Jarðskjálftar árin 1954 og 1955

The seismograph station at Reykjavik was operated with three short period Sprengnether seismographs during these years. New stations were erected at Akureyri (65°40.3' N, 18°06.0' W) and at Vík (63°25.3' N, 19°01.0' W). At both these stations, one Mainka seismograph is operated,...

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Main Author: Tryggvason, Eysteinn
Other Authors: Raunvísindastofnun (HÍ), Science Institute (UI), Verkfræði- og náttúruvísindasvið (HÍ), School of Engineering and Natural Sciences (UI), Háskóli Íslands, University of Iceland
Format: Article in Journal/Newspaper
Language:Icelandic
Published: Hið íslenzka náttúrufræðifélag 1956
Subjects:
Online Access:https://hdl.handle.net/20.500.11815/1326
id ftopinvisindi:oai:opinvisindi.is:20.500.11815/1326
record_format openpolar
spelling ftopinvisindi:oai:opinvisindi.is:20.500.11815/1326 2023-05-15T13:08:26+02:00 Jarðskjálftar árin 1954 og 1955 Earthquakes in Iceland during 1954 and 1955 Tryggvason, Eysteinn Raunvísindastofnun (HÍ) Science Institute (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland 1956 77-86 https://hdl.handle.net/20.500.11815/1326 is ice Hið íslenzka náttúrufræðifélag Náttúrufræðingurinn;26(2) 0028-0550 https://hdl.handle.net/20.500.11815/1326 Náttúrufræðingurinn info:eu-repo/semantics/openAccess Jarðskjálftar Jarðskjálftamælingar Ísland Earthquakes Iceland 1954 1955 info:eu-repo/semantics/article 1956 ftopinvisindi https://doi.org/20.500.11815/1326 2022-11-18T06:51:46Z The seismograph station at Reykjavik was operated with three short period Sprengnether seismographs during these years. New stations were erected at Akureyri (65°40.3' N, 18°06.0' W) and at Vík (63°25.3' N, 19°01.0' W). At both these stations, one Mainka seismograph is operated, static magnification about 70. The seismic activity in Iceland was rather high during these years, especially during the period September 1954 to May 1955. At Reykjavík about 500 tremors were recorded during 1954 and about 365 during 1955. Of these, about 350 in 1954 and 300 in 1955 were of local origin, epicentral distance less than 500 km. At Akureyri about 90 earthquakes were recorded during 1954 and about 70 during 1955. Earthquakes were felt on at least 21 days during 1954, three days in Northlceland and 18 days in Southwest-Iceland. During 1955 earthquakes were felt on at least 37 days, 24 days in North-Iceland and 15 days in Southwest- Iceland. The most pronounced earthquakes occurred as follows: 1954. September 15th. About 10 shocks were felt at Grindavík. October 29th. Numerous shocks felt at Hveragerði and Hveradalir. The largest shocks were felt over area of about 7000 km-. October 30th. One shock felt over the same area as on October 29th. November 21st. Several earthquakes felt at Hveragerði and Hveradalir. Largest shocks felt over the same area as on October 29th. 1955. January 15th. Considerable earthquakes at Grindavík. Macroseismic area of the largest shocks about 30000 km2. January 18th. Earthquakes felt over 8000 km- area in South-Iceland. February 27th. Strong earthquakes in Axarfjörður, North-Iceland, where tremors were felt on almost all days untill March 20th. Macroseismic area of the largest shocks about 30000 km2. In the epicentral area about 200 shocks were felt during this swarm, the maximum intensity beeing VII on modified Mercalli scale. Minor damage was done in the epicentral region. March 13lh. Strong earthquake in South-Iceland, felt over 10000 km2. April lsl. Strong earthquakes at Hveragerði, where minor ... Article in Journal/Newspaper Akureyri Akureyri Akureyri Grindavík Iceland Reykjavík Reykjavík Opin vísindi (Iceland) Akureyri Axarfjörður ENVELOPE(-16.764,-16.764,66.296,66.296) Grindavík ENVELOPE(-22.439,-22.439,63.838,63.838) Hveragerði ENVELOPE(-21.186,-21.186,64.000,64.000) Reykjavík Vík ENVELOPE(-18.762,-18.762,66.136,66.136)
institution Open Polar
collection Opin vísindi (Iceland)
op_collection_id ftopinvisindi
language Icelandic
topic Jarðskjálftar
Jarðskjálftamælingar
Ísland
Earthquakes
Iceland
1954
1955
spellingShingle Jarðskjálftar
Jarðskjálftamælingar
Ísland
Earthquakes
Iceland
1954
1955
Tryggvason, Eysteinn
Jarðskjálftar árin 1954 og 1955
topic_facet Jarðskjálftar
Jarðskjálftamælingar
Ísland
Earthquakes
Iceland
1954
1955
description The seismograph station at Reykjavik was operated with three short period Sprengnether seismographs during these years. New stations were erected at Akureyri (65°40.3' N, 18°06.0' W) and at Vík (63°25.3' N, 19°01.0' W). At both these stations, one Mainka seismograph is operated, static magnification about 70. The seismic activity in Iceland was rather high during these years, especially during the period September 1954 to May 1955. At Reykjavík about 500 tremors were recorded during 1954 and about 365 during 1955. Of these, about 350 in 1954 and 300 in 1955 were of local origin, epicentral distance less than 500 km. At Akureyri about 90 earthquakes were recorded during 1954 and about 70 during 1955. Earthquakes were felt on at least 21 days during 1954, three days in Northlceland and 18 days in Southwest-Iceland. During 1955 earthquakes were felt on at least 37 days, 24 days in North-Iceland and 15 days in Southwest- Iceland. The most pronounced earthquakes occurred as follows: 1954. September 15th. About 10 shocks were felt at Grindavík. October 29th. Numerous shocks felt at Hveragerði and Hveradalir. The largest shocks were felt over area of about 7000 km-. October 30th. One shock felt over the same area as on October 29th. November 21st. Several earthquakes felt at Hveragerði and Hveradalir. Largest shocks felt over the same area as on October 29th. 1955. January 15th. Considerable earthquakes at Grindavík. Macroseismic area of the largest shocks about 30000 km2. January 18th. Earthquakes felt over 8000 km- area in South-Iceland. February 27th. Strong earthquakes in Axarfjörður, North-Iceland, where tremors were felt on almost all days untill March 20th. Macroseismic area of the largest shocks about 30000 km2. In the epicentral area about 200 shocks were felt during this swarm, the maximum intensity beeing VII on modified Mercalli scale. Minor damage was done in the epicentral region. March 13lh. Strong earthquake in South-Iceland, felt over 10000 km2. April lsl. Strong earthquakes at Hveragerði, where minor ...
author2 Raunvísindastofnun (HÍ)
Science Institute (UI)
Verkfræði- og náttúruvísindasvið (HÍ)
School of Engineering and Natural Sciences (UI)
Háskóli Íslands
University of Iceland
format Article in Journal/Newspaper
author Tryggvason, Eysteinn
author_facet Tryggvason, Eysteinn
author_sort Tryggvason, Eysteinn
title Jarðskjálftar árin 1954 og 1955
title_short Jarðskjálftar árin 1954 og 1955
title_full Jarðskjálftar árin 1954 og 1955
title_fullStr Jarðskjálftar árin 1954 og 1955
title_full_unstemmed Jarðskjálftar árin 1954 og 1955
title_sort jarðskjálftar árin 1954 og 1955
publisher Hið íslenzka náttúrufræðifélag
publishDate 1956
url https://hdl.handle.net/20.500.11815/1326
long_lat ENVELOPE(-16.764,-16.764,66.296,66.296)
ENVELOPE(-22.439,-22.439,63.838,63.838)
ENVELOPE(-21.186,-21.186,64.000,64.000)
ENVELOPE(-18.762,-18.762,66.136,66.136)
geographic Akureyri
Axarfjörður
Grindavík
Hveragerði
Reykjavík
Vík
geographic_facet Akureyri
Axarfjörður
Grindavík
Hveragerði
Reykjavík
Vík
genre Akureyri
Akureyri
Akureyri
Grindavík
Iceland
Reykjavík
Reykjavík
genre_facet Akureyri
Akureyri
Akureyri
Grindavík
Iceland
Reykjavík
Reykjavík
op_relation Náttúrufræðingurinn;26(2)
0028-0550
https://hdl.handle.net/20.500.11815/1326
Náttúrufræðingurinn
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/20.500.11815/1326
_version_ 1766090349041680384