36:
20:
115:. This would indicated that Paleozoic strata that covered much of Fennoscandia elsewhere had been locally uplifted and eroded prior to the formation of the Sub-Mesozoic hilly relief.
179:; Bonow, Johan M.; Japsen, Peter (2013). "Stratigraphic Landscape Analysis and geomorphological paradigms: Scandinavia as an example of Phanerozoic uplift and subsidence".
1009:
448:
88:. Later erosion of the cover rocks partly re-exposed this landscape. During the Quaternary epoch the re-exposed Mesozoic hilly relief escaped major
142:. In parts this surface and unconformity makes up an undulating hilly relief, while in other locations like Blekinge and northern Halland it is an
1004:
994:
999:
296:"The South Swedish Dome: a key structure for identification of peneplains and conclusions on Phanerozoic tectonics of an ancient shield"
882:
434:
220:(2008). "Patterns of Quaternary ice sheet erosion and deposition in Fennoscandia and a theoretical framework for explanation".
963:
441:
1034:
573:
548:
348:"The major landforms of the bedrock of Sweden–with a view on the relationships between physical geography and geology"
181:
938:
892:
686:
498:
257:
Lidmar-Bergström, Karna (1993). "Denudation surfaces and tectonics in the southernmost part of the Baltic Shield".
1024:
1019:
912:
666:
343:
176:
150:
associated with hilly relief is likely also responsible for creating the numerous small rock basins carved into
1014:
948:
1029:
843:
788:
508:
503:
395:
222:
119:
24:
958:
897:
833:
518:
143:
973:
917:
853:
112:
35:
19:
953:
691:
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404:
361:
309:
268:
259:
231:
190:
78:
40:
838:
681:
933:
614:
493:
352:
757:
661:
135:
118:
The Sub-Mesozoic hilly peneplains covers a contiguous zone along western and southern rims of the
633:
393:; Olvmo, Mats (2001). "Development of joint-controlled rock basins in Bohus granite, SW Sweden".
325:
762:
727:
722:
651:
108:
907:
818:
412:
369:
317:
276:
239:
198:
85:
968:
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568:
295:
89:
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194:
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604:
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553:
483:
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457:
329:
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868:
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243:
71:
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347:
321:
887:
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123:
60:
848:
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619:
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147:
82:
767:
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131:
104:
813:
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737:
609:
540:
127:
100:
67:
44:
28:
823:
707:
139:
64:
430:
294:
Lidmar-Bergström, Karna; Olvmo, Mats; Bonow, Johan M. (2017).
16:
Landscape in
Scandinavia of undulating hills and joint valleys
63:
made up of undulating hills and joint valleys and occasional
360:(1). Swedish Society for Anthropology and Geography: 1–11.
107:. Remnants of this peneplain can be traced as a tilted
95:
The Sub-Mesozoic hilly relief formed starting from a
926:
866:
781:
700:
641:
632:
592:
539:
532:
464:
74:and was eventually drowned by the sea during the
171:
169:
167:
70:in valley bottoms. The landscape formed in the
442:
8:
638:
536:
449:
435:
427:
373:
92:being only surficially scoured in parts.
34:
18:
163:
7:
1010:Landforms of Västra Götaland County
81:and covered by a thick blanket of
14:
39:An undulating hilly landscape in
23:An undulating hilly landscape in
883:Central SkĂĄne Volcanic Province
203:10.1016/j.gloplacha.2012.10.015
964:Transscandinavian Igneous Belt
244:10.1016/j.geomorph.2007.02.049
1:
417:10.1016/S0169-555X(01)00042-3
375:10.1080/04353676.2019.1702809
322:10.1080/11035897.2017.1364293
154:that characterize the coast.
122:. This zone includes most of
53:Sub-Mesozoic hilly peneplains
995:Landforms of Blekinge County
281:10.1016/0301-9268(93)90086-H
216:Kleman, J.; Stroeven, A.P.;
1000:Landforms of Halland County
182:Global and Planetary Change
146:. In Bohuslän the Mesozoic
1051:
939:Blekinge-Bornholm Province
893:Kattsund-Koster dyke swarm
549:Billingen terminal moraine
1005:Landforms of SkĂĄne County
687:Sorgenfrei-Tornquist Zone
667:Nordfjord-Sogn Detachment
524:Sub-Mesozoic hilly relief
57:Sub-Mesozoic hilly relief
949:Scandinavian Caledonides
692:South Finland Shear Zone
610:Jotnian sedimentary rock
959:Sveconorwegian Province
789:Central Swedish lowland
574:Skövde terminal moraine
499:South SmĂĄland peneplain
458:Geology of Fennoscandia
344:Lidmar-Bergström, Karna
177:Lidmar-Bergström, Karna
25:Falkenberg Municipality
913:Särna Alkaline Complex
898:Kola Alkaline Province
834:Scandinavian Mountains
519:Sub-Cambrian peneplain
144:joint valley landscape
48:
32:
974:Western Gneiss Region
954:Svecofennian Province
927:Provinces and orogens
918:Satakunta dyke swarms
854:White Sea Rift System
38:
22:
1035:Weathering landforms
794:Gulf of Bothnia rift
701:Large impact craters
600:Alum Shale Formation
260:Precambrian Research
134:as well as parts of
41:Varberg Municipality
934:Belomorian Province
494:Ostrobothnian Plain
409:2001Geomo..40..145J
389:Johansson, Magnus;
366:2020GeAnA.102....1L
353:Geografiska Annaler
314:2017GFF...139..244L
273:1993PreR...64..337L
236:2008Geomo..97...73K
195:2013GPC...100..153L
844:South Swedish Dome
804:Lake Ladoga graben
120:South Swedish Dome
113:Swedish West Coast
59:is a landscape in
49:
33:
982:
981:
908:Rapakivi granites
862:
861:
799:Lake Inari graben
723:Hummeln structure
628:
627:
533:Sedimentary cover
109:summit accordance
86:sedimentary rocks
1042:
1025:Plains of Sweden
1020:Plains of Norway
819:Norrland terrain
639:
615:Reusch's Moraine
593:Sedimentary rock
537:
451:
444:
437:
428:
421:
420:
403:(1–2): 145–161.
386:
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340:
334:
333:
291:
285:
284:
267:(1–4): 337–345.
254:
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213:
207:
206:
173:
1050:
1049:
1045:
1044:
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1040:
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1015:Mesozoic Europe
985:
984:
983:
978:
969:Timanide Orogen
922:
858:
782:Morphostrucures
777:
696:
624:
588:
569:Sevetti moraine
528:
509:200 m peneplain
504:300 m peneplain
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90:glacier erosion
17:
12:
11:
5:
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1038:
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1032:
1030:Unconformities
1027:
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895:
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864:
863:
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859:
857:
856:
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849:Vättern graben
846:
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839:Scanian horsts
836:
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826:
821:
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796:
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760:
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748:Ritland crater
745:
740:
735:
730:
725:
720:
715:
713:Gardnos crater
710:
704:
702:
698:
697:
695:
694:
689:
684:
682:Röjnoret Fault
679:
677:Protogine Zone
674:
669:
664:
659:
657:Iapetus Suture
654:
652:Burträsk Fault
648:
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636:
630:
629:
626:
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620:Visingsö Group
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489:Paleic surface
486:
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479:Hardangervidda
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454:
453:
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439:
431:
423:
422:
381:
335:
308:(4): 244–259.
286:
249:
230:(1–2): 73–90.
218:Lundqvist, Jan
208:
162:
161:
159:
156:
99:formed in the
15:
13:
10:
9:
6:
4:
3:
2:
1047:
1036:
1033:
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1023:
1021:
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1016:
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960:
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947:
945:
944:Kola Province
942:
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919:
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845:
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840:
837:
835:
832:
830:
827:
825:
822:
820:
817:
815:
812:
810:
809:Lofoten horst
807:
805:
802:
800:
797:
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790:
787:
786:
784:
780:
774:
771:
769:
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764:
761:
759:
756:
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751:
749:
746:
744:
741:
739:
736:
734:
733:Lockne crater
731:
729:
726:
724:
721:
719:
718:Granby crater
716:
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637:
635:
631:
621:
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613:
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608:
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605:Hedmark Group
603:
601:
598:
597:
595:
591:
585:
584:Veiki moraine
582:
580:
577:
575:
572:
570:
567:
565:
562:
560:
559:Rogen moraine
557:
555:
554:Pulju moraine
552:
550:
547:
546:
544:
542:
538:
535:
531:
525:
522:
520:
517:
515:
512:
510:
507:
505:
502:
500:
497:
495:
492:
490:
487:
485:
484:Muddus plains
482:
480:
477:
475:
474:Borsu surface
472:
471:
469:
467:
466:Paleosurfaces
463:
459:
452:
447:
445:
440:
438:
433:
432:
429:
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406:
402:
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396:Geomorphology
392:
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223:Geomorphology
219:
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200:
196:
192:
188:
184:
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172:
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157:
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153:
152:Bohus granite
149:
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141:
137:
136:Västergötland
133:
129:
125:
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106:
102:
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79:transgression
77:
73:
69:
66:
62:
58:
54:
46:
42:
37:
30:
26:
21:
878:Alnö Complex
824:Omberg horst
814:Muhos Graben
763:Söderfjärden
672:Pärvie Fault
662:Lainio Fault
564:Salpausselkä
523:
400:
394:
391:Migon, Piotr
384:
357:
351:
338:
305:
299:
289:
264:
258:
252:
227:
221:
211:
186:
180:
117:
94:
72:Mesozoic Era
56:
52:
50:
888:Fen Complex
829:Oslo Graben
753:Siljan Ring
644:shear zones
642:Faults and
579:Trollgarden
189:: 153–171.
61:Scandinavia
989:Categories
903:Norra Kärr
758:Sääksjärvi
728:Lappajärvi
634:Structures
514:Strandflat
158:References
148:weathering
83:Cretaceous
65:kaolinized
871:provinces
768:Suvasvesi
330:134300755
97:peneplain
76:Campanian
541:Moraines
346:(2020).
132:Blekinge
124:Bohuslän
105:Triassic
869:igneous
867:Lesser
738:Lumparn
405:Bibcode
362:Bibcode
310:Bibcode
269:Bibcode
232:Bibcode
191:Bibcode
128:Halland
111:in the
101:Permian
68:bedrock
45:Halland
29:Halland
773:Tvären
708:Dellen
328:
140:Scania
326:S2CID
743:Mien
138:and
130:and
103:and
51:The
413:doi
370:doi
358:102
318:doi
306:139
301:GFF
277:doi
240:doi
199:doi
187:100
55:or
991::
411:.
401:40
399:.
368:.
356:.
350:.
324:.
316:.
304:.
298:.
275:.
265:64
263:.
238:.
228:97
226:.
197:.
185:.
166:^
126:,
43:,
27:,
450:e
443:t
436:v
419:.
415::
407::
378:.
372::
364::
332:.
320::
312::
283:.
279::
271::
246:.
242::
234::
205:.
201::
193::
47:.
31:.
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