:
231:
219:
765:
8:
1074:
1037:
989:
861:
844:
821:
728:
337:
192:
908:
380:
329:
302:
271:
25:
997:
969:
428:
372:
936:
596:
519:, were detached and thrust over the Tatric. These nappes are generally composed of
496:
356:
353:
267:
222:. Mountains of the area are located in two ranges. The external range consists of
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807:
676:
592:
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528:
333:
227:
589:
508:
440:
247:
158:
275:
1099:
715:
651:
Princípy regionalizácie geologickej stavby Malých Karpát a Považského Inovca.
412:
360:
81:
68:
239:
436:
400:
392:
388:
376:
251:
212:
1017:
384:
636:
Plašienka, D., Grecula, P., Putiš, M., Kováč, M. a
Hovorka, D., 1997:
573:
532:
520:
404:
368:
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259:
424:
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196:
1002:
446:
363:
and locally also a sedimentary cover of various thickness. In the
416:
408:
200:
638:
Evolution and structure of the
Western Carpathians: an overview.
1007:
577:
243:
204:
49:
411:, which accompanied the Hercynian collision (generally in the
328:
is derived from the structural element, resistant crystalline
1012:
536:
512:
657:
Zborník 2006, Univerzita
Komenského, Bratislava, p. 51 – 56
524:
218:
The Fatra-Tatra Area is from the northern side bounded by
403:). Regional and contact metamorphism was induced also by
576:
subsidence along the normal faults caused formation of
625:
Geomorfologické členenie SSR a ČSSR. Časť Slovensko.
348:
The basement of the core mountains is formed by the
655:
Nové metódy a výsledky v geológii Západných Karpát.
450:Schematic cross section through the core mountain:
419:and at the end of the Paleozoic affected by marine
207:. The highest summit of the whole Carpathians, the
30:
Kolový štít and Jahňací štít over Veľké Biele Pleso
660:
1097:
640:Mineralia Slovaca - Monograph, Košice, s. 1 – 24
175:Extent of the Fatra-Tatra Area (red) in Slovakia
701:
211:at 2,655 m (8,711 ft), lies in the
415:). Basement rocks were later exposed due to
129:Location of the Fatra-Tatra Area in Slovakia
1111:Mountain ranges of the Western Carpathians
708:
694:
679:Univerzita Komenského, Bratislava, 43 p.
666:Hók, J., Kahan, Š., Aubrecht, R., 2001.
445:
435:, deposited. They generally consists of
371:deposited in the area, but later during
170:
286:. The southern boundary of Area is the
1098:
375:, sediments were metamorphosed in the
352:Unit, which is composed of dominantly
689:
599:terminology, similar model is called
116:
13:
309:sedimentary cover, over which the
215:range which belongs to this area.
185:Tatra-Fatra Belt of core mountains
14:
1122:
627:Slovenská kartografia, Bratislava
297:The Tatra-Fatra Belt consists of
834:
582:Inner Carpathian Paleogene Basin
115:
108:
24:
1044:Outer Subcarpathian depressions
952:Retezat-Godeanu Mountains group
915:Moldavian-Muntenian Carpathians
603:, it is typical in the area of
199:with small parts reaching into
643:
630:
617:
187:(in geology) is a part of the
1:
653:In: Kováč, M., Dubíková, K.,
610:
539:. The lower nappes is called
962:Western Romanian Carpathians
793:Central Moravian Carpathians
719:, Groups, and Ranges of the
623:Mazúr, E., Lukniš, M. 1986:
423:that lasted till the end of
336:, often forming the highest
142:Slovakia, Austria and Poland
54:2,655 m (8,711 ft)
7:
1106:Mountain ranges of Slovakia
798:Slovak-Moravian Carpathians
367:clastic and volcanoclastic
332:, preserved in the core of
258:). Inner range consists of
195:. Most of the area lies in
10:
1127:
895:Central Beskidian Piedmont
872:Căliman-Harghita Mountains
803:Western Beskidian Piedmont
788:South-Moravian Carpathians
183:(in geomorphology) or the
1052:
1026:
988:
960:
927:
885:
877:Giurgeu-Brașov Depression
852:
843:
832:
778:
770:North Hungarian Mountains
761:Lučenec-Košice Depression
736:
727:
383:(forming large amount of
343:
189:Inner Western Carpathians
165:Inner Western Carpathians
157:
146:
138:
102:
97:
58:
48:
40:
35:
23:
18:
756:Slovak Central Mountains
290:, south of which is the
942:Făgăraș Mountains group
191:, a subprovince of the
975:Poiana Ruscă Mountains
947:Parâng Mountains group
503:Unit, was affected by
492:
176:
1085:Ukrainian Carpathians
1060:Hungarian Carpathians
1034:Transylvanian Plateau
649:Plašienka, D., 2006:
449:
427:. During this period
174:
1070:Romanian Carpathians
929:Southern Carpathians
746:Slovak Ore Mountains
721:Carpathian Mountains
601:Fault-block mountain
489:Crystalline basement
220:Pieniny Klippen Belt
1075:Serbian Carpathians
1053:Grouping by country
1038:Transylvanian Plain
990:Serbian Carpathians
862:Vihorlat-Gutin Area
845:Eastern Carpathians
822:Podhale-Magura Area
729:Western Carpathians
669:Geológia Slovenska.
547:) and the upper is
301:alpine crystalline
193:Western Carpathians
78: /
1080:Slovak Carpathians
1065:Polish Carpathians
909:Polonynian Beskids
867:Bistrița Mountains
675:2011-07-19 at the
493:
480:Tatric cover units
433:Tatric cover units
381:amphibolite facies
340:of the mountains.
274:, Ďumbier part of
177:
36:Highest point
1093:
1092:
998:Homolje Mountains
970:Apuseni Mountains
923:
922:
830:
829:
766:Mátra-Slanec Area
580:- intra-mountain
463:sedimentary cover
429:sedimentary rocks
373:Hercynian orogeny
209:Gerlachovský štít
169:
168:
82:49.167°N 20.133°E
44:Gerlachovský štít
1118:
1027:Adjacent regions
937:Bucegi Mountains
850:
849:
838:
751:Fatra-Tatra Area
734:
733:
710:
703:
696:
687:
686:
680:
664:
658:
647:
641:
634:
628:
621:
517:Subtatric Nappes
497:Upper Cretaceous
486:
477:
471:Subtatric Nappes
468:
454:
311:Subtatric nappes
236:Strážovské vrchy
230:(Pezinok part),
181:Fatra-Tatra Area
161:
119:
118:
112:
93:
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83:
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28:
16:
15:
1126:
1125:
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1120:
1119:
1117:
1116:
1115:
1096:
1095:
1094:
1089:
1048:
1022:
1003:Kučaj Mountains
984:
980:Banat Mountains
956:
919:
905:Eastern Beskids
900:Central Beskids
881:
839:
826:
816:Central section
812:Eastern section
808:Western Beskids
774:
723:
714:
684:
683:
677:Wayback Machine
665:
661:
648:
644:
635:
631:
622:
618:
613:
605:Basin and Range
593:Pannonian Basin
491:
484:
482:
475:
473:
466:
464:
452:
441:carbonate rocks
391:, only locally
346:
321:) were thrust.
256:Belianske Tatry
232:Považský Inovec
159:
134:
133:
132:
131:
130:
127:
126:
125:
124:
120:
86:
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31:
12:
11:
5:
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731:
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724:
713:
712:
705:
698:
690:
682:
681:
659:
642:
629:
615:
614:
612:
609:
566:Veľký Bok Unit
509:Alpine Orogeny
483:
474:
465:
451:
345:
342:
330:basement rocks
326:core mountains
288:Čertovica line
278:and massif of
224:Hainburg Hills
167:
166:
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155:
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136:
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128:
122:
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114:
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87:49.167; 20.133
62:
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52:
46:
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42:
38:
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33:
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21:
20:
9:
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930:
926:
916:
913:
910:
906:
903:
901:
898:
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893:
892:
890:
888:
887:Outer Eastern
884:
878:
875:
873:
870:
868:
865:
863:
860:
859:
857:
855:
854:Inner Eastern
851:
848:
846:
842:
837:
823:
820:
817:
813:
809:
806:
804:
801:
799:
796:
794:
791:
789:
786:
785:
783:
781:
780:Outer Western
777:
771:
767:
764:
762:
759:
757:
754:
752:
749:
747:
744:
743:
741:
739:
738:Inner Western
735:
732:
730:
726:
722:
718:
711:
706:
704:
699:
697:
692:
691:
688:
678:
674:
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663:
656:
652:
646:
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633:
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608:
606:
602:
598:
594:
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587:
583:
579:
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558:
554:
550:
546:
542:
538:
534:
530:
526:
522:
518:
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510:
506:
502:
498:
490:
481:
472:
462:
458:
448:
444:
442:
438:
434:
430:
426:
422:
421:transgression
418:
414:
413:Carboniferous
410:
406:
402:
398:
394:
393:orthogneisses
390:
386:
382:
378:
374:
370:
366:
362:
361:igneous rocks
358:
355:
351:
341:
339:
335:
331:
327:
322:
320:
316:
312:
308:
307:autochthonous
304:
300:
295:
293:
289:
285:
281:
277:
273:
272:Chočské vrchy
269:
265:
261:
257:
253:
249:
245:
241:
237:
233:
229:
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221:
216:
214:
210:
206:
202:
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182:
173:
164:
162:
156:
152:
149:
145:
141:
137:
111:
101:
96:
91:
63:
61:
57:
53:
51:
47:
43:
39:
34:
27:
22:
17:
750:
668:
662:
654:
650:
645:
637:
632:
624:
619:
571:
541:Krížna Nappe
531:and less by
515:, so called
494:
401:mica schists
389:amphibolites
385:paragneisses
347:
325:
323:
296:
228:Malé Karpaty
217:
184:
180:
178:
160:Parent range
147:Subdivisions
431:, known as
377:greenschist
357:metamorphic
276:Nízke Tatry
268:Veľká Fatra
213:High Tatras
123:Fatra-Tatra
85: /
60:Coordinates
19:Fatra-Tatra
1100:Categories
1018:Deli Jovan
611:References
549:Choč Nappe
533:sandstones
457:Cretaceous
405:intrusions
292:Vepor Belt
280:Smrekovica
240:Malá Fatra
717:Divisions
574:Paleogene
521:limestone
505:Eo-Alpine
461:Paleogene
397:phyllites
369:sediments
365:Paleozoic
354:hercynian
324:The name
139:Countries
98:Geography
50:Elevation
673:Archived
590:back-arc
551:(or the
543:(or the
529:dolomite
499:area of
425:Mesozoic
409:granites
305:and its
303:basement
284:Branisko
197:Slovakia
151:Branisko
597:English
578:grabens
561:Veporic
495:In the
437:clastic
417:erosion
282:in the
248:Western
201:Austria
70:49°10′N
1008:Devica
586:horsts
557:Tatric
553:Hronic
545:Fatric
537:slates
513:nappes
501:Tatric
487:
485:
478:
476:
469:
467:
455:
453:
350:Tatric
344:Origin
334:horsts
319:Hronic
315:Fatric
299:Tatric
260:Tribeč
244:Tatras
205:Poland
73:20°8′E
1013:Rtanj
338:peaks
768:and
584:and
559:and
535:and
525:marl
459:and
439:and
399:and
387:and
379:and
359:and
317:and
264:Žiar
254:and
252:High
203:and
179:The
41:Peak
507:of
407:of
1102::
814:,
607:.
527:,
523:,
443:.
395:,
294:.
270:,
266:,
262:,
250:,
242:,
238:,
234:,
226:,
1040:)
1036:(
911:)
907:(
818:)
810:(
709:e
702:t
695:v
313:(
246:(
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