Náttúrufræðingurinn

Volume

Náttúrufræðingurinn - 1986, Page 10

Náttúrufræðingurinn - 1986, Page 10
Sigurður Þórarinsson. 1949. Um aldur Geysis. - Náttúrufr. 19: 34-41. Sigurður Þórarinsson. 1958. Jarðskjálfta- kort Eysteins Tryggvasonar með hlið- sjón af því sem vitað er um jarðskjálfta á fslandi af sögulegum heimildum. - í: Greinargerð jarðskjálftanefndar um jarðskjálftahættu á íslandi (höf. Eysteinn Tryggvason, Sigurður Thor- oddsen og Sigurður Þórarinsson). Tímarit V.F.Í. 43: 81-97. Sigurður Þórarinsson. 1967. The eruption of Hekla in historical times. - The Eruption of Hekla 1947-1948 I: 1- 170. Vísindafélag íslendinga. SUMMARY An ancient earthquake fracture at Holt, Biskupstungur, South Iceland by Haukur Jóhannesson and Bryndís G. Róbertsdóttir Icelandic Museum of Natural History P.O. Box 5320 Reykjavík An ancient earthquake fracture at Holt in Biskupstungur, South Iceland (Fig. 1) is described. It consists of three short en echelon fractures with an overall trend of N20°E and individual trends N32°E to N56°E. The fractures are covered by soil and are exposed as pits and elongated furrows (Fig. 3). The fracture seems to be related to the Vatnsleysa fault (Fig. 2) and may have been formed as a result of a Storm, G. 1888. Islandske Annaler intil 1578. — Christiania: 667 s. Sunnlenskar byggðir. 1980. 1. bindi. Tung- ur, Hreppar, Skeið. Búnaðarsamband Suðurlands, Reykjavík: 520 s. Sveinbjörn Björnsson. 1975. Jarðskjálftar á íslandi. — Náttúrufr. 45: 110—133. Sveinbjörn Björnsson. 1978. sjá Almanna- varnir 1978. Trausti Einarsson. 1938. Geysir í Hauka- dal. — Tímarit V.F.Í. 23: 53—56. Þorvaldur Thoroddsen. 1899—1905. Landskjálftar á íslandi. — Hið íslenzka bókmentafélag, Kaupmannahöfn: 269 s. strike-slip movement along it (Fig. 4). The age of the Holt fracture is uncert- ain. A minor movement of the fracture was observed in the 1896 earthquake. There are ruins of farmhouses on the edge of the fracture. It has been suggested that the farm (named Holt or Útholt) was abandoned in the course of rifting of the fracture and rebuilt about 1200 m further east and renamed Holtakot. No literary sources mention this event but from writt- en accounts it is obvious that the Holtakot farm has existed since early in the seven- teenth century. The changing of the farm site thus happened before 1600. In the course of a great earthquake in the year 1294 considerable changes occur- red at the Geysir thermal field, which is a short distance north of Holt. It has also been suggested that the Great Geysir was formed during that earthquake. It is possi- ble that rifting may have taken place along the Holt fracture during the 1294 earth- quake. 108
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