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Leitin

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20: 60: 46: 68: 36: 294:, if all Icelanders should become Christians, a messenger came running from Hellisheiði and called out: “There is a fire up there.” After the decision was made, that all Icelanders—willing or not—should leave the pagan gods behind, some said that it were the wrath of the pagan gods that had caused the eruption. 244:
But actually, the Svínahraun is composed of 3 lava layers, all from the same volcanic system, the Brennisteinsfjöll, but from different times. The lowermost layer is the 5000 year old Leitahraun, in between is a 2000 year old lava, more or less from the same time as the eruptions in the neighbouring
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This small volcano produced an astonishing quantity of lavas reaching like a girdle over the peninsula of Reykjanes, entering the sea to the north next to the present capital city of Iceland
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Part of the Leitahraun lava flows travelled to the west against the valley opening between Sauðadalahnúkar and Lambafell and then to the north. People of the region call the lava field here
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This Elliðahraun travelled about 27 km down to today’s Reykjavík, and on its way it initiated explosions on a swamp or more probably on small lake which produced the
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For detailed maps of the region see eg. pp. 32 and 84 in: Þór Vigfússon: Í Árnesþingi vestanverðu. Ferðafélag Íslands Árbók 2003. Reykjavík 2003.
422: 560: 27:: Lambafell in the foreground, behind it to the left the valley with the low shield of Leitin, Leitarhraun lavas and small craters of the 487: 575: 399: 339: 39: 555: 516: 425:
Sverrir Hólmarsson, etal.: Icelandic Online Dictionary and Readings. University of Wisconsin. Retrieved 29 July 2020.
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http://digicoll.library.wisc.edu/cgi-bin/IcelOnline/IcelOnline.TEId-idx?type=entry&eid=leiti&q1=Leiti
203: 59: 45: 72: 19: 395: 570: 282:(“Christianisation-Lava”), is connected to a special story: When in June of the year 1000, Christian 199: 183: 28: 307: 403: 379: 50: 507:
Björn Hróarsson: Hellahandbókin. Leiðsögn um 77 Íslenska hraunhella. Reykjavík 2008, pp. 107 – 123
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in the direction of Hellisheiði and again on its western side. They are under nature protection.
358: 318: 302: 263: 254: 237: 178: 169: 160: 151: 119: 113: 91: 466:Þór Vigfússon: Í Árnesþingi vestanverðu. Ferðafélag Íslands Árbók 2003. Reykjavík 2003, pp.13-15 372:
The southern Leitahraun produced a.o. multi colored lava tubes of which the best known are Búri
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Thor Thordarson, Armann Hoskuldsson: Iceland. Classic geology of Europe 3. Harpenden 2002, p.56
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lava tube which can be visited with guided tours are well known visitor attractions.
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The Hringvegur itself is also for a good part constructed on top of these lavas.
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The same lava flow branch produced other interesting landforms like the group of
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and looking to the west, the volcano is to be seen in a broad valley between the
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Some parts of the Leitahraun travelled to the south, over the mountain pass of
363: 343: 143: 139: 531: 518: 382:, situated between the south coast of Reykjanes and the pass of Þrengsli on 132: 53: 498:
Snæbjörn Guðmundsson: Vegavísir um jarðfræði Íslands. Reykjavík 2015, p. 48
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Snæbjörn Guðmundsson: Vegavísir um jarðfræði Íslands. Reykjavík 2015, p. 42
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Tröllabörn-Lækjarbotnum. Friðyst svæði. Suðvesturland. Umhverfisstofnun.
475: 350: 342:. The pseudocraters are located immediately at the western side of the 246: 100: 283: 287: 224:. Today, these lavas are partially covered by younger lava flows. 66: 58: 44: 34: 306:
and reached the coast not far from today’s fisher village of
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Lava flows and fields: Leitahraun, Svínahraun, Elliðahraun
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Whereas the volcano itself is rather remote, some of its
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Part of the northern Leitahraun flows is also called
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Leitin ("the hills") is sometimes also called Leiti
123:after its eruption products (“the lava of Leiti”). 198:shield volcano Leitin is itself also part of the 209:It originated in a probably long drawn, mostly 326:where outcrops are to be found in the valley. 322:, because it followed the course of the river 135:peninsula some 25 km south of Reykjavík. 8: 444: 442: 440: 278:Acc. to Medieval sources, this lava, the 18: 415: 346:when entering the city from the south. 249:system, and the uppermost layer is the 220:as well as to the south in the bay of 131:The lava shield is located on the big 476:https://ferlir.is/kristnitokuhraun-2/ 373: 357: 317: 301: 262: 253: 236: 177: 168: 159: 150: 118: 112: 90: 7: 63:In the lava tube of Raufarhólshellir 330:Other connected volcanic landforms 14: 581:Brennisteinsfjöll Volcanic System 255:[ˈkʰrɪstnɪˌtʰœːkʏˌr̥œyːn] 200:Brennisteinsfjöll volcanic system 164:and behind some small cones, the 161:[ˈsœyːðaˌtaːlaˌn̥uːkar̥] 264:[ˈsviːnaˌr̥œynsˌprʏːnɪ] 1: 267:emitted by the small craters 561:Shield volcanoes of Iceland 402:rootless cone group or the 359:[ˈtʰrœtlaˌpœ(r)tn̥] 597: 362:, some 10 km up the 319:[ˈɛtlɪːðaˌr̥œyːn] 179:[ˈsɪðrɪˈɛltˌpɔrk] 238:[ˈsviːnaˌr̥œyːn] 182:, eruptive vents of the 120:[ˈleiːtaˌr̥œyːn] 117:("hills") or Leitahraun 88:Icelandic pronunciation: 576:Reykjanes Volcanic Belt 532:64.008056°N 21.543611°W 204:Reykjanes Volcanic Belt 138:When travelling on the 213:, ca. 5000 years ago. 155:with its quarries and 152:[ˈlampaˌfɛtl̥] 80: 73:(volcanogenic) tumulus 64: 56: 42: 32: 537:64.008056; -21.543611 286:were discussing with 202:and therefore of the 190:Geology and volcanism 70: 62: 48: 38: 23:Aerial photograph of 22: 556:Volcanoes of Iceland 303:[ˈθreiŋstlɪ] 99:in the southwest of 16:Small shield volcano 528: /  390:Visitor attractions 75:in the foreground, 71:Leitarhraun with a 275:in the year 1000. 92:[ˈleiːtɪn] 81: 65: 57: 43: 33: 396:eruption products 211:effusive eruption 186:volcanic system. 184:Brennisteinsfjöll 170:[ˈnɪrðrɪ] 114:[ˈleiːtɪ] 79:in the background 29:Brennisteinsfjöll 588: 543: 542: 540: 539: 538: 533: 529: 526: 525: 524: 521: 508: 505: 499: 496: 490: 485: 479: 473: 467: 464: 458: 455: 449: 446: 435: 432: 426: 420: 404:Raufarhólshellir 380:Raufarhólshellir 377: 375:[ˈpuːrɪ] 361: 321: 305: 280:Kristnitökuhraun 266: 260:Svínahraunsbruni 257: 251:Kristnitökuhraun 240: 181: 172: 163: 154: 122: 116: 94: 89: 51:Raufarhólshellir 596: 595: 591: 590: 589: 587: 586: 585: 546: 545: 536: 534: 530: 527: 522: 519: 517: 515: 514: 512: 511: 506: 502: 497: 493: 486: 482: 474: 470: 465: 461: 456: 452: 447: 438: 433: 429: 421: 417: 412: 392: 332: 230: 192: 157:Sauðadalahnúkar 129: 109: 87: 31:volcanic system 17: 12: 11: 5: 594: 592: 584: 583: 578: 573: 568: 563: 558: 548: 547: 510: 509: 500: 491: 480: 468: 459: 450: 436: 427: 414: 413: 411: 408: 391: 388: 331: 328: 229: 226: 191: 188: 128: 125: 108: 105: 97:shield volcano 15: 13: 10: 9: 6: 4: 3: 2: 593: 582: 579: 577: 574: 572: 569: 567: 564: 562: 559: 557: 554: 553: 551: 544: 541: 504: 501: 495: 492: 489: 484: 481: 477: 472: 469: 463: 460: 454: 451: 445: 443: 441: 437: 431: 428: 424: 419: 416: 409: 407: 405: 401: 397: 389: 387: 385: 381: 376: 370: 367: 365: 360: 356: 352: 347: 345: 341: 337: 336:rootless cone 329: 327: 325: 320: 316: 311: 309: 304: 300: 295: 293: 289: 285: 281: 276: 274: 273:Syðri Eldborg 270: 265: 261: 256: 252: 248: 242: 239: 235: 227: 225: 223: 219: 214: 212: 207: 205: 201: 197: 189: 187: 185: 180: 176: 175:Syðri Eldborg 171: 167: 162: 158: 153: 149: 145: 141: 136: 134: 126: 124: 121: 115: 106: 104: 102: 98: 95:) is a small 93: 85: 78: 74: 69: 61: 55: 52: 47: 41: 37: 30: 26: 21: 513: 503: 494: 483: 471: 462: 453: 430: 418: 393: 371: 368: 354: 348: 333: 314: 312: 296: 279: 277: 272: 268: 259: 250: 243: 233: 231: 221: 215: 208: 193: 174: 165: 156: 147: 137: 130: 110: 83: 82: 571:Lava fields 535: / 384:Hellisheiði 315:Elliðahraun 308:Þorlákshöfn 25:Hellisheiði 550:Categories 523:21°32′37″W 520:64°00′29″N 410:References 364:Hringvegur 355:Tröllabörn 344:Hringvegur 292:Þingvellir 234:Svínahraun 146:ridges of 144:palagonite 140:hringvegur 566:Reykjanes 478:Ferlir.is 400:Rauðhólar 398:like the 353:, called 340:Rauðhólar 218:Reykjavík 148:Lambafell 133:Reykjanes 127:Geography 54:lava tube 40:Rauðhólar 351:hornitos 324:Elliðaár 299:Þrengsli 290:ones at 222:Selvogur 196:Holocene 77:Bláfjöll 284:vikings 247:Hengill 101:Iceland 49:Within 338:group 166:Nyrðri 84:Leitin 288:pagan 269:Nyðri 378:and 271:and 194:The 173:and 107:Name 258:or 552:: 439:^ 386:. 310:. 241:. 206:. 103:. 86:(

Index


Hellisheiði
Brennisteinsfjöll

Rauðhólar

Raufarhólshellir
lava tube


(volcanogenic) tumulus
Bláfjöll
[ˈleiːtɪn]
shield volcano
Iceland
[ˈleiːtɪ]
[ˈleiːtaˌr̥œyːn]
Reykjanes
hringvegur
palagonite
[ˈlampaˌfɛtl̥]
[ˈsœyːðaˌtaːlaˌn̥uːkar̥]
[ˈnɪrðrɪ]
[ˈsɪðrɪˈɛltˌpɔrk]
Brennisteinsfjöll
Holocene
Brennisteinsfjöll volcanic system
Reykjanes Volcanic Belt
effusive eruption
Reykjavík

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