Knowledge (XXG)

Lummelunda Cave

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479: 467: 28: 491: 423: 443: 40: 234:) a few hundred meters from the coastline. The stream was much larger and more forceful before the mire, once the largest on Gotland, was drained at the end of the 19th century. The remaining drainage is led through an underground 1,150 m (3,770 ft) canal, dropping 17 m (56 ft) from Martebo mire to Lummelunda, at 400 liters/second. 369:
system, and a wet, active part. A large number of fossils and stalactite formations can be found in the dry part. The cave has a relatively stable climate with a humidity of 95–100%. According to a source from 1989, the temperature is on average 7 Â°C (45 Â°F) and points out that fluctuations
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in the summer of 1741. The part of the cave where the stream has its outlet, the LinnĂ©'s Cave, is named after him. The LinnĂ©'s Cave is 6 m (20 ft) wide, 3 m (9.8 ft) high and about 12 m (39 ft) long. The bottom of it is filled with water. The Lummelunda Cave is mentioned
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The Lummelunda Cave has been open to the public since 1959. It is visited by about 100,000 people each year, making it the most visited cave in Sweden, and one of the major tourist attractions on Gotland. "The Mountain King's Hall" and "The Chapel" (these combined are called the Visitors' Cave) are
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At least 83 different species of animals including worms, spiders, centipedes, crayfish, beetles, butterflies, fish, mice and bats, have been found in the cave. Plants grow near the artificial lights in the outer parts of the cave. Since the plants are not a natural part of it, they are removed to
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have been found in the main canal leading the water from Martebo mire to the cave. In the area west of the cliff there are five springs. After the draining of the mire the flow of water in the canal have decreased significantly, from 5.5 m/s (190 cu ft/s) in 1948, to 1.4 m/s
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Although the entrance of the cave has been known for centuries, the main part of it was discovered by three teenage boys during the 1940s–50s. It is visited by around 100,000 people every year and is one of the major tourist attractions on Gotland.
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In 1959, a 60 m (200 ft) long tunnel was made from the surface to "The Hall of the Mountain King" to make the cave more accessible to visitors. Another 400 m (1,300 ft) of tunnels and the largest hall so far, was discovered by
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After having explored the first hall of the cave for two years, a large block of stone fell from one of the walls, widening a small opening in the cliff. This led to a 20 m (66 ft) long passage (later called "The Boys' Passage",
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included in the regular tours. It is also possible to go another 500 m (1,600 ft) into the cave system with the special tours. These tours require a trained guide and visitors have to wear special gear and use small boats.
295:), named thus by the boys who thought it looked like a church, where their exploration was hindered by a lake. It was not until 1955, that they managed to get another 175 m (574 ft) further in, using an inflatable boat. 241:. According to an undocumented litigation in 1778, a mill was built at Lummelunda in 1418. The oldest reliable record is from 1594, where three mills are listed at the stream. In the 1620s, six mills were in use at the 306:. Lars Olsson passed away on 19 October 2011, Percy Nilsson passed away in December 2013 and Ă–rjan HĂĄkansson passed in early 2021. All three were made honorary members of the Swedish Speleology Society ( 265:
The first documented attempt to explore the cave was made in 1924 by zoologist Torsten GislĂ©n, but he never got further than 40 m (130 ft) into the cave despite several later attempts.
603: 354:, it starts to dissolve the limestone and widen the cracks into passages and halls. It is one of the longest caves in Sweden; the explored part of it is almost 4.5 km (2.8 mi) long. 932: 887: 279:), found an entrance to the rest of the cave. For seven years they explored the cave on Sundays using matches, candles, planks and a small boat to get deeper into the system. 442: 636: 362:(49 cu ft/s) in 1977. This has caused some of the sinkholes to disappear. During dry summers there is an impending danger that the cave is completely drained. 466: 275:
The breakthrough in finding the cave system happened in 1948, when three teenage boys, Lars Olsson, Ă–rjan HĂĄkansson and Percy Nilsson, known as "The Three Boys" (
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The Lummelunda Cave is situated in Lummelunda, about 13 km (8.1 mi) north of Visby. Its opening is behind the Lummelunda Manor at the old mill
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of the area. It is bisected by a steep cliff running in a north–south direction through the reserve. The eastern part on top of the cliff, is covered in
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in temperature have been noticed as a result of the many visitors. A source from 2011, states that the temperature is 8–12 Â°C (46–54 Â°F).
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is almost 4.5 km (2.8 mi), making it one of the longest caves in Sweden. It is created by the drainage water from the
386:(42 acres); it includes the cave and the corresponding area above the ground and is called the Lummelunda Cave Nature Reserve ( 956: 291:). From 1959 onwards, this hall became the location for the start of the guided tours. A bit further in is "The Chapel" ( 399:
keep the environment as original as possible. The many visitors also have a negative effect on the biology of the cave.
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which is approximately 11 km (6.8 mi) east of Lummelunda. Most of the water runs as a stream, the
868:(in Swedish). Svenska Turistföreningens förlag. pp. 46–48. Archived from the original on 29 July 2016 27: 422: 913:(in Swedish). Svenska Turistföreningens förlag. p. 3. Archived from the original on 29 July 2016 534: 347: 802: 402:
The landscape above the cave, which is also part of the nature reserve, is characterized by the
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cave, formed by surface water trickling down through cracks in the limestones of the Lower
960: 324: 230:, through the north part of the cave system, exiting the limestone cliffs (known as the 648: 599: 303: 39: 969: 507: 250: 246: 637:"Bildande av naturresrevatet Lummelundagrotta i Lummelunda socken, Gotlands Kommun" 825: 44:
Approximate location, size and shape of the explored parts of the Lummelunda Cave.
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forest, and the western part between the cliff and the shore is grassland with
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The Mountain King's Hall: three boys finds the way into the Lummelunda Cave
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Berga-kungens sal: tre pojkar finner vägen till Lummelundagrottans inre
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in September 1985, after they had passed four underwater passages (or "
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A nature reserve to protect the Lummelunda Cave, was established on 20
245:. The cave itself has been known as long as the stream has been used. 366: 365:
The cave is roughly divided into two parts: one dry, also called the
61: 764: 598:[The Lummelunda Cave]. The County Administrative Boards of 529: 287:) into the first large cave hall, "The Hall of the Mountain King" ( 148: 421: 403: 343: 185: 177: 671: 302:
January 2011, "The Three Boys" were honored in a ceremony at the
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Lummelunds bruk: anteckningar om de gotländska järnbruken
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Lummelunda Factory: Notes about the Gotlandic ironworks
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mire. The water forms a stream with its outlet in the
144: 136: 128: 120: 112: 104: 67: 49: 20: 647:(in Swedish). The County Administrative Boards of 472:Stalactite drapery and straws in the Visitors Cave 801:. Helagotland.se. 7 November 2011. Archived from 219:. The water that creates it is drainage from the 931:: CS1 maint: bot: original URL status unknown ( 886:: CS1 maint: bot: original URL status unknown ( 740:[Come with us to the Lummelunda Caves]. 258:and Gotlander Henrik Munthe, where it is called 237:The stream has been used for industry since the 215:The cave was most likely formed before the last 199:. In the 15th to 19th centuries, mills and an 8: 17: 851: 849: 847: 631: 629: 627: 625: 623: 621: 590: 588: 586: 584: 582: 32:Original entrance of the Lummelunda Cave 738:"Följ med oss till Lummelundagrottorna" 706:. Geologiska Föreningen. pp. 86–89 518: 438: 254:in the 1917 cave investigation made by 924: 879: 689: 687: 731: 729: 727: 725: 723: 721: 7: 824:Jarl, Lars-Gunnar (2 January 2014). 524: 522: 184:, Sweden. The explored part of this 382:March 1989. The reserve is 17  350:. When the surface water meets the 954:A tour through the Lummelunda Cave 484:The tourist's entrance to the cave 14: 986:Nature reserves in Gotland County 698:[The cave at Lummelunda] 606:from the original on 26 July 2011 388:Naturreservatet Lummelundagrottan 532:[The Lummelunda Caves]. 496:The entrance of the LinnĂ©'s Cave 489: 477: 465: 441: 426:Lummelunda cave visitors center. 249:wrote about the cave during his 38: 26: 132:Sveriges Speleologförbund – SSF 828:[Percy Nilsson dead]. 563:[The cave data base]. 308:Sveriges Speleologförbund, SSF 1: 991:Landforms of Gotland County 949:Pictures of Lummelunda Cave 832:. Sveriges Speleologförbund 567:. Sveriges Speleologförbund 203:were set up by the stream. 1012: 905:[Caves in Sweden] 901:Ă…ström, Lars-Erik (1986). 860:[Caves in Sweden] 856:Ă…ström, Lars-Erik (1986). 670:Lundberg, Erik B. (1939). 116:Daily tours May–September 108:4.5 km (2.8 mi) 37: 25: 959:19 December 2019 at the 696:"Grottorna i Lummelunda" 262:("Kytt-Jann's cellar"). 549:(subscription required) 456:formation known as the 795:"Lars Olsson Obituary" 694:Tell, Leander (1961). 427: 165: 89:57.738000°N 18.40500°E 763:Olsson, Lars (2005). 530:"Lummelundagrottorna" 425: 331:Geology and geography 645:www.lansstyrelsen.se 535:Nationalencyklopedin 314:Further explorations 168:, also known as the 149:lummelundagrottan.se 137:Land registry number 903:"Grottor i Sverige" 858:"Grottor i Sverige" 826:"Percy Nilsson död" 805:on 12 November 2021 596:"Lummelundagrottan" 94:57.738000; 18.40500 85: /  799:www.helagotland.se 428: 260:Kytt-Janns källare 251:journey to Gotland 418:Tourism and tours 339:("Topmost Mill). 166:Lummelundagrottan 154: 153: 1003: 937: 936: 930: 922: 920: 918: 908: 898: 892: 891: 885: 877: 875: 873: 863: 853: 842: 841: 839: 837: 821: 815: 814: 812: 810: 791: 785: 784: 760: 754: 753: 751: 749: 736:Klint, Kerstin. 733: 716: 715: 713: 711: 701: 691: 682: 681: 667: 661: 660: 658: 656: 642: 633: 616: 615: 613: 611: 592: 577: 576: 574: 572: 561:"Grottdatabasen" 557: 551: 550: 547: 545: 543: 526: 493: 481: 469: 445: 381: 301: 289:Bergakungens sal 100: 99: 97: 96: 95: 90: 86: 83: 82: 81: 78: 42: 30: 18: 1011: 1010: 1006: 1005: 1004: 1002: 1001: 1000: 996:Limestone caves 976:Caves of Sweden 966: 965: 961:Wayback Machine 945: 940: 923: 916: 914: 906: 900: 899: 895: 878: 871: 869: 861: 855: 854: 845: 835: 833: 823: 822: 818: 808: 806: 793: 792: 788: 781: 762: 761: 757: 747: 745: 742:www.gotland.net 735: 734: 719: 709: 707: 699: 693: 692: 685: 669: 668: 664: 654: 652: 651:. 20 March 1989 640: 635: 634: 619: 609: 607: 594: 593: 580: 570: 568: 559: 558: 554: 548: 541: 539: 528: 527: 520: 516: 504: 497: 494: 485: 482: 473: 470: 461: 446: 437: 420: 396: 379: 376: 348:Visby Formation 333: 316: 299: 277:De tre pojkarna 273: 213: 158:Lummelunda Cave 93: 91: 87: 84: 79: 76: 74: 72: 71: 45: 33: 21:Lummelunda Cave 12: 11: 5: 1009: 1007: 999: 998: 993: 988: 983: 978: 968: 967: 964: 963: 951: 944: 943:External links 941: 939: 938: 893: 843: 816: 786: 779: 755: 717: 704:www.grottor.se 683: 662: 649:Gotland County 617: 600:Gotland County 578: 552: 517: 515: 512: 511: 510: 503: 500: 499: 498: 495: 488: 486: 483: 476: 474: 471: 464: 462: 447: 440: 436: 433: 419: 416: 404:karstification 395: 392: 375: 374:Nature reserve 372: 342:The cave is a 332: 329: 315: 312: 304:Campus Gotland 285:Pojkarnas gĂĄng 272: 270:The Three Boys 267: 212: 209: 152: 151: 146: 142: 141: 138: 134: 133: 130: 126: 125: 122: 118: 117: 114: 110: 109: 106: 102: 101: 69: 65: 64: 51: 47: 46: 43: 35: 34: 31: 23: 22: 13: 10: 9: 6: 4: 3: 2: 1008: 997: 994: 992: 989: 987: 984: 982: 979: 977: 974: 973: 971: 962: 958: 955: 952: 950: 947: 946: 942: 934: 928: 912: 911:www.speleo.se 904: 897: 894: 889: 883: 867: 866:www.speleo.se 859: 852: 850: 848: 844: 831: 830:www.speleo.se 827: 820: 817: 804: 800: 796: 790: 787: 782: 780:91-631-7236-4 776: 772: 768: 767: 759: 756: 744:. 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Index



Lummelunda
Gotland
Sweden
57°44′16.8″N 18°24′18″E / 57.738000°N 18.40500°E / 57.738000; 18.40500
lummelundagrottan.se
Swedish
Lummelunda
Visby
Gotland
karst
cave
Martebo
Baltic Sea
ironwork
ice age
Martebo
mire
Middle Ages
Carl Linnaeus
journey to Gotland
geologist
Campus Gotland
cave divers
traps
karst
Visby Formation
groundwater
sinkholes

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